JP2595412B2 - Prediction method of railroad embankment critical rainfall and train operation management system using the method - Google Patents
Prediction method of railroad embankment critical rainfall and train operation management system using the methodInfo
- Publication number
- JP2595412B2 JP2595412B2 JP12721592A JP12721592A JP2595412B2 JP 2595412 B2 JP2595412 B2 JP 2595412B2 JP 12721592 A JP12721592 A JP 12721592A JP 12721592 A JP12721592 A JP 12721592A JP 2595412 B2 JP2595412 B2 JP 2595412B2
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- Prior art keywords
- rainfall
- embankment
- railway
- collapse
- condition
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- 238000011160 research Methods 0.000 description 2
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- Traffic Control Systems (AREA)
Description
【0001】[0001]
【産業上の利用分野】本発明は、鉄道盛土が崩壊に至る
限界雨量の予測方法及びそれを用いた列車の運転管理シ
ステムに関するものである。BACKGROUND OF THE INVENTION 1. Field of the Invention The present invention relates to a method for predicting a critical rainfall amount at which a railway embankment will collapse and a train operation management system using the method.
【0002】[0002]
【従来の技術】鉄道沿線の盛土は梅雨期の長雨や台風等
による集中豪雨によって崩壊することがあり、これが列
車の安全・安定輸送を阻害する。このような災害を防止
するためには、危険個所の抽出と、これらの地域の防災
対策を適切に実施する必要があることは勿論であるが、
線区の特性に見合った適切な運転規制が必要となる。こ
のため鉄道の保守担当者にとっては、降雨による鉄道盛
土の崩壊の危険性を精度よく予知でき、しかも現場の技
術者が容易に活用できる危険度評価方法が必要となる。2. Description of the Related Art Embankments along railway lines may collapse due to prolonged rainy season or torrential rain caused by typhoons, which hinders safe and stable transportation of trains. In order to prevent such disasters, it is, of course, necessary to identify danger points and appropriately implement disaster prevention measures in these areas.
Appropriate operation regulations that match the characteristics of the line section are required. For this reason, a railway maintenance person needs a risk evaluation method that can accurately predict the risk of collapse of the railway embankment due to rainfall and that can be easily utilized by on-site engineers.
【0003】従来、鉄道盛土の崩壊に関する危険度評価
は、判別解析によって得た結果でその耐雨量を24時間
雨量で示すようになっており、一方、降雨時の列車の徐
行や停止を行なう運転規制では、過去の降雨災害を受け
た雨量から1時間当りの雨量と降り始めからの総雨量を
経験的に決める方法が使用されている。すなわち、危険
箇所の斜面の危険度評価としては、のり面の採点表を用
い、表層土質、高さ、集水条件により採点を行い、これ
に耐雨量性として日雨量(24時間雨量)でもって評価
するようにしている。Conventionally, the evaluation of the risk of collapse of a railway embankment is based on the result obtained by discriminant analysis, and the rain resistance is shown as a 24-hour rainfall. The regulation uses a method of empirically determining the amount of rainfall per hour and the total amount of rainfall from the start of rainfall from the amount of rainfall caused by past rainfall disasters. In other words, as the evaluation of the degree of danger of the slope at the danger point, the slope is graded according to the surface soil, height, and water collection conditions using a scoring table, and daily rainfall (24-hour rainfall) is used as rain resistance. I try to evaluate.
【0004】[0004]
【発明が解決しようとする課題】しかしながら、上記し
た従来の鉄道盛土の崩壊に関する危険度評価方法では、
のり面の採点は、外観的な素因で決定され、地域の特性
を考慮しない全国一律な基準によっており、評価結果の
精度に問題があった。また、のり面の採点結果と、上記
した運転規制雨量とが直接関連付けられておらず、危険
度評価の雨量と運転規制での雨量がそれぞれ別の指標と
なっているといった問題があった。However, in the above-mentioned conventional risk evaluation method for collapse of railway embankment,
The scoring of the slope is determined based on the appearance factors, and is based on a uniform nationwide standard that does not consider the characteristics of the area, and there was a problem with the accuracy of the evaluation results. In addition, there was a problem that the graded result of the slope was not directly associated with the above-mentioned rainfall for operation regulation, and the rainfall for the risk evaluation and the rainfall for operation regulation were different indices.
【0005】このような状況に鑑みて、精度の高い鉄道
盛土の崩壊限界雨量の評価方法の開発が要請されてい
る。本発明は、上記問題点を解決するために、危険度評
価の結果得られる盛土の崩壊限界雨量を、鉄道で使用し
ている運転管理雨量に直接適用でき、精度が高く、列車
の安全運行を行うことができる鉄道盛土の崩壊限界雨量
の予測方法及びそれを用いた列車の運転管理システムを
提供することを目的とする。[0005] In view of such circumstances, there has been a demand for the development of a highly accurate method for evaluating the collapse critical rainfall of railway embankments. The present invention, in order to solve the above problems, can be directly applied to the collapse rainfall of the embankment obtained as a result of the risk assessment to the operation management rainfall used in the railway, high accuracy, safe operation of the train It is an object of the present invention to provide a method of predicting a collapse rainfall of a railway embankment that can be performed and a train operation management system using the method.
【0006】[0006]
【課題を解決するための手段】本発明は、上記目的を達
成するために、鉄道盛土の崩壊限界雨量の予測方法にお
いて、盛土の構造・土質条件、基盤の構造・土質条件、
集水・浸透条件及び経験雨量条件のそれぞれの評価点の
合計を求め、基本点に前記合計された評価点を加算して
総合評価点を求め、予測の対象となる鉄道盛土が存在す
る地域の24時間以内の単位時間当りの最大降雨量であ
る時間雨量を求め、前記地域の降雨開始から累積された
降雨量である連続雨量を求め、前記総合評価点に基づい
て前記連続雨量と前記時間雨量のそれぞれのべき乗で得
られる鉄道盛土の崩壊限界雨量を推定するようにしたも
のである。SUMMARY OF THE INVENTION In order to achieve the above object, the present invention provides a method for predicting a collapse limit rainfall of a railway embankment, comprising: a structure and soil condition of an embankment;
The sum of the respective evaluation points of the water collection and infiltration conditions and the empirical rainfall conditions is obtained, and the total evaluation points are added to the basic points to obtain an overall evaluation point. The time rainfall which is the maximum rainfall per unit time within 24 hours is obtained, the continuous rainfall which is the rainfall accumulated from the start of rainfall in the area is obtained, and the continuous rainfall and the time rainfall are calculated based on the comprehensive evaluation point. It estimates the critical rainfall of the railway embankment obtained by each power of.
【0007】また、列車の運転管理システムにおいて、
盛土の構造・土質条件、基盤の構造・土質条件、集水・
浸透条件及び経験雨量条件のそれぞれの評価点の合計を
求める手段と、基本点に前記合計された評価点を加算し
て、総合評価点を求める手段と、予測の対象となる鉄道
盛土が存在する地域の24時間以内の単位時間当りの最
大降雨量である時間雨量を求める手段と、前記地域の降
雨開始から累積された降雨量である連続雨量を求める手
段と、前記総合評価点に基づいて前記連続雨量と前記時
間雨量のそれぞれのべき乗で得られる鉄道盛土の崩壊限
界雨量を推定する手段と、該鉄道盛土の崩壊限界雨量に
達するか否かを判定する手段と、その結果、崩壊限界雨
量に達する場合には、該鉄道盛土の区間の列車の運転を
規制するようにしたものである。In a train operation management system,
Embankment structure / soil condition, foundation structure / soil condition,
There are means for calculating the sum of the respective evaluation points of the infiltration condition and the empirical rainfall condition, means for adding the totaled evaluation points to the basic points to obtain a comprehensive evaluation point, and a railway embankment to be predicted. A means for calculating a time rainfall which is a maximum rainfall per unit time within 24 hours of the area; a means for calculating a continuous rainfall which is a rainfall accumulated from the start of rainfall in the area; and Means for estimating the collapse limit rainfall of the railway embankment obtained by each power of the continuous rainfall and the hourly rainfall, and means for determining whether or not the collapse embankment of the railway embankment is reached, and as a result, When it reaches, the operation of the train in the section of the railway embankment is regulated.
【0008】[0008]
【作用】本発明によれば、上記のように、盛土の構造・
土質条件、基盤の構造・土質条件、集水・浸透条件及び
経験雨量条件のそれぞれの得点の合計を求め、評価基本
点に前記合計された得点を加算して、総合評価点を求
め、その総合評価点を次式に代入することによって、盛
土の崩壊限界雨量を推定する。 (時間雨量)n ×(総雨量)m =Σ(盛土条件の得点) ここで、n=m=0.3とし、鉄道盛土の崩壊限界雨量
R・rは、 R・r=(時間雨量)×(連続雨量)=〔Σ(盛土条件
の得点)〕1/0.3 この鉄道盛土の崩壊限界雨量に基づいて、鉄道盛土の崩
壊限界雨量に達するか否かを判定し、その結果、崩壊限
界雨量に達する場合には、該鉄道盛土の区間の列車の運
転を規制する。According to the present invention, as described above, the structure of the embankment
The total score of each of soil condition, basement structure / soil condition, water collection / infiltration condition and empirical rainfall condition is obtained, and the total score is added to the evaluation basic point to obtain an overall evaluation score. By substituting the evaluation points into the following equation, the critical rainfall of the embankment is estimated. (Time rainfall) n × (Total rainfall) m = Σ (Score of embankment condition) Here, n = m = 0.3, and the collapse limit rainfall R · r of railway embankment is Rr = (Time rainfall) × (Continuous rainfall) = [Σ (Score of embankment condition)] 1 / 0.3 Based on this railroad embankment's limit collapse rainfall, it is determined whether or not the railway embankment's collapse limit rainfall is reached. , The operation of the train in the section of the railway embankment is regulated.
【0009】[0009]
【実施例】以下、本発明の実施例について図面を参照し
ながら詳細に説明する。図1は本発明の実施例を示す盛
土の危険度評価基準と盛土の崩壊限界雨量を示す図であ
る。図1は本発明の実施例を示す鉄道盛土の崩壊限界雨
量の予測とそれを用いた列車の運転規制システムの概略
全体構成図である。Embodiments of the present invention will be described below in detail with reference to the drawings. FIG. 1 is a diagram showing an embankment risk evaluation criterion and a collapse limit rainfall of the embankment showing an embodiment of the present invention. FIG. 1 is a schematic overall configuration diagram of a prediction of a collapse critical rainfall of a railway embankment and a train operation control system using the prediction according to an embodiment of the present invention.
【0010】以下、盛土の危険度評価基準と盛土の崩壊
限界雨量の予測、更にはそれを用いた列車の運転規制シ
ステムについて説明する。 (A)盛土崩壊に関与する要因アイテムの抽出 降雨時の盛土の安定性に関するポテンシャルは一般には
斜面安定の理論から、 S=f(β,H,c,φ,γ,uW ,ε) …(1) などで表されることは周知のとおりである。ここに、盛
土の構造条件として、βは盛土勾配、Hは盛土高さ、ま
た土質条件として、cは盛土の粘着力、φは内部摩擦
角、γは単位体積重量、uW は間隙水圧であり、εはそ
の他の要因である。Hereinafter, a description will be given of a risk evaluation criterion for embankment, a prediction of embankment critical rainfall, and a train operation regulation system using the same. (A) Extraction of factors related to embankment collapse The potential for embankment stability during rainfall is generally calculated from the theory of slope stability, as follows: S = f (β, H, c, φ, γ, u W , ε) It is well known that (1) is represented. Here, as the structural conditions of the embankment, β is the embankment gradient, H is the embankment height, and as the soil condition, c is the adhesive force of the embankment, φ is the internal friction angle, γ is the unit volume weight, and u W is the pore water pressure. And ε is another factor.
【0011】前記の式(1)は盛土内崩壊に対するもの
であるが、基盤を巻き込む基底崩壊を考えると、基盤厚
さD、基盤の地下水位hB 、表層地盤の土質強度qB 、
基盤傾斜角θB 等がεとして関係する。また、実際には
鉄道盛土における降雨による崩壊の実体を考えると、前
記の式(1)のεは、降雨の集水・浸透条件として、線
路上部の地形的な集水状態WG、線路方向の落ち込み勾
配等で代表される盛土の縦断形態TL や、片切片盛など
の盛土の横断形態TH が崩壊に及ぼす要因になる。The above equation (1) is for the collapse in the embankment. Considering the base collapse involving the basement, the base thickness D, the groundwater level h B of the base, the soil strength q B of the surface ground,
The base inclination angle θ B and the like are related as ε. Further, when actually think the entity of degradation by rain in the railway embankment, said ε of the formula (1) of the water collecting-penetration condition of rain, the line top of topographical catchment state W G, line direction The vertical form T L of the embankment represented by the drop slope of the embankment and the transverse form T H of the embankment such as a one-piece section embankment are factors that influence the collapse.
【0012】更に、鉄道盛土として供用開始直後には、
土羽の締め固め不足部分が降雨侵食などの被害を受けた
り、供用中の長い期間には崩壊に至らないような小規模
な被害を受けることがある。しかし、それらは定常的な
保守の範囲で若干の修復が行なわれるため、盛土が供用
中に受ける経験雨量RE が大きいほど、小規模の補修を
受ける確率が高く、致命的な崩壊に対する盛土の耐降雨
性が大きくなるものと考えられる。なお、この経験雨量
RE については、後述する。Further, immediately after the start of operation as a railway embankment,
Insufficiently compacted portions of the blade may be damaged by rainfall erosion, etc., or may be damaged in a small scale such that they do not collapse during a long period of service. However, since they are slightly repair in the range of routine maintenance is performed, the greater the experienced rainfall R E which embankment is subjected in service, high probability of receiving a small repair, embankment against fatal collapse It is considered that the rain resistance is increased. It should be noted that, for this experience rainfall R E will be described later.
【0013】したがって、前記の式(1)のεは、 ε=g(D,hB ,qB ,θB ,WG ,TL ,TH ,RE )…(2) で表される。前記の式(1)と(2)は降雨による盛土
崩壊に及ぼす要因として、盛土・表層地盤の構造条件、
土質条件、集水地形等の環境条件と経験的な雨量条件を
示したものである。しかし、これらをもとに、鉄道現場
で実用的な評価を行なおうとする場合は、用いる要因が
簡易な試験と現場調査で得られるものである必要があ
る。[0013] Thus, said epsilon of formula (1) of, ε = g (D, h B, q B, θ B, W G, T L, T H, R E) is represented by ... (2) . The above equations (1) and (2) are factors that affect the embankment collapse due to rainfall,
It shows environmental conditions such as soil conditions and catchment topography, and empirical rainfall conditions. However, when trying to make a practical evaluation at a railway site based on these, it is necessary for the factors to be used to be obtained by simple tests and site surveys.
【0014】盛土の土質条件であるc,φ,γは、粘性
土、砂質土と礫質土の土質分類SEと、盛土の表層部の
簡易貫入試験による貫入強度NC によって代表させるこ
とにした。盛土の間隙水圧uW の上昇に関係する要因と
しては、大きくは土質分類によっても区分できるが、H
azen、Creagerなどが提案する粒度特性から
得られる透水係数kを用いる。また、盛土の構造条件の
うち、盛土勾配βは鉄道盛土ではほとんど一定である。
すなわち、ここで用いたデータの平均値は1:1.4で
あり、その標準偏差は1:0.2であるので、この要因
は割愛する。The soil conditions c, φ, and γ of the embankment are represented by the soil classification S E of cohesive soil, sandy soil and gravel soil, and the penetration strength N C of the surface layer of the embankment by a simple penetration test. I made it. Factors related to the rise in the pore water pressure u W of the embankment can be broadly classified by soil classification.
The permeability coefficient k obtained from the particle size characteristics proposed by Azen, Creager and the like is used. In the embankment structural conditions, the embankment gradient β is almost constant in railway embankment.
That is, since the average value of the data used here is 1: 1.4 and the standard deviation is 1: 0.2, this factor is omitted.
【0015】盛土下の表層地盤を巻き込む基底崩壊はほ
とんど発生していないので、基盤の構造・土質条件であ
るD,hB ,qB ,θB を要因とみなす必要はないが、
盛土内の水位の上昇は地下水位と密接に関係すると考え
られるため、表層地盤に関する要因として、基盤傾斜角
θB と表層地盤の地質SB (沖積層、その他)で代表さ
せることにする。Since almost no base collapse involving the surface ground under the embankment has occurred, it is not necessary to consider D, h B , q B and θ B which are the structural and soil conditions of the base as factors.
Since the rise in water level in the fill are considered closely related to groundwater level, as factors related surface layers, geology S B (alluvium, etc.) of the base inclination angle theta B and surface ground to be represented by.
【0016】なお、前記の式(2)の中で盛土に与える
降雨の集水・浸透に関係するWG ,TL ,TH は現場調
査により、また、経験雨量RE は降雨の統計量により簡
単に求められる。したがって、前記の式(1)と(2)
から、Sは、 S=f(H,SE ,NC ,k,SB ,θB ,WG ,TL ,TH ,RE )…(3) で表されることになることになり、本解析に使用するア
イテムとしては前記の式(3)の右辺に示す10個の変
数で代表させることにした。 (B)盛土崩壊に関与する外的基準の抽出 盛土崩壊に関与する外的基準として降雨量を考えるが、
どのような降雨概念を適用すべきかについては、有効雨
量、先行雨量の考え方について多くの研究がある。[0016] In addition, W G related to the catchment-penetration of rainfall to be applied to fill in the above formula (2), T L, by T H is on-site investigation, also, experience rainfall R E is the statistical amount of rainfall Is more easily sought. Therefore, the above equations (1) and (2)
From, S is, S = f (H, S E, N C, k, S B, θ B, W G, T L, T H, R E) ... in becoming represented that by (3) That is, the items used in this analysis are represented by the ten variables shown on the right side of the above equation (3). (B) Extraction of external standards related to embankment collapse Rainfall is considered as an external standard related to embankment collapse.
There are many studies on the concept of effective rainfall and precedent rainfall on what kind of rainfall concept should be applied.
【0017】一方、従来、のり面採点表では日雨量を用
いた評価を行なっている。また、運転規制に用いる雨量
については、一定線区内の過去の災害記録を基にした連
続雨量と時間雨量の組み合わせを適用している。本解析
では、従来から運転規制に用いられてきた経緯も考慮し
て、時間雨量rと連続雨量Rの積値による限界雨量を外
的基準とするが、それぞれの雨量のべき乗(定数m,
n)の積値とすることにし、盛土の耐降雨ポテンシャル
として、 S=Rm ・ rn …(4) で表されるものとした。m=1,n=1の場合は、従来
の運転規制に用いられる外的基準となり、m=1,n=
0の場合には上記ののり面採点表で示される日連続雨量
にほぼ相当する。On the other hand, conventionally, the evaluation using the daily rainfall is performed in the slope scoring table. As for the rainfall used for driving regulation, a combination of continuous rainfall and hourly rainfall based on past disaster records in a certain line section is applied. In this analysis, the critical rainfall based on the product of the hourly rainfall r and the continuous rainfall R is used as an external reference in consideration of the background that has been conventionally used for the operation regulation, but the power of each rainfall (constant m,
to be the product value of n), as耐降rain potential embankment was assumed to be represented by S = R m · r n ... (4). When m = 1 and n = 1, it becomes an external standard used for the conventional driving regulation, and m = 1 and n =
In the case of 0, it corresponds to the daily continuous rainfall shown in the above-mentioned slope scoring table.
【0018】従って、前記の式(3)と式(4)から、 Rm ・ rn =f(H,SE ,NC ,k,SB ,θB ,WG ,TL ,TH ,RE ) …(5) となる。なお、時間雨量は災害発生時のものとせず、2
4時間以内の最大値とした。これはのり面浸食による崩
壊だけでなく、盛土内の間隙水圧の上昇による崩壊も考
慮したためである。すなわち、一降雨時の最大時間雨量
を記録した後、数時間して崩壊した事例もあり、また、
既設盛土における降雨と盛土内間隙水圧に関する計測結
果でも同様の上昇傾向を示していることも考慮したもの
である。[0018] Therefore, the above equations (3) from equation (4), R m · r n = f (H, S E, N C, k, S B, θ B, W G, T L, T H , R E ) (5). The hourly rainfall shall not be the value at the time of disaster,
The maximum value was set within 4 hours. This is because not only collapse due to slope erosion but also collapse due to rise in pore water pressure in the embankment was considered. In other words, after recording the maximum hourly rainfall at the time of one rainfall, there was a case that collapsed several hours later,
This also takes into account the fact that the measurement results of rainfall and pore water pressure in the embankment on the existing embankment show a similar upward trend.
【0019】また、盛土評価地点が既往の鉄道雨量計の
設置地点や気象観測点とは一致しない場合は、そこの雨
量を前記の式(5)に示す盛土評価地点の雨量(rと
R)の値として用いることはできない。そのような場合
には、既往の雨量観測点の時間雨量r0iから盛土評価地
点の時間雨量rD を推定する本願発明者らによるアメダ
ス補完法によって、当該データの雨量を推定した。すな
わち、pを既往の雨量観測地点数、D1 をそれと災害地
との距離としたとき、If the embankment evaluation point does not coincide with the existing railway rain gauge installation point or weather observation point, the rainfall there is calculated as the rainfall (r and R) at the embankment evaluation point shown in the above equation (5). Cannot be used as the value of In such a case, by AMEDAS Interpolation methods by the present inventors to estimate the amount of rainfall per hour r D embankment evaluation point from the time rainfall r 0i of history of rainfall observation point was estimated rainfall of the data. In other words, rainfall observation location number of the history of the p, when the distance between the D 1 At the same disaster areas,
【0020】[0020]
【数1】 (Equation 1)
【0021】で表され、rD とrOiの残差を最小とする
ように、定数Nとpを求めると、N=0.96、p=3
となる。 (C)外的基準とアイテムの統計量 (a)崩壊時の雨量条件 崩壊までの連続雨量R、時間雨量rの頻度分布を図2に
示す。なお、連続雨量とは降雨開始から災害発生時まで
の累積降雨量であるが、途中12時間以上の降雨中断が
ある場合は、中断後からの累積値とする。 (b)盛土の構造・土質条件(H,SE ,NC ) 盛土の構造・土質条件のうち、盛土高さHの頻度分布を
図3(a)に示すが、その平均値は7.5mである。連
続雨量R及び時間雨量rと盛土高さHの関係を図4に示
す。なお、連続雨量R及び時間雨量rは、図4の横軸に
示す盛土高さHの範囲について、それぞれの平均値を表
したものであるが、盛土高さHが高くなると連続雨量R
と時間雨量rは小さくなる傾向があり、土質力学的な安
定計算における傾向とほぼ一致するようである。When constants N and p are determined so as to minimize the residual difference between r D and r Oi , N = 0.96 and p = 3
Becomes (C) External Criteria and Statistics of Items (a) Rainfall Conditions at Collapse FIG. 2 shows the frequency distribution of continuous rainfall R and hourly rainfall r until collapse. The continuous rainfall is the cumulative rainfall from the start of the rainfall to the time of the occurrence of a disaster, and when rainfall is interrupted for 12 hours or more on the way, the continuous rainfall is the accumulated value after the interruption. (B) Embankment structure / soil condition (H, S E , N C ) Among the embankment structure / soil conditions, the frequency distribution of the embankment height H is shown in FIG. 5 m. FIG. 4 shows the relationship between the continuous rainfall R, the hourly rainfall r, and the embankment height H. The continuous rainfall R and the hourly rainfall r represent average values for the range of the embankment height H shown on the horizontal axis of FIG. 4, but when the embankment height H increases, the continuous rainfall R increases.
And the hourly rainfall r tend to be small, which seems to substantially match the tendency in the geodynamic stability calculation.
【0022】盛土の土質SE については、のり面表層部
0.5m〜1.0mの深さから採取した試料の粒度試験
により分類した。これによると、70%が砂質土であ
り、礫質土22%、粘性土8%であった。従来、鉄道の
盛土強度については、スウェーデン式サウンディング試
験機等によって求められることが多かったが、より簡単
で短時間に多くの調査が可能となる斜面調査用簡易貫入
試験機によって盛土強度を求めた。調査によると崩壊事
例の70%以上は崩壊厚さ3m未満であり、盛土表層部
が崩壊する事例が多い。そこで盛土強度NC は表層から
深さ3mまでの平均値とすることとした。崩壊箇所の盛
土強度の頻度分布は図3(b)の通りであった。崩壊盛
土の盛土強度の平均値はNC =5.4であった。また、
NC <6の盛土が全体の約70%を占めている。なお、
従来から使用されてきたスウェーデン式サウンディング
試験と簡易貫入試験との相関式は土質別に本願発明者ら
によって与えられている。 (c)基盤の構造・土質条件(SE ,θB ) 崩壊盛土のうち基盤傾斜角θB が10度以上の、いわゆ
る傾斜地盤上の盛土は全体の半数以上を占めており、基
盤の傾斜が盛土の安定度に影響をもっていることがわか
る。The soil S E of the embankment was classified by a particle size test of a sample taken from a depth of 0.5 m to 1.0 m on the surface of the slope. According to this, 70% was sandy soil, 22% gravel soil and 8% clayey soil. Conventionally, the embankment strength of railways was often determined by a Swedish sounding tester, etc., but the embankment strength was determined by a simple penetrating tester for slope inspection, which enables simpler and more rapid surveys. . According to the survey, more than 70% of collapse cases are less than 3m in collapse thickness, and there are many cases where the embankment surface layer collapses. Therefore embankment strength N C was be an average of up to 3m deep from the surface layer. The frequency distribution of the embankment strength at the collapse site was as shown in FIG. The average value of the embankment strength of the collapsed embankment was N C = 5.4. Also,
Embankments with N C <6 make up about 70% of the total. In addition,
The correlation formula between the Swedish sounding test and the simple penetration test, which have been conventionally used, is given by the present inventors for each soil type. (C) Structural and soil conditions of the basement (S E , θ B ) Of the collapsed embankment, the embankment on the so-called sloping ground where the base inclination angle θ B is 10 degrees or more occupies more than half of the whole, and Has an effect on the stability of the embankment.
【0023】盛土が構築される表層地盤SE には、地質
学的に多くの分類法があるが、できるだけ簡易に分類で
きる方法として、地盤の軟弱さと地下水位を区分できる
点から沖積層と洪積層、岩盤の3つに区分した。その頻
度はそれぞれ23%、15%、24%である。 (d)集水・浸透条件(WG ,k,TL ,TH ) 盛土への水の集中が崩壊に大きく寄与していることは、
過去の崩壊事例について常に言われてきたことではある
が、集水地形条件WG として崩壊側が集水地形、崩壊の
反対側が集水地形、及び非集水地形の3つに分類した。
崩壊事例の中の約20%は集水地形となっている。There are many geological classification methods for the surface ground S E on which the embankment is constructed, but as a method that can be classified as simply as possible, alluvial sedimentation and flooding are performed because the softness of the ground and the groundwater level can be distinguished. It was divided into three layers, lamination and bedrock. The frequencies are 23%, 15% and 24%, respectively. (D) Water collection and infiltration conditions (W G , k, T L , T H ) The concentration of water on the embankment greatly contributes to the collapse.
Albeit it has been said always about the past of the collapse of the case, but the collapse side as the water collecting topographical conditions W G is the water collecting terrain, the other side of the collapse were classified into three catchment terrain, and Hishu water terrain.
Approximately 20% of the collapse cases have catchment topography.
【0024】盛土の縦断形態TL としては、単勾配、落
込勾配点、切盛境界等がある。図5(a)によると雨水
の集中が予想される切盛境界の崩壊が30%以上を占め
ている。また、図5(b)には横断形態TH について、
純盛,片盛(片切片盛を含む)、腹付盛土別の頻度を示
す。一種の片盛である腹付盛土を片盛に合わせて評価す
ると純盛よりも、崩壊事例が多くなっており、構造的に
崩壊に対して弱点となることを示している。 (e)経験雨量条件(RE ) 解析データは盛土建設後5年未満の比較的新しい盛土か
ら90年以上の古いものまでほぼ均等に分布している。
一方、図6(a)のように経年yと崩壊時の連続雨量
R、時間雨量rの関係を地域別に比較してみると、経年
の小さな盛土は少ない降雨量で崩壊している。また、図
6(b)に示すように、崩壊箇所近傍の気象観測所の年
平均降雨量Ry が小さい地域の盛土も少ない雨量で崩壊
している傾向が明らかである。すなわち、年平均降雨量
Ry が多い箇所では災害に至らないような小規模な被害
をうける確率が高く、排水設備の充実やのり面工の施工
等を行うので、年平均降雨量Ry が少ない地域の同じ条
件の盛土よりも耐降雨量が向上していることがあるもの
と考えられる。このことは、災害に至らない降雨による
災害を含めた盛土の被災件数を線路延長で除した被災率
Pを地域別に求め、これと年平均降雨量Ry との関係を
示した図7からも推定できる。The vertical profile T L of the embankment includes a single slope, a drop slope point, a cut embankment boundary, and the like. According to FIG. 5A, the collapse of the cut boundary where the concentration of rainwater is expected accounts for 30% or more. Moreover, the transverse mode T H in FIG. 5 (b), the
Shows the frequency of pure embankment, single embankment (including single section embankment), and belly embankment. When one kind of one-sided embankment is evaluated according to one-sided embankment, the number of collapse cases is larger than that of pure embankment, which indicates that it is structurally vulnerable to collapse. (E) Empirical rainfall condition (R E ) Analysis data is distributed almost uniformly from relatively new embankments less than 5 years after embankment construction to old ones more than 90 years old.
On the other hand, as shown in FIG. 6A, when comparing the relationship between the aging y and the continuous rainfall R at the time of collapse and the hourly rainfall r for each region, the small embankment over time collapses with a small amount of rainfall. In addition, as shown in FIG. 6B, it is clear that the embankment in the area where the annual average rainfall Ry is small at the weather station near the collapse point also collapses with small rainfall. In other words, the higher the probability to receive a small-scale damage, such as not lead to disaster at the location annual average rainfall R y is large, since the construction, etc. of the rich and glue surface engineering of drainage facilities, the average annual rainfall R y It is considered that the rainfall resistance may be higher than the embankment of the same condition in a small area. This can be seen from FIG. 7 which shows the damage rate P obtained by dividing the number of damages of embankment including the disaster caused by rainfall that did not lead to disaster by the track length for each region, and the relationship between this and the annual average rainfall Ry . Can be estimated.
【0025】このように、耐降雨性には盛土の経過年数
yと平均降雨量Ry の両者が互いに関係すると考えられ
るので、盛土が建設後から崩壊時までに受けた総降雨量
に着目した経験雨量RE という概念も導入することとし
た。 (D)数量化I類による限界雨量の予測 (a)解析の実行 降雨による盛土崩壊の限界雨量を求めるにあたり、前記
の式(5)の右辺を一次展開した形で、前記(C)
(b)〜(e)を考慮し、図8のようなカテゴリーにつ
いて数量化I類による多変量解析を実施した。As described above, since the elapsed years y of the embankment and the average rainfall Ry are considered to be related to each other in the rainfall resistance, attention was paid to the total rainfall that the embankment received from the time of its construction until its collapse. the concept of experience rainfall R E also was decided to introduce. (D) Prediction of critical rainfall by quantification type I (a) Execution of analysis In order to determine the critical rainfall of embankment collapse due to rainfall, the above-mentioned (C) is obtained by linearly expanding the right side of the above equation (5).
In consideration of (b) to (e), a multivariate analysis was performed on the category as shown in FIG.
【0026】その時、前記の式(5)の左辺に示すべき
乗m,nを0.1のピッチで1.2まで順次変えて解析
を行い、得られた重相関係数rO を補完して等高線を描
くと図9のようになる。図によれば、等高線は0.2<
m,n<0.4の領域にrOの高いところがあることを
示しており、そのピーク位置は、m=n=0.3の時で
ある。その時の重相関係数は、rO =0.87である。
このrO に対応する各カテゴリー毎のアイテムの偏相関
係数とウェイトは、図8のようになる。At this time, analysis is performed by sequentially changing the powers m and n shown on the left side of the above equation (5) to 1.2 at a pitch of 0.1 to complement the obtained multiple correlation coefficient r O. Drawing contour lines results in FIG. According to the figure, the contour line is 0.2 <
This shows that there is a place where r O is high in the region where m, n <0.4, and the peak position is when m = n = 0.3. Multiple correlation coefficient at that time is r O = 0.87.
FIG. 8 shows the partial correlation coefficient and weight of the item for each category corresponding to r O.
【0027】限界雨量Rm ・rn (m=n=0.3)に
対する予測値と観測値の関係は図10のようであり、的
中率は高い。 (b)解析結果の総括 上記した解析で得られた各アイテムの偏相関係数から最
も限界雨量に大きく寄与するアイテムから順位をつけれ
ば、RE >WG >θB >NC >TL >H>k>SE >S
B >TH である。The relationship predicted and observed values for the limit rainfall R m · r n (m = n = 0.3) is like in Figure 10, predictive value is high. (B) I mean rank from greatly contributes item most limiting rainfall from the partial correlation of each item was obtained in the analysis summary the above analysis results, R E> W G> θ B> N C> T L >H>k> S E > S
B> is a T H.
【0028】なお、図8のカテゴリーウェイトから得ら
れるレンジについて各アイテムの順位をつけると、偏相
関係数から得られたものと比較して、盛土強度NC ,盛
土の縦断形態TL と盛土高さHについては順位が相違す
るが、これは前者のレンジが各アイテムの中で離散的な
ウェイトの絶対値の幅を示すのに対して、後者の偏相関
係数はアイテム中の各カテゴリーに対する相関係数に相
当する値を与えたものであり、これら両者に若干の順位
の差を生じたものであると考えられる。The ranking of each item in the range obtained from the category weights shown in FIG. 8 shows that the embankment strength N C , the longitudinal profile T L of the embankment and the embankment are compared with those obtained from the partial correlation coefficient. The rank is different for the height H. This is because the former range indicates the width of the absolute value of the discrete weight in each item, whereas the latter partial correlation coefficient is different for each category in the item. , A value corresponding to the correlation coefficient with respect to is given, and it is considered that there is a slight difference between the two.
【0029】経験雨量RE が大きくなるにしたがい、限
界雨量は大きくなる傾向にあり、盛土崩壊の危険度は低
くなる傾向となる。盛土条件のうち、盛土高さHについ
ては図4とほぼ同じ傾向を示し、盛土高さHが高くなる
と限界雨量は小さくなる傾向となる。盛土強度NC につ
いては、頻度の小さいNC >8のアイテムを除いては強
度が大きくなれば限界雨量は向上する傾向を示す。ま
た、盛土土質SE については、砂質土の新設盛土の表層
部は集中豪雨によって侵食崩壊しやすいと言われていた
が、本解析では粘性土盛土のウェイトが負となってお
り、砂質土盛土よりも粘性土盛土の方が危険度は高くな
る結果となった。これは間隙水圧の排出が砂質土や礫質
土よりも抑制されるものを示すものと考えられる。一
方、透水係数kについては、kが10-3cm/sのオー
ダーの時が最も危険であることを示している。[0029] In accordance with experience rainfall R E increases, limit rainfall tends to be greater, the risk of embankment collapse tends to be low. Among the embankment conditions, the embankment height H shows almost the same tendency as that in FIG. 4, and as the embankment height H increases, the critical rainfall tends to decrease. Regarding the embankment strength N C , the marginal rainfall tends to increase as the strength increases, except for items with low frequency N C > 8. Regarding the embankment soil S E, it was said that the surface layer of the newly built embankment of sandy soil was likely to be eroded and collapsed by concentrated torrential rain. However, in this analysis, the weight of the cohesive embankment was negative, The risk was higher for cohesive embankment than for embankment. This is considered to indicate that the discharge of pore water pressure is suppressed more than that of sandy or gravel soil. On the other hand, it is shown that the permeability is most dangerous when k is on the order of 10 −3 cm / s.
【0030】基盤の構造・土質条件のうち、基盤傾斜角
度θB については、これが10度以上の場合であると危
険性が高くなることを示しているが、これは経験的にい
われてきたことと一致する。表層地盤地質SB について
は、沖積層地盤の場合が、危険度が高いという結果とな
った。集水・浸透条件のうち、集水地形WG について
は、崩壊側の集水地形が危険度が非常に高く、集水地形
でない場合は安全側となっている。盛土の横断形態TH
については、片切片盛、腹付盛土のような条件であると
危険度は高くなる結果となった。一方、盛土の縦断形態
TL については、安全側という定説と異なり、切盛境界
等の特殊な条件の場合が安全という結果となった。この
ような条件の盛土は、予め排水対策などの処置がなされ
ていたことが原因した結果といえる。 (E)盛土の危険度評価基準 (a)鉄道盛土における危険度評価基準 数量化I類による解析で得たカテゴリーのウェイトに対
して、(D)(b)で述べた評価に加え鉄道盛土の実態
に即した経験的、工学的な配慮を行ない、図11に示す
盛土の危険度評価基準を提案する。Among the structural and soil conditions of the basement, the base inclination angle θ B indicates that the danger increases when the inclination angle θ B is 10 degrees or more, which has been empirically described. Matches. For surface soil geology S B, the case of alluvium soil has become a result of a high degree of risk. Among the catchment-osmotic conditions, for the water collecting terrain W G, danger degree of water collecting terrain of collapse side is very high, if not the water collecting terrain has become a safe side. Embankment crossing form TH
As for, when the conditions were such as single-section and one-sided embankment, the risk became high. On the other hand, with respect to the longitudinal form TL of the embankment, unlike the consensus on the safe side, the result was safe under special conditions such as a cut boundary. The embankment under such conditions can be said to be a result of the fact that measures such as drainage measures have been taken in advance. (E) Criterion evaluation criteria for embankment (a) Criterion evaluation criteria for railway embankment In addition to the evaluations described in (D) and (b), the railway embankment Considering empirical and engineering considerations based on the actual situation, we propose the evaluation criteria for the risk of embankment shown in FIG.
【0031】この評価基準は基本点である13.14点
に盛土の構造・土質条件、基盤の構造・土質条件、集水
・浸透条件及び経験雨量条件の該当する評価点の合計を
加えて、連続雨量と時間雨量の積値Rm ・rn (ただし
m=n=0.3)を求めようとするものである。個々の
盛土については前記の式(5)の右辺は定数となるの
で、限界雨量は、図12に示すように、Rとrを変数と
する双曲線で表されることになる。This evaluation criterion is obtained by adding 13.14 points, which are the basic points, to the sum of the corresponding evaluation points of the embankment structure / soil condition, basement structure / soil condition, water collection / penetration condition, and empirical rainfall condition. is intended to be obtained a continuous rainfall and time rainfall product values R m · r n (provided that m = n = 0.3). For each embankment, the right side of the above equation (5) is a constant, so that the critical rainfall is represented by a hyperbola with R and r as variables, as shown in FIG.
【0032】ただし、盛土の条件によっては、限界雨量
が非常に小さくなる場合が生ずるが、この場合は、分析
に使用した崩壊事例の最低雨量が、R・r=635mm
2 /h(R0.3 r0.3 =6.93)を下限値とする。こ
の時、鉄道盛土の降雨に対する危険度評価の手法は図1
3のようになる。まず、着目する盛土に対して踏査を行
ない、図11の危険度評価基準に示されるアイテムにつ
いて評価を行う〔ステップ (1)〕。一般には盛土強度N
C を除けば踏査のみで十分な資料が得られる。盛土強度
NC については必要があれば簡易貫入試験によるサウン
ディングを行う〔ステップ (2)〕。これらの評価データ
を図11に適合させ〔ステップ (3)〕 、Rm ・rn の
計算を実行する〔ステップ(4)〕。However, depending on the conditions of the embankment, the critical rainfall may become very small. In this case, the minimum rainfall of the collapse case used in the analysis is R · r = 635 mm.
2 / h (R 0.3 r 0.3 = 6.93) is the lower limit. At this time, the method of risk assessment for rainfall on railway embankment is shown in Fig. 1.
It looks like 3. First, the embankment of interest is surveyed, and the items shown in the risk evaluation criteria of FIG. 11 are evaluated [step (1)]. Generally embankment strength N
Except for C , sufficient data can be obtained by reconnaissance alone. The embankment strength N C performs sounding by cone penetration test if necessary [Step (2)]. The evaluation data are adapted to the 11 [Step (3)], to perform the calculation of R m · r n [Step (4)].
【0033】限界雨量R・rが上述の下限値635mm
2 /h以上であるかをチェック〔ステップ (5)〕して、
降雨災害に対する限界雨量を決定する。更に、実際に降
りつつある降雨量に対して、経時的な危険度評価を行う
必要があるか否かを判断〔ステップ (7)〕して、着目す
る盛土地点の経時的な雨量データの有無を判断〔ステッ
プ (8)〕して、盛土地点の経時的な雨量データがない場
合には、前記の式(6)より近傍のアメダス、雨量計か
ら補完雨量を算出する〔ステップ (9)〕。なお、この時
の時間雨量rは、(B)で定義したように、降りつつあ
る現時点から過去24時間以内の最大時間雨量であるの
で、たとえ小雨になり、時間雨量が小さくなっても、過
去24時間以内の最大値が時間雨量rとして採用される
ことになる。一方、盛土のジャストポイントの雨量を適
時把握することが困難な場合には、近傍の雨量計のデー
タを前記の式(6)に代入して補完する。これによって
限界雨量R・rと実降雨量との比較を行い〔ステップ(1
0)〕、経時的な危険度評価〔ステップ(11)〕が可能とな
る。 (F)典型的な崩壊事例に対する検証 前項で示した危険度評価基準を盛土の崩壊事例に適用
し、その精度の検証を試みた。 (a)崩壊事例1 昭和63年7月の三重県中・北西部を襲った梅雨末期
の、最大時間雨量r=41.5mm/h,連続降雨量R
=389.7mmに達する集中豪雨により、高さH=
6.6mの複線盛土の右側のり面が施工基面を含むのり
肩から延長約50mにわたって崩壊した。その崩壊断面
図は、図14のようである。The critical rainfall R · r is equal to the above-mentioned lower limit of 635 mm.
Check if it is 2 / h or more [Step (5)]
Determine the critical rainfall for rainfall disasters. Furthermore, it is determined whether or not it is necessary to evaluate the risk over time for the rainfall that is actually falling [Step (7)]. [Step (8)], and if there is no time-dependent rainfall data at the embankment point, a supplementary rainfall is calculated from the nearby AMeDAS and rain gauge from the above equation (6) [Step (9)] . The hourly rainfall r at this time is, as defined in (B), the maximum hourly rainfall within the past 24 hours from the falling current time. The maximum value within 24 hours will be adopted as the hourly rainfall r. On the other hand, when it is difficult to grasp the rainfall amount at the just point of the embankment in a timely manner, the data of the nearby rainfall gauge is substituted into the above equation (6) for complementation. In this way, the critical rainfall R · r is compared with the actual rainfall [Step (1)
0)], and the risk evaluation over time [step (11)] becomes possible. (F) Verification of typical collapse cases The risk evaluation criteria shown in the preceding section were applied to embankment collapse cases, and verification of the accuracy was attempted. (A) Collapse example 1 Maximum hourly rainfall r = 41.5 mm / h, continuous rainfall R at the end of the rainy season in the middle and northwestern part of Mie Prefecture in July 1988
= H due to torrential rainfall reaching 389.7 mm
The right slope of the 6.6 m double track embankment collapsed over a length of about 50 m from the shoulder including the construction base. The collapsed sectional view is as shown in FIG.
【0034】当該崩壊地は沖積低地の中にあり、自然堤
防の後背湿地となっており、周辺は水田として利用され
ている。軟弱層の厚さは3〜4mである。のり面下部に
高さ1mの腰土留があるが、根入れはなく厚さ30cm
の栗石の上にある。のり面の下部は平板ブロック張りと
なっているが、表面侵食防止程度の効果しか発揮できな
いものと考えられる。一方、崩壊地の反対側の左側のり
面は、図15のように、右側のり面の構造に加えて平板
ブロックの上方に更に3.5mのプレキャスト格子枠工
(鋼管杭1.5m)を施工していたために、崩壊を免れ
たものと考えられる。The collapse site is located in an alluvial lowland, and is a back marsh of a natural embankment, and the surrounding area is used as a paddy field. The thickness of the soft layer is 3 to 4 m. There is a 1m high waist sill at the bottom of the slope, but there is no rooting and the thickness is 30cm
It is on the chestnut stone. Although the lower part of the slope is covered with a flat block, it is considered that only the effect of preventing surface erosion can be exerted. On the other hand, on the left side of the slope opposite to the collapsed land, as shown in Fig. 15, in addition to the structure of the right side slope, a 3.5m precast grid frame (1.5m steel pipe pile) is constructed above the flat plate block. It is thought that he had escaped collapse.
【0035】線路は終点方に向かって1.2%の下り勾
配で粒度試験によって得られた土質は(SM)であり、
透水係数kは10-3cm/sのオーダーである。またの
り面の深さ3mまでの平均盛土強度NC =5.0であっ
た。このような状況のもとで、のり面の補強工が施工さ
れていないために盛土崩壊を起こした線路右側につい
て、提案した評価基準を適用した結果を図16に示す。
得られた限界雨量はR・r=7870mm2 /hとな
り、限界雨量曲線と災害時の雨量との関係を示すと図1
7のようになる。この崩壊は連続雨量Rが約350mm
の時に発生していることから、予測値はこの災害時の雨
量観測値と良く一致している。The soil obtained by the grain size test on the track at a 1.2% downward gradient toward the end point is (SM),
The permeability k is of the order of 10 -3 cm / s. In addition, the average embankment strength up to a depth of 3 m of the slope was N C = 5.0. FIG. 16 shows the result of applying the proposed evaluation criteria to the right side of the track where the embankment collapsed due to the lack of reinforcement work on the slope under such circumstances.
The obtained critical rainfall is R · r = 7870 mm 2 / h, and the relationship between the critical rainfall curve and the rainfall at the time of disaster is shown in FIG.
It looks like 7. This collapse is caused by a continuous rainfall R of about 350 mm.
Since it occurred at the time of the disaster, the predicted value agrees well with the rainfall observation value at the time of this disaster.
【0036】また、図には過去の降雨履歴10例につい
ても示した。そのうち2例は付近の同じような条件の盛
土が崩壊を起こしており、実測した降雨履歴は推定した
限界雨量曲線を超え、危険ゾーンに入っている。また、
残りの事例は崩壊を起こさなかったものであり、ほぼ限
界雨量曲線の下の領域にある。従って、推定値は実測値
を十分満足する。 (b)崩壊事例2 平成元年8月四国地方を襲った台風17号による集中豪
雨により瀬戸内海側の鉄道沿線では、土石流による災害
をはじめとして各所で斜面災害が発生した。これらの災
害のうち、単線盛土が崩壊した事例に適用してみる。The figure also shows ten past rainfall histories. In two of them, the embankment under similar conditions in the vicinity has collapsed, and the measured rainfall history exceeds the estimated critical rainfall curve and is in the danger zone. Also,
The remaining cases, which did not collapse, are almost in the area below the marginal rainfall curve. Therefore, the estimated value sufficiently satisfies the measured value. (B) Collapse Case 2 Heavy rain caused by typhoon No. 17 which hit the Shikoku region in August 1989 caused slope disasters at various places along the railway along the Seto Inland Sea, including debris flow. Among these disasters, we will apply it to the case where a single-line embankment collapsed.
【0037】この盛土は和泉層群の砂岩・頁岩の互層か
らなる山腹に沿った傾斜地盤上の純盛土である。線路は
終点方に向かって12.5%の下り勾配であり、縦断的
には起点方が切取区間の切盛境界にあたる。盛土材料は
砂質土であり、盛土強度は図18に示すように崩壊側で
ある盛土右側ののり肩部で、表層から3mまでは盛土強
度NC =2.3程度と非常に緩い状態である。このよう
な条件のもと提案した評価基準に適用した結果を図16
に示す。This embankment is a pure embankment on a sloping ground along the hillside composed of alternating layers of sandstone and shale of the Izumi Group. The track has a downward slope of 12.5% toward the end point, and the starting point corresponds to the cut boundary of the cut section in the longitudinal direction. The embankment material is sandy soil, and the embankment strength is as shown in Fig. 18 at the right shoulder of the embankment, which is the collapse side, and the embankment strength N C = about 2.3 m from the surface layer, which is very loose. is there. FIG. 16 shows the result of applying the proposed evaluation criteria under these conditions.
Shown in
【0038】得られた限界雨量はR・r=3851mm
2 /hであり、推定した限界雨量曲線と災害時の実測雨
量とは:図19に示すように良く一致している。なお、
図には過去の代表的な降雨履歴6例についても示した。
このうち2例については限界雨量曲線を超え、崩壊危険
ゾーンに入っているが、これは昭和51年の台風17
号、昭和54年の台風20号の記録であり、この時は全
国の鉄道沿線で切取、盛土が数多く崩壊した災害を受け
たものであり、当該盛土付近でも数箇所の災害が発生し
ている。また、残りの降雨履歴は崩壊を起こさなかった
ものであるが、ほぼ限界雨量曲線の安全側の領域にあ
り、推定した限界雨量は実測値をほぼ満足する。The obtained critical rainfall is R · r = 3851 mm
2 / h, and the estimated critical rainfall curve and the actual rainfall measured at the time of disaster are in good agreement as shown in FIG. In addition,
The figure also shows six past typical rainfall histories.
Two of these cases exceeded the critical rainfall curve and entered the collapse danger zone.
The record of Typhoon No. 20 in 1979 was cut off along the railroads nationwide, and the embankment was damaged by many disasters. Several disasters occurred near the embankment. . The remaining rainfall history, which did not cause collapse, is almost on the safe side of the critical rainfall curve, and the estimated critical rainfall almost satisfies the measured value.
【0039】このように、鉄道盛土の降雨による過去の
崩壊事例をもとに、数量化I類によって崩壊に至る限界
雨量を、連続雨量Rと時間雨量rの積値によって予測す
る手法を提案したものである。この盛土の危険度評価手
法を、最近発生した典型的な鉄道盛土崩壊事例に適用し
たところ、予測値と実測値とは良く一致した。ここで提
案した評価基準は、のり面工などの対策がされていない
一般的な盛土の過去の崩壊事例に基づき統計的に求めた
ものはあるが、崩壊を事前に予測する一つの手法として
適用でき、この予測に基づいた列車の運転規制を行うこ
とにより、安全運行を確保することができる。As described above, based on the past collapse cases due to the rainfall on the railway embankment, a method of predicting the critical rainfall that will lead to the collapse by quantification type I by the product value of the continuous rainfall R and the hourly rainfall r has been proposed. Things. When this method for evaluating the risk of embankment was applied to a typical recent case of railway embankment collapse, the predicted value and the measured value agreed well. The evaluation criteria proposed here are statistically calculated based on past collapse cases of general embankments that have not taken measures such as slope work, but are applied as one method of predicting collapse in advance. It is possible to ensure safe operation by restricting train operation based on the prediction.
【0040】このようにして、鉄道盛土の降雨による崩
壊限界雨量の予測を行うことができる。そこで、限界雨
量と実雨量の比較を行い、限界雨量に近づくと、列車の
徐行を行い、限界雨量になると、着目する盛土地点の列
車の運転を停止する。以下、その鉄道盛土における危険
度評価基準を用いた列車の運転規制システムについて、
図1を参照しながら説明する。In this way, it is possible to predict the collapse rainfall due to the rainfall on the railway embankment. Then, the critical rainfall is compared with the actual rainfall, and when approaching the critical rainfall, the train is slowed down, and when the rainfall is reached, the operation of the train at the embankment point of interest is stopped. In the following, the train operation regulation system using the risk evaluation criteria in the railway embankment,
This will be described with reference to FIG.
【0041】上記したように、列車運行管理センター1
に設置される盛土危険度予測装置2にデータ入力装置8
より、 (1)盛土の構造・土質条件としての盛土の高さ
H、土質SE 、盛土強度NC 、(2) 基盤の構造・土質条
件としての表層地盤地質SB 、基盤傾斜角θB 、(3) 集
水・浸透条件としての透水係数k、集水地形WG 、縦断
形態TL 、横断形態TH 、(4) 経験雨量条件としての経
験雨量RE を入力し、それぞれの評価点の合計を求め
る。なお、図1において、3は盛土危険度予測装置2の
全体的情報処理と統括制御を行うCPU(中央処理装
置)、4は各線区からの雨量データを受ける入力インタ
ーフェース、5は外部雨量情報を受けたり、他の盛土危
険度予測装置11,12とのデータの授受を行うインタ
ーフェース、6は一時的にデータを記憶するRAMや盛
土危険度予測装置2のデータ処理・制御を行うプログラ
ムを記憶するROMを内蔵するメモリ、7は盛土危険度
予測のデータの表示装置(CRT)、9は外部記憶装
置、10は盛土危険度予測装置の出力データを外部へ送
信するための出力インターフェース、13は出力インタ
ーフェース10に接続され、各線区への列車運行を実行
させる指令を行う通信装置、20は外部気象情報センタ
ー50からの雨量情報を受けて、その処理を行う外部雨
量情報処理装置である。この外部雨量情報処理装置20
においては、具体的には外部の雨量情報に基づく補完雨
量を算出し、盛土危険度予測装置2,11,12へその
雨量データを送信する。21は各装置間を接続する伝送
路(例えば、LAN)である。As described above, the train operation management center 1
Data input device 8 to embankment risk prediction device 2 installed in
From the following, (1) embankment height H, soil S E , embankment strength N C as the embankment structure / soil condition, (2) surface ground geology S B as the base structure / soil condition, base inclination angle θ B , (3) permeability of the water collecting-osmotic conditions k, collecting terrain W G, vertical form T L, transverse form T H, enter the experience rainfall R E as (4) experience rainfall conditions, each evaluation Find the sum of points. In FIG. 1, reference numeral 3 denotes a CPU (central processing unit) for performing overall information processing and general control of the embankment risk prediction device 2, 4 denotes an input interface for receiving rainfall data from each line section, and 5 denotes external rainfall information. An interface for receiving data and transmitting and receiving data to and from the other embankment risk prediction devices 11 and 12. A RAM 6 for temporarily storing data and a program for performing data processing and control of the embankment risk prediction device 2 are stored. A memory having a built-in ROM, 7 is a display device (CRT) for data of the embankment risk prediction, 9 is an external storage device, 10 is an output interface for transmitting output data of the embankment risk prediction device to the outside, and 13 is an output. A communication device that is connected to the interface 10 and issues a command to execute a train operation to each line section. The communication device 20 receives rainfall information from the external weather information center 50. Te is an external rainfall information processing apparatus for performing the process. This external rainfall information processing device 20
In, specifically, a complementary rainfall is calculated based on external rainfall information, and the rainfall data is transmitted to the embankment risk estimation devices 2, 11, and 12. Reference numeral 21 denotes a transmission line (for example, a LAN) connecting the devices.
【0042】次に、盛土危険度予測装置2に基本点1
3.14を入力し、その基本点を前記合計された評価点
を加算して、総合評価点を求める。一方、予測の対象と
なる鉄道盛土が存在する地域に設置される鉄道雨量デー
タ収集システム30においては、その地域の各所に設置
される雨量計31により、実際の降雨量が測定され、そ
の測定データを送信装置32により送信し、その送信さ
れた測定データを受信装置33にて受信し、雨量データ
管理装置35により、雨量データとして管理するととも
に、その雨量データは通信回線42を介して列車運行管
理センター1に設置される盛土危険度予測装置2に送ら
れる。なお、雨量データ管理装置35において、36は
中央処理装置(CPU)、37は表示装置(CRT)、
38はデータ入力装置、39は入力インターフェース、
40は出力インターフェース、41はRAM及びROM
等のメモリである。Next, the embankment risk prediction device 2 has the basic point 1
3.14 is input, and the basic points are added to the totaled evaluation points to obtain an overall evaluation point. On the other hand, in the railway rainfall data collection system 30 installed in the area where the railway embankment to be predicted exists, the actual rainfall is measured by the rain gauges 31 installed in various parts of the area, and the measurement data is obtained. Is transmitted by the transmitting device 32, the transmitted measurement data is received by the receiving device 33, and is managed as rainfall data by the rainfall data management device 35, and the rainfall data is train operation management via the communication line 42. It is sent to the embankment risk estimation device 2 installed in the center 1. In the rainfall data management device 35, 36 is a central processing unit (CPU), 37 is a display device (CRT),
38 is a data input device, 39 is an input interface,
40 is an output interface, 41 is RAM and ROM
And the like.
【0043】また、前記したように、アメダス補完法に
よって、雨量データ補う場合には、外部気象情報センタ
ー50(例えば、日本気象協会)の雨量情報を通信回線
51を介して、外部雨量情報処理装置20に収集して、
前記雨量データの実測値に代替させることができる。こ
れらの雨量データを基にして、盛土危険度予測装置2に
おいて、24時間以内の単位時間当りの最大降雨量であ
る時間雨量を求める。As described above, when rainfall data is supplemented by the AMeDAS interpolation method, the rainfall information of the external weather information center 50 (for example, Japan Meteorological Association) is transmitted to the external rainfall information processing device via the communication line 51. Collect to 20,
It can be replaced with an actual measurement value of the rainfall data. On the basis of these rainfall data, the embankment risk prediction device 2 obtains the hourly rainfall, which is the maximum rainfall per unit time within 24 hours.
【0044】また、前記地域の降雨開始から累積された
降雨量である連続雨量を求める。そこで、前記総合評価
点に基づいて前記連続雨量と前記時間雨量のそれぞれの
べき乗〔Rm (連続雨量)×rn (時間雨量)〕で得ら
れる鉄道盛土の崩壊限界雨量R・r=(時間雨量)×
(連続雨量)=〔Σ(盛土条件の得点)〕1/0.3 を推定
する。Further, a continuous rainfall, which is a rainfall accumulated from the start of rainfall in the area, is obtained. Therefore, each of power of the time rainfall and the continuous rainfall on the basis of the overall score [R m (continuous rain) × r n (time rainfall)] railway embankment obtained by disintegrating limit rainfall R · r = (Time Rainfall) ×
(Continuous rainfall) = [Σ (score of embankment condition)] 1 / 0.3 is estimated.
【0045】この鉄道盛土の崩壊限界雨量R・rから、
図12に示すように、危険度が予測でき、図20に示す
ように、それに基づき、その鉄道盛土が存在する線区の
列車の運行管理を行う。例えば、限界雨量曲線aに近づ
く場合は、列車徐行情報を盛土危険度予測のデータの表
示装置7に表示したり、警報装置(図示なし)を作動さ
せ、その線区の列車の徐行を通信装置13を介して指示
したり、限界雨量曲線aを超える場合には、その線区の
列車の運行を停止を措置を講じる。図20において点線
bは列車管理のために設定される限界雨量報知曲線であ
り、この線に達すると列車の運行を停止させ、安全な列
車の運行管理を実施することができる。なお、線cは従
来の列車の運行規制を示している。From the collapse rainfall R · r of this railway embankment,
As shown in FIG. 12, the degree of danger can be predicted, and as shown in FIG. 20, the operation management of the train in the line section where the railway embankment exists is performed based on it. For example, when approaching the critical rainfall curve a, the train slow-down information is displayed on the display device 7 for the data of the embankment risk prediction, an alarm device (not shown) is operated, and the slow-down of the train in the line section is performed by the communication device. In the case where an instruction is made via the line 13 or the threshold rain curve a is exceeded, measures are taken to stop the operation of the trains in the line section. In FIG. 20, a dotted line b is a critical rainfall information curve set for train management. When the line reaches this line, train operation is stopped, and safe train operation management can be performed. Line c indicates the conventional train operation regulation.
【0046】なお、本発明は上記実施例に限定されるも
のではなく、本発明の趣旨に基づいて種々の変形が可能
であり、これらを本発明の範囲から排除するものではな
い。It should be noted that the present invention is not limited to the above embodiment, but various modifications are possible based on the spirit of the present invention, and these are not excluded from the scope of the present invention.
【0047】[0047]
【発明の効果】以上、詳細に説明したように、本発明に
よれば、現場調査で得られた盛土の条件を得ることによ
り、時間雨量と連続雨量のそれぞれのべき乗で得られる
崩壊限界雨量を求め、鉄道盛土の崩壊危険予測の精度を
高め、この限界雨量に基づいて、列車の運転規制を確実
に行い、安全運行とそれに伴う安全対策を迅速、かつ的
確に講じることができ、その実用的効果は著大である。As described above in detail, according to the present invention, by obtaining the embankment conditions obtained in the field survey, the collapse limit rainfall obtained by each power of the hourly rainfall and the continuous rainfall can be obtained. And improve the accuracy of the prediction of the risk of collapse of railway embankments, and based on this critical rainfall, ensure that train operation is regulated and that safe operation and associated safety measures can be taken promptly and accurately. The effect is significant.
【図1】本発明の実施例を示す鉄道盛土の崩壊限界雨量
の予測とそれを用いた列車の運転管理システムの全体構
成図である。FIG. 1 is an overall configuration diagram of a prediction of a collapse rainfall of a railway embankment and a train operation management system using the prediction according to an embodiment of the present invention.
【図2】連続雨量と時間雨量の頻度分布を示す図であ
る。FIG. 2 is a diagram showing a frequency distribution of continuous rainfall and hourly rainfall.
【図3】盛土高さと盛土強度の頻度分布を示す図であ
る。FIG. 3 is a diagram showing a frequency distribution of embankment height and embankment strength.
【図4】連続雨量及び時間雨量と盛土高さの関係を示す
図である。FIG. 4 is a diagram showing a relationship between continuous rainfall, hourly rainfall, and embankment height.
【図5】盛土の縦断形態と横断形態の頻度分布を示す図
である。FIG. 5 is a diagram showing a frequency distribution of a vertical form and a transverse form of an embankment.
【図6】連続雨量,時間雨量と経年,年平均雨量の関係
を示す図である。FIG. 6 is a diagram showing a relationship between continuous rainfall, hourly rainfall, aging, and annual average rainfall.
【図7】年平均雨量と盛土被災率の関係を示す図であ
る。FIG. 7 is a diagram showing the relationship between the annual average rainfall and the embankment damage rate.
【図8】偏相関係数とウェイトを示す図である。FIG. 8 is a diagram showing partial correlation coefficients and weights.
【図9】重相関係数の等高線を示す図である。FIG. 9 is a diagram showing contour lines of a multiple correlation coefficient.
【図10】限界雨量の観測値と予測値の相関を示す図で
ある。FIG. 10 is a diagram showing a correlation between an observed value and a predicted value of a critical rainfall.
【図11】鉄道盛土の危険度評価基準を示す図である。FIG. 11 is a diagram showing a risk evaluation standard for railway embankment.
【図12】限界雨量曲線に基づく危険度を示す図であ
る。FIG. 12 is a diagram showing a degree of risk based on a critical rainfall curve.
【図13】鉄道盛土の危険度評価フローチャートであ
る。FIG. 13 is a flowchart for evaluating the risk of railway embankment.
【図14】崩壊事例1の盛土断面図である。FIG. 14 is an embankment cross-sectional view of Collapse Example 1.
【図15】盛土断面形状と盛土強度を示す図である。FIG. 15 is a diagram showing an embankment cross-sectional shape and embankment strength.
【図16】盛土の危険度評価基準の適用例を示す図であ
る。FIG. 16 is a diagram showing an application example of a risk evaluation standard for embankment.
【図17】崩壊事例1の限界雨量曲線を示す図である。FIG. 17 is a diagram showing a critical rainfall curve of Collapse Example 1.
【図18】崩壊事例2の断面図と盛土強度を示す図であ
る。FIG. 18 is a diagram illustrating a cross-sectional view of embankment example 2 and embankment strength.
【図19】崩壊事例2の限界雨量曲線を示す図である。FIG. 19 is a diagram showing a critical rainfall curve of Collapse Case 2.
【図20】限界雨量曲線と列車の運行管理を示す図であ
る。FIG. 20 is a diagram showing a critical rainfall curve and train operation management.
1 列車運行管理センター 2 盛土危険度予測装置 3,36 CPU(中央処理装置) 4,39 入力インターフェース 5 インターフェース 6,41 メモリ 7,37 表示装置(CRT) 8,38 データ入力装置 9 外部メモリ 10,40 出力インターフェース 11,12 他の盛土危険度予測装置 13 通信装置 20 外部雨量情報処理装置 21 伝送路 30 鉄道雨量データ収集システム 31 雨量計 32 送信装置 33 受信装置 35 雨量データ管理装置 42,51 通信回線 50 外部気象情報センター H 盛土の高さ SE 土質 NC 盛土強度 SB 表層地盤地質 θB 基盤傾斜角 k 透水係数 WG 集水地形 TL 縦断形態 TH 横断形態 RE 経験雨量1 Train Operation Management Center 2 Embankment Risk Prediction Device 3,36 CPU (Central Processing Unit) 4,39 Input Interface 5 Interface 6,41 Memory 7,37 Display Device (CRT) 8,38 Data Input Device 9 External Memory 10, Reference Signs List 40 Output interface 11, 12 Other embankment risk prediction device 13 Communication device 20 External rainfall information processing device 21 Transmission line 30 Railway rainfall data collection system 31 Rain gauge 32 Transmitting device 33 Receiving device 35 Rainfall data management device 42, 51 Communication line 50 external weather information center H embankment height S E soil N C embankment strength S B surface ground geology theta B foundation inclination k permeability W G collecting terrain T L vertical form T H cross form R E experience rainfall
───────────────────────────────────────────────────── フロントページの続き (72)発明者 岡田 勝也 東京都国分寺市光町二丁目8番地38 財 団法人 鉄道総合技術研究所内 (72)発明者 野口 達雄 東京都国分寺市光町二丁目8番地38 財 団法人 鉄道総合技術研究所内 (56)参考文献 特公 平3−50969(JP,B2) 特公 平3−22953(JP,B2) ──────────────────────────────────────────────────続 き Continuing on the front page (72) Katsuya Okada, 2-8-8 Hikaricho, Kokubunji-shi, Tokyo 38 Within the Railway Technical Research Institute (72) Tatsuo Noguchi 2--8 Hikaricho, Kokubunji, Tokyo 38 National Railway Technical Research Institute (56) References Japanese Patent Publication No. 3-50969 (JP, B2) Japanese Patent Publication No. 3-22953 (JP, B2)
Claims (6)
・土質条件、集水・浸透条件及び経験雨量条件のそれぞ
れの評価点の合計を求め、(b)基本点に前記合計され
た評価点を加算して、総合評価点を求め、(c)予測の
対象となる鉄道盛土が存在する地域の24時間以内の単
位時間当りの最大降雨量である時間雨量を求め、(d)
前記地域の降雨開始から累積された降雨量である連続雨
量を求め、(e)前記総合評価点に基づいて前記連続雨
量と前記時間雨量のそれぞれのべき乗で得られる鉄道盛
土の崩壊限界雨量を推定することを特徴とする鉄道盛土
の崩壊限界雨量の予測方法。1. The sum of the evaluation points of (a) the structure / soil condition of the embankment, the structure / soil condition of the base, the water collection / infiltration condition and the empirical rainfall condition is calculated, and (b) the sum is calculated to the basic point. (C) determine the hourly rainfall, which is the maximum rainfall per unit time within 24 hours in the area where the railway embankment to be predicted exists, and (c) calculate the total rainfall.
A continuous rainfall, which is the amount of rainfall accumulated from the start of rainfall in the area, is obtained, and (e) a collapse critical rainfall of the railway embankment obtained by each power of the continuous rainfall and the hourly rainfall is estimated based on the comprehensive evaluation point. A method for predicting the critical rainfall of a railway embankment characterized by performing:
さ、土質、盛土強度を含み、基盤の構造・土質条件は表
層地盤地質、基盤傾斜角を含み、集水・浸透条件は透水
係数、集水地形、縦断形態、横断形態を含む請求項1記
載の鉄道盛土の崩壊限界雨量の予測方法。2. The structure / soil condition of the embankment includes height, soil quality, and embankment strength of the embankment, the structure / soil condition of the basement includes surface geology and inclination angle of the basement, and the condition of water collection / penetration is a permeability coefficient. 2. The method for predicting a collapse rainfall of a railway embankment according to claim 1, wherein the method includes a catchment topography, a vertical cross section, and a cross section.
と時間雨量のそれぞれのべき乗は0.3である請求項1
記載の鉄道盛土の崩壊限界雨量の予測方法。3. The evaluation basic point is 13.14, and each power of continuous rainfall and hourly rainfall is 0.3.
The method for predicting the critical rainfall of railway embankment described.
た総降雨量である請求項1記載の鉄道盛土の崩壊限界雨
量の予測方法。4. The method according to claim 1, wherein the empirical rainfall is a total rainfall received from the embankment after construction.
途中12時間以上の降雨中断がある場合は中断後からの
累積された降雨量である請求項1記載の鉄道盛土の崩壊
限界雨量の予測方法。5. The rainfall accumulated from the start of rainfall is:
2. The method according to claim 1, wherein when the rainfall is interrupted for 12 hours or more on the way, the rainfall accumulated after the interruption is the rainfall limit of the railway embankment.
・土質条件、集水・浸透条件及び経験雨量条件のそれぞ
れの評価点の合計を求める手段と、(b)基本点に前記
合計された評価点を加算して、総合評価点を求める手段
と、(c)予測の対象となる鉄道盛土が存在する地域の
24時間以内の単位時間当りの最大降雨量である時間雨
量を求める手段と、(d)前記地域の降雨開始から累積
された降雨量である連続雨量を求める手段と、(e)前
記総合評価点に基づいて前記連続雨量と前記時間雨量の
それぞれのべき乗で得られる鉄道盛土の崩壊限界雨量を
推定する手段と、(f)該鉄道盛土の崩壊限界雨量に達
するか否かを判定する手段と、(g)その結果、崩壊限
界雨量に達する場合には、該鉄道盛土の区間の列車の運
転を規制する列車の運転管理システム。6. A means for calculating the sum of the evaluation points of the structure / soil condition of the embankment, the structure / soil condition of the basement, the water collecting / penetration condition and the empirical rainfall condition, and (b) the basic point Means for obtaining the total evaluation point by adding the total evaluation points; and (c) calculating the hourly rainfall that is the maximum rainfall per unit time within 24 hours in the area where the railway embankment to be predicted exists. Means, (d) means for calculating continuous rainfall, which is the amount of rainfall accumulated from the start of rainfall in the area, and (e) power of each of the continuous rainfall and the hourly rainfall based on the comprehensive evaluation point. Means for estimating the critical rainfall of the railway embankment; (f) means for determining whether the critical rainfall of the railway embankment is reached; and (g) as a result, when the critical rainfall of the railway embankment is reached, Trains that regulate the operation of trains on embankment sections Operation management system.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP12721592A JP2595412B2 (en) | 1992-05-20 | 1992-05-20 | Prediction method of railroad embankment critical rainfall and train operation management system using the method |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP12721592A JP2595412B2 (en) | 1992-05-20 | 1992-05-20 | Prediction method of railroad embankment critical rainfall and train operation management system using the method |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPH05323043A JPH05323043A (en) | 1993-12-07 |
| JP2595412B2 true JP2595412B2 (en) | 1997-04-02 |
Family
ID=14954580
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP12721592A Expired - Lifetime JP2595412B2 (en) | 1992-05-20 | 1992-05-20 | Prediction method of railroad embankment critical rainfall and train operation management system using the method |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JP2595412B2 (en) |
Families Citing this family (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JP5301212B2 (en) * | 2008-08-05 | 2013-09-25 | 前田工繊株式会社 | Evaluation system for embankment stability |
| JP5415175B2 (en) * | 2009-07-31 | 2014-02-12 | 公益財団法人鉄道総合技術研究所 | Advanced train safety control system using ground and vehicle observation data |
| JP5405228B2 (en) * | 2009-07-31 | 2014-02-05 | 公益財団法人鉄道総合技術研究所 | Advanced train safety control system that gathers information on the vehicle |
| CN106054284B (en) * | 2016-07-27 | 2018-08-14 | 中国路桥工程有限责任公司 | The full-automatic Integrate Natural Disasters Prevention early warning system of railway |
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1992
- 1992-05-20 JP JP12721592A patent/JP2595412B2/en not_active Expired - Lifetime
Also Published As
| Publication number | Publication date |
|---|---|
| JPH05323043A (en) | 1993-12-07 |
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