JP2788400B2 - Hydraulic analysis method of water distribution network - Google Patents
Hydraulic analysis method of water distribution networkInfo
- Publication number
- JP2788400B2 JP2788400B2 JP27139393A JP27139393A JP2788400B2 JP 2788400 B2 JP2788400 B2 JP 2788400B2 JP 27139393 A JP27139393 A JP 27139393A JP 27139393 A JP27139393 A JP 27139393A JP 2788400 B2 JP2788400 B2 JP 2788400B2
- Authority
- JP
- Japan
- Prior art keywords
- water
- hydraulic
- model
- extracted
- node
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- Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
- Expired - Lifetime
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- Management, Administration, Business Operations System, And Electronic Commerce (AREA)
- Pipeline Systems (AREA)
- Flow Control (AREA)
Description
【0001】[0001]
【産業上の利用分野】本発明は、配水管網に関する増設
工事、メンテナンス、緊急事態の対応等、保守管理作業
を効率よく行うための配水管網の水理解析方法に関し、
解析対象となる配水管網の各節点から取り出される水量
モデルを生成して、この取り出し水量モデルに対して前
記配水管網の各節点水頭や各管路流量等の水理データを
計算機を用いて演算導出する配水管網の水理解析方法に
関する。BACKGROUND OF THE INVENTION 1. Field of the Invention The present invention relates to a hydraulic analysis method for a water distribution network for efficiently performing maintenance work, such as extension work, maintenance, and response to emergencies.
Generate a water volume model extracted from each node of the distribution network to be analyzed, and use a computer to calculate hydraulic data such as each node head and each pipeline flow of the distribution network with respect to the extracted water volume model. The present invention relates to a hydraulic analysis method for a water distribution network to be derived.
【0002】[0002]
【従来の技術】従来、水源から実際に取り出される水量
パターンを検針水量データから求まる各節点からの実際
の取り出し水量で比例配分して求まる水量パターンを、
前記取り出し水量モデルとして近似して、その取り出し
水量モデルで特定される所定時間毎の取り出し水量に対
して、その都度水理解析を実行することにより、配水管
網の各節点水頭や各管路流量等の所定時間毎の水理デー
タを演算導出していた。例えば、一日の水量パターンに
対して一時間毎の変遷を調べる場合には、合計24回の
水理解析を実行する必要があった。2. Description of the Related Art Conventionally, a water amount pattern obtained by proportionally distributing a water amount pattern actually taken out from a water source with an actual water taken out from each node obtained from meter reading water amount data,
Approximately as the withdrawal water model, by performing hydraulic analysis each time with respect to the withdrawal water amount specified by the withdrawal water amount model specified by the withdrawal water amount model, each node head and each pipeline flow rate of the distribution pipe network The hydraulic data for each predetermined time such as the above was calculated and derived. For example, when examining hourly changes in the daily water volume pattern, it was necessary to execute a total of 24 hydraulic analyzes.
【0003】[0003]
【発明が解決しようとする課題】しかし、上述した従来
の配水管網の水理解析方法によれば、取り出し水量モデ
ルで特定される所定時間毎の取り出し水量に対して、そ
の都度、計算機を用いて水理解析を実行する必要があ
り、時間がかかるという欠点があった。この欠点は、解
析対象となる配水管網の規模が大きくなればそれだけ増
大するもので、日常の業務を想定すると実用に供しえな
いという欠点があった。本発明の目的は上述した従来欠
点を解消する点にある。However, according to the above-mentioned conventional hydraulic analysis method for a water distribution network, a computer is used each time with respect to the amount of water taken out at every predetermined time specified by the model of the amount of water taken out. Hydraulic analysis must be performed, which is time-consuming. This drawback increases as the scale of the distribution pipe network to be analyzed increases, and has a drawback that it cannot be put to practical use assuming daily work. An object of the present invention is to eliminate the above-mentioned conventional disadvantages.
【0004】[0004]
【課題を解決するための手段】この目的を達成するた
め、本発明による配水管網の水理解析方法の特徴構成
は、水源から実際に取り出される水量パターンを検針水
量データから求まる各節点からの実際の取り出し水量で
比例配分して求まる水量パターンを、前記取り出し水量
モデルとして近似して、近似された取り出し水量モデル
で特定される任意時刻における取り出し水量に対して水
理解析を実行して、水理解析により得られた水理データ
を、近似された取り出し水量モデルで特定される特定時
刻における取り出し水量比に基づいて換算して、当該特
定時刻における水理データとするところにある。In order to achieve this object, a characteristic structure of the hydraulic analysis method for a water distribution network according to the present invention is characterized in that a water amount pattern actually taken out from a water source is calculated from each node obtained from meter reading water amount data. The water volume pattern obtained by proportionally distributing the actual water volume is approximated as the water volume model, and a hydraulic analysis is performed on the water volume at an arbitrary time specified by the approximated water volume model. The hydraulic data obtained by the physical analysis is converted into hydraulic data at the specific time by converting the hydraulic data at the specific time specified by the approximated water model.
【0005】[0005]
【作用】各節点から取り出される水量パターンが水源か
ら取り出される水量パターンと相似するとの想定の下、
先ず、水源から実際に取り出される一定期間の水量パタ
ーンを計測して、次に、各節点から取り出される水量比
をそれぞれの節点に接続されている水栓の一定期間の検
針水量データの総和から求めた後に、各節点からの取り
出し水量パターンを、計測された水源の水量パターンを
比例配分して近似する。近似された取り出し水量モデル
で特定される任意時刻における取り出し水量に対して水
理解析を実行して各節点水頭、各管路流速などの水理デ
ータを演算導出する。解析対象となる配水管網の特定時
刻における各節点水頭、各管路流速などの水理データ
を、近似された取り出し水量モデルで求まる当該特定時
刻における使用水量比に基づいて換算するのである。[Effect] Under the assumption that the water amount pattern taken out from each node is similar to the water amount pattern taken out from the water source,
First, the water amount pattern actually taken out from the water source for a certain period is measured, and then the water amount ratio taken out of each node is obtained from the sum of the metering water amount data of the faucet connected to each node for a certain period. After that, the water flow pattern taken out from each node is approximated by proportional distribution of the measured water flow pattern of the water source. Hydraulic analysis is performed on the extracted water amount at an arbitrary time specified by the approximated extracted water amount model to calculate and derive hydraulic data such as each node head and each pipe flow velocity. Hydraulic data such as each node head and each pipeline flow velocity at a specific time of the distribution network to be analyzed is converted based on the used water ratio at the specific time obtained by the approximated taken water amount model.
【0006】図4に示すように、水源からP地点までの
管路が途中で2本の管路S1,S2に分岐している場合
に、ある時刻における解析の結果、P地点における流量
がQ0で、管路S1における流量がQ1、管路S2にお
ける流量がQ2であったとすると、 管路S1における損失水頭 H1=r’(Q1)u 管路S2における損失水頭 H2=r’’(Q2)u と表すことができる。ここに、 r’,r’’,uは定
数である。両管路の損失水頭は等しい筈であるから、H
1=H2とおくことができ、これから、r’(Q1)u
=r’’(Q2)u 、従って、 (Q2/Q1)u =r’’/r’(定数) となり、Q0(=Q1+Q2)がQ0/2と半減する
と、管路Q1,Q2それぞれが半減することになると考
えられる。つまり、他の時刻における流量は、水理解析
を行わなくとも、水理解析により求まったある時刻にお
ける流量をベースに、近似された取り出し水量モデルで
求まる水量比で配分することにより求まることになる。As shown in FIG. 4, when the pipeline from the water source to the point P branches halfway into two pipelines S1 and S2, the analysis at a certain time shows that the flow rate at the point P is Q0. in, the flow rate in line S1 is Q1, the flow rate was Q2 in line S2, head losses H1 = r in line S1 '(Q1) head losses in the u pipe S2 H2 = r''(Q2 ) It can be expressed as u . Here, r ′, r ″, and u are constants. Since the head loss of both pipelines should be equal, H
1 = H2, from which r ′ (Q1) u
= R ″ (Q2) u , and therefore (Q2 / Q1) u = r ″ / r ′ (constant). It is thought that it will be. In other words, the flow rate at another time can be obtained by allocating the flow rate at a certain time obtained by the hydraulic analysis based on the flow rate obtained by the approximated water flow rate model without performing the hydraulic analysis. .
【0007】[0007]
【発明の効果】従って、本発明によれば、複雑な配水管
網であっても、極めて容易且つ高速に所定時間毎の水理
データを導出できる配水管網の水理解析方法を提供でき
るようになった。Thus, according to the present invention, it is possible to provide a hydraulic analysis method for a water distribution network which can very easily and rapidly derive hydraulic data at predetermined time intervals even in a complicated water distribution network. Became.
【0008】[0008]
【実施例】以下に本発明の実施例を説明する。配水管網
の水理解析を行う管網解析装置は、パーソナルコンピュ
ータ或いはワークステーション等の計算機1で構成さ
れ、その機能ブロックは、図1に示すように、解析対象
となる配水管網の水源からの24時間の配水パターン
(取り出し水量パターン)を示すデータと、各節点につ
ながる水栓の検針データとを入力して各節点からの24
時間の取り出し水量パターンを生成する入力モデル生成
部2と、入力モデル生成部2で生成された取り出し水量
パターンの任意時刻Tにおける取り出し水量と、記憶装
置Mに格納された配水管の延長や管径等の管網データを
入力して水理解析を実行する水理解析部3と、水理解析
により得られた時刻Tにおける水理データを、入力モデ
ル生成部2で生成された取り出し水量パターンで特定さ
れる特定時刻T’における取り出し水量比に基づいて換
算して、当該特定時刻T’における水理データとして求
める水理データ生成部4とからなる。Embodiments of the present invention will be described below. A pipe network analysis device for performing hydraulic analysis of a distribution pipe network is configured by a computer 1 such as a personal computer or a workstation, and its functional blocks are, as shown in FIG. 1, from a water source of a distribution pipe network to be analyzed. 24 hours of water distribution pattern (take-out water volume pattern) and water tap data of the faucet connected to each node
An input model generation unit 2 for generating a water withdrawal pattern for time, a water withdrawal amount at an arbitrary time T of the water withdrawal pattern generated by the input model generation unit 2, an extension of the water distribution pipe stored in the storage device M, and a pipe diameter And hydraulic data at time T obtained by hydraulic analysis using the extracted water volume pattern generated by the input model generating unit 2. A hydraulic data generation unit 4 which converts the extracted water amount ratio at the specified time T ′ to obtain hydraulic data at the specified time T ′.
【0009】管網データは、水道施設を構成する配水
管、弁栓、水源等の配置情報を表した図面データと、そ
れら水道施設の管理データ、即ち配水管であれば管種
類、管径、管路長、敷設位置、施工日等を表すデータや
前記図面データにおける配水管同士の接続情報でなる属
性データとからなる。The pipe network data includes drawing data representing arrangement information of water distribution pipes, valve plugs, water sources, etc., constituting water supply facilities, and management data of those water supply facilities, that is, pipe types, pipe diameters, It consists of data representing pipeline length, laying position, construction date, etc., and attribute data consisting of connection information between distribution pipes in the drawing data.
【0010】入力モデル生成部2では、図2(イ)に示
すように、検針された各戸の月当たりの使用水量から時
間平均使用水量を導出し、水源の一日の時間平均配水量
に対する任意の時刻の配水量の比率である時間係数を導
出し、各戸の時間平均使用水量と、時間係数とから取り
出し水量モデルを決定する。即ち、 配水量=Σ取り出し水量 取り出し水量=時間係数×補正係数×検針水量+修正水
量となる。ここで補正係数とは、漏水のような無効無収
水量を考慮するもので、1.0以上の値が適宜設定され
る。さらに、緊急事態や保守工事で必要とされる消火栓
の使用や洗管等に用いられる有効無収水量を考慮するた
め、想定される修正水量を適宜加算する。即ち、入力モ
デル生成部2は目的に応じて適宜取り出し水量モデルが
生成できる。例えば、1月から12月までの各月毎、日
曜から土曜までの1週間を一日毎、1日を0時から23
時までの1時間毎に分割して、それぞれに対応した時間
係数、補正係数を昨年度の収集データから予め求めてテ
ーブルを作成しておけばよい。As shown in FIG. 2A, the input model generation unit 2 derives a time-average water usage from the monthly water usage of each of the measured homes, and calculates an arbitrary water-source daily average water-distribution amount. The time coefficient which is the ratio of the amount of water distribution at the time is derived, and the water amount model is determined by taking out the time average used water amount of each house and the time coefficient. That is, water distribution amount = Σ taken water amount taken water amount = time coefficient x correction coefficient x meter reading water amount + corrected water amount. Here, the correction coefficient takes into consideration the amount of invalid non-revenue water such as water leakage, and is appropriately set to a value of 1.0 or more. Furthermore, in order to consider the use of fire hydrants and the amount of effective non-revenue water used for washing pipes and the like required in emergency situations and maintenance work, the estimated corrected water amount is added as appropriate. That is, the input model generation unit 2 can generate a taken-out water amount model as appropriate according to the purpose. For example, every month from January to December, one week from Sunday to Saturday every day, and one day from 0:00 to 23
The table may be created by dividing the data every hour until the hour, and obtaining the time coefficient and the correction coefficient corresponding to each time from the collected data of the previous year.
【0011】水理解析部3では、上述した各節点からの
取り出し水量モデルの任意時刻における取り出し水量に
対して、接点水頭法を用いて管網の各節点の損失水頭を
流量連続条件に基づいて解いて各管路流量を演算導出す
る。損失水頭Hは次式で求まる。 H =r’Qu ここに、r’=10.666CH -1.85 D-4.87 L,u
=1.85(CH は流速係数、Lは距離、Qは流量、D
は口径)である。The hydraulic analysis unit 3 calculates the loss head at each node of the pipe network based on the continuous flow rate condition by using the contact head method with respect to the water amount taken out at any time of the water amount model taken out from each node described above. By solving, the flow rate of each pipeline is calculated and derived. The head loss H is obtained by the following equation. H = r'Q u where r '= 10.666 CH -1.85 D -4.87 L, u
= 1.85 (CH is flow coefficient, L is distance, Q is flow rate, D
Is the caliber).
【0012】水理データ生成部4では、図2(ロ)に示
すように、取り出し水量モデルの変動パターン毎に管網
計算することなく、残り23回の各管路流量を、取り出
し水量モデルで特定される特定時刻における取り出し水
量比に基づいて換算する。さらに、図3(イ)に示す管
網では、各節点を水源から同図(ロ)に示すような木を
通ってたどり、管路の損失を積み上げて算出する。例え
ば、同図の交点Aの動水位が、水源の高さ−(管路1か
ら5の損失和)で求まり、有効水頭が、動水位−地盤高
さで求まる。As shown in FIG. 2 (b), the hydraulic data generator 4 calculates the remaining 23 pipe flow rates using the extracted water flow model without calculating the pipe network for each variation pattern of the extracted water flow model. The conversion is performed based on the ratio of the amount of water taken out at the specified time. Further, in the pipe network shown in FIG. 3A, each node is traced from a water source through a tree as shown in FIG. For example, the hydraulic level at the intersection A in the figure is obtained by the height of the water source-(the sum of the losses of the pipes 1 to 5), and the effective head is obtained by the hydraulic level-the ground height.
【図1】配水管網の水理解析方法を説明するブロック構
成図FIG. 1 is a block diagram illustrating a hydraulic analysis method for a water distribution network.
【図2】取り出し水量モデルと管路流量の説明図FIG. 2 is an explanatory diagram of a taken-out water amount model and a pipe flow rate.
【図3】節点での水頭を導出する説明図FIG. 3 is an explanatory diagram for deriving a head at a node;
【図4】要部の説明図FIG. 4 is an explanatory view of a main part.
───────────────────────────────────────────────────── フロントページの続き (58)調査した分野(Int.Cl.6,DB名) E03B 1/00──────────────────────────────────────────────────続 き Continued on front page (58) Field surveyed (Int.Cl. 6 , DB name) E03B 1/00
Claims (1)
り出される水量モデルを生成して、この取り出し水量モ
デルに対して前記配水管網の各節点水頭や各管路流量等
の水理データを計算機を用いて演算導出する配水管網の
水理解析方法であって、 水源から実際に取り出される水量パターンを検針水量デ
ータから求まる各節点からの実際の取り出し水量で比例
配分して求まる水量パターンを、前記取り出し水量モデ
ルとして近似して、 近似された取り出し水量モデルで特定される任意時刻に
おける取り出し水量に対して水理解析を実行して、 水理解析により得られた水理データを、近似された取り
出し水量モデルで特定される特定時刻における取り出し
水量比に基づいて換算して、当該特定時刻における水理
データとする配水管網の水理解析方法。1. A water flow model extracted from each node of a distribution pipe network to be analyzed is generated, and hydraulic data such as a head of each node and a flow rate of each pipeline of the distribution pipe network are generated with respect to the extracted water volume model. Is a hydraulic analysis method for a water distribution network that uses a computer to calculate and calculate the water flow pattern, which is obtained by proportionally distributing the water flow pattern actually taken out from the water source to the actual water taken out from each node obtained from the metering water flow data. Is approximated as the extracted water amount model, hydraulic analysis is performed on the extracted water amount at an arbitrary time specified by the approximated extracted water amount model, and the hydraulic data obtained by the hydraulic analysis is approximated. Hydraulic analysis of the water distribution network based on the extracted water volume ratio at the specific time specified by the extracted water volume model Method.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP27139393A JP2788400B2 (en) | 1993-10-29 | 1993-10-29 | Hydraulic analysis method of water distribution network |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP27139393A JP2788400B2 (en) | 1993-10-29 | 1993-10-29 | Hydraulic analysis method of water distribution network |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPH07127105A JPH07127105A (en) | 1995-05-16 |
| JP2788400B2 true JP2788400B2 (en) | 1998-08-20 |
Family
ID=17499444
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP27139393A Expired - Lifetime JP2788400B2 (en) | 1993-10-29 | 1993-10-29 | Hydraulic analysis method of water distribution network |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JP2788400B2 (en) |
Families Citing this family (2)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JP4716694B2 (en) * | 2004-08-24 | 2011-07-06 | 株式会社クボタ | Pipe network analysis method |
| JP4562132B2 (en) * | 2005-03-31 | 2010-10-13 | 国立大学法人横浜国立大学 | Pipe break position specifying device, program and method |
-
1993
- 1993-10-29 JP JP27139393A patent/JP2788400B2/en not_active Expired - Lifetime
Also Published As
| Publication number | Publication date |
|---|---|
| JPH07127105A (en) | 1995-05-16 |
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