JP3996407B2 - Sediment accumulation structure - Google Patents

Sediment accumulation structure Download PDF

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Publication number
JP3996407B2
JP3996407B2 JP2002049673A JP2002049673A JP3996407B2 JP 3996407 B2 JP3996407 B2 JP 3996407B2 JP 2002049673 A JP2002049673 A JP 2002049673A JP 2002049673 A JP2002049673 A JP 2002049673A JP 3996407 B2 JP3996407 B2 JP 3996407B2
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Japan
Prior art keywords
sand
earth
sediment
dike
accumulation
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Expired - Lifetime
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JP2002049673A
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Japanese (ja)
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JP2003247222A (en
Inventor
良一 下倉
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Toa Corp
Toray Engineering Co Ltd
Penta Ocean Construction Co Ltd
Kabuki Construction Co Ltd
Honma Corp
Ohmoto Gumi Co Ltd
Original Assignee
Toa Corp
Penta Ocean Construction Co Ltd
Kabuki Construction Co Ltd
Toyo Construction Co Ltd
Honma Corp
Ohmoto Gumi Co Ltd
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Application filed by Toa Corp, Penta Ocean Construction Co Ltd, Kabuki Construction Co Ltd, Toyo Construction Co Ltd, Honma Corp, Ohmoto Gumi Co Ltd filed Critical Toa Corp
Priority to JP2002049673A priority Critical patent/JP3996407B2/en
Publication of JP2003247222A publication Critical patent/JP2003247222A/en
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Description

【0001】
【発明の属する技術分野】
本発明はダム湖、貯水池及び河川に形成された土砂の集積構造に関するものである。
【0002】
【従来の技術】
一般的に、ダム湖は水の流れがほとんどないため、濁水とともに流れ込んだウオッシュロードと呼ばれる微細粒土や浮遊砂などの土砂が湖底に堆積している。この土砂の堆積が多くなると貯水量が低下してダム本来の機能が発揮できなくなるため、種々の方法で浚渫が行われている。
【0003】
【発明が解決しようとする課題】
しかし、平均粒径が0.017mm程度のウオッシュロードと、粒径が0.15〜0.25mmの浮遊砂とは、薄い層として湖底全域にわたって堆積しているため、浚渫エリアが広範になって効率的な浚渫ができないという問題があった。
【0004】
本発明は上記のような問題に鑑みてなされたものであり、その目的は、土砂の効率的な浚渫ができる集積構造を提供することである。
【0005】
【課題を解決するための手段】
以上の課題を解決するための本発明の土砂の集積構造の要旨は、水が流れ込む流入斜面路の上流部から貯水底にかけて土砂用導流路が形成され、該土砂用導流路は流入斜面路の上流部に、流入斜面路の一部を塞ぐように横方向に突出した横導流堤と、該横導流堤の先端部から貯水底までの流入斜面路に沿って築堤された縦導流堤とからなることを特徴とする。また横導流堤の上流側には流入斜面路を横断した分流堤が築堤されたことを含む。また土砂用導流路の流出口付近には土砂用集積部が形成され、該土砂用集積部は流出口付近の土砂用集積エリアと、縦導流堤の先端から適宜離れた箇所に流出口を横切るように築堤された堰堤とにより形成されたことを含む。また土砂用導流路は上流側から下流側にかけて漸次幅広に形成されたことを含む。また縦導流堤の先端部には流出口と反対方向に伸びた堰堤が築堤されたことを含む。また縦導流堤にはシルトプロテクターが形成されたことを含む。さらに横導流堤、縦導流堤は湖底から排出された堆積土で築堤されたことを含むものである。
【0006】
ウオッシュロードや浮遊砂を含んだ濁水が土砂用導流路を通ってダム湖(または貯水池)に流れ込むため、ウオッシュロードや浮遊砂などの土砂をダム湖の所定箇所、すなわちダム湖全体ではなくある一部の箇所に集積させることができる。また、これらの土砂をダム湖の形状に合わせて、最も効率的な浚渫ができる箇所に集積させることができる。また分流堤により大きな石や木の枝などをせき止めることができる。濁水とともにダム湖に流れ込んだウオッシュロードや浮遊砂などの土砂を湖底における土砂用集積エリアに集積させることができる。また上流側から下流側にかけて漸次幅広に形成された土砂用導流路によって濁水を上流側から下流にかけて漸次遅く流することがができるので、ウオッシュロードや浮遊砂などの土砂を土砂用集積エリアに集積させることができる。また縦導流堤の先端部に流出口と反対方向に設けた堰堤より、ウオッシュロードや浮遊砂などの土砂を拡散させずに土砂用集積エリアに集積することができる。湖底から排出された堆積土で縦導流堤および堰堤が築堤されたことにより、堆積土の有効利用が図れる。ウオッシュロードや浮遊砂などの土砂をダム湖の一定箇所に集積させたことにより、一箇所で効率的な浚渫作業をすることができるとともに、効率的な浚渫作業をすることができる箇所にウオッシュロードや浮遊砂などの土砂を集積することができる。
【0007】
【発明の実施の形態】
以下、本発明の土砂の集積構造(以下集積構造という)について図面に基づいて説明する。各実施の形態において同じ構成は同じ符号を付して説明し、異なった構成にのみ異なった符号を付して説明する。この集積構造はダム湖、貯水池および河川に形成されるものであるが、以下の実施の形態においては、ダム湖に形成された集積構造について説明する。
【0008】
図1および2は第1の実施の形態の集積構造1を示したものである。この集積構造1はダム湖2に水を流し込む流入斜面路3に、ウオッシュロードや浮遊砂などの土砂を含んだ濁水を流す土砂用導流路(以下導流路という)4と、この導流路4の流出口付近に形成された土砂用集積部(以下集積部という)5とから構成されている。また、上記のウオッシュロードは平均粒径が17μ程度の微細粒土をいい、浮遊砂は粒径が0.15〜0.25mmの土砂をいう。
【0009】
導流路4は流入斜面路3の分流堤6の下流側に設けた横導流堤7と、該横導流堤7の先端部から湖底までの流入斜面路3に築堤された縦導流堤8とから構成されている。この横導流堤7および縦導流堤8は湖底から排出された堆積土により築堤されたものであり、前者は右岸(下流側に向かって)から左岸にかけて流入斜面路3の一部を塞ぐようにして築堤され、後者は横導流堤7の先端部から湖底にかけて導流路4が漸次広くなるように築堤されている。また縦導流堤8の水没部から先端部にかけての潜堤部にシルトプロテクター9が形成されている。
【0010】
このシルトプロテクター9は、図3に示すように、フロータ10aで吊り下げられたカーテン10bの下端部が潜堤部8aに固定されて形成されている。またフロータ10aとカーテン10bとの間に1m程度の隙間10cを設けることにより、湖内と導流路4との水位差によってシルトプロテクター9に作用する力を低減させている。
【0011】
また導流路4は、図1において左岸側に形成されているが、左右どちらかに形成するかは、ダム湖2の水理特性や地形特性などを考慮してきめられる。さらに流入斜面路3の水深が浅い場合は、シルトプロテクター9のみ、もしくは縦導流堤8のみで導流路4を形成することもできる。
【0012】
このように形成された導流路4は自然の河川と同じように、ウオッシュロードや浮遊砂などの土砂を含んだ濁水12が上流側から下流側にかけて漸次ゆっくりと流れ、河口に相当する流出口13付近で流れが止まるようになっている。
【0013】
一方、流出口13付近における集積部5は、土砂用集積エリア(以下集積エリアという)14と、湖底から排出された堆積土によって築堤された堰堤15、16とから構成されている。このように集積エリア14の周囲に形成された堰堤15、16によって流出口付近には窪み、すなわち集積部5が形成されている。したがって、分流堤6で大きな石などと分別されたウオッシュロードや浮遊砂などの土砂を含んだ濁水12は、導流路4からダム湖2に流れ込むことにより、前側の堰堤15で留められるとともに、後側の堰堤16で他に拡散されず、ここに土砂が沈殿するようになっている。
【0014】
図4および5は第2の実施の形態の集積構造17を示したものである。この集積構造17は集積部5をダム湖2の地形を利用して、ウオッシュロードや浮遊砂などの土砂が集積しやすい窪み部に形成したことが特徴であり、流出口13付近における自然に形成された突起部18が前側の堰堤15の代わりとなって、後側の堰堤16とともに集積部5を形成している。このように集積構造17は、ダム湖2の地形を利用して集積部5を形成した以外は第1の実施の形態の集積構造1と同じ構成である。したがって、前記と同様に、分流堤6で大きな石などと分別された濁水12は、導流路4からダム湖2に流れ込んで、突起部18で留められ、かつ後側の堰堤16で他に拡散しないようになっている。
【0015】
【発明の効果】
ウオッシュロードや浮遊砂などの土砂を含んだ濁水が導流路を通ってダム湖に流れ込むため、土砂をダム湖の所定箇所、すなわちダム湖全体ではなく、ある一定の箇所に集積させることができる。
【0016】
ウオッシュロードや浮遊砂などの土砂をダム湖の形状に合わせて、最も効率的な浚渫ができる箇所に集積することができる。
【0017】
分流堤によって大きな石や木の枝などをせき止めることができる。
【0018】
濁水とともにダム湖に流れ込んだウオッシュロードや浮遊砂などの土砂を湖底の集積エリアに集積させることができる。
【0019】
上流側から下流側にかけて漸次幅広に形成された導流路によって濁水を上流側から下流にかけて漸次遅く流することがができるので、ウオッシュロードや浮遊砂などの土砂を集積エリアに集積させることができる。
【0020】
堰堤よってウオッシュロードや浮遊砂などの土砂を拡散させずに集積エリアに集めることができる。
【0021】
湖底から排出された堆積土で横横導流堤、縦横導流堤および堰堤が築堤されたことにより、堆積土の有効利用が図れる。
【0022】
ウオッシュロードや浮遊砂などの土砂をダム湖の一定箇所に集積させることができるため、効率的な浚渫作業をすることができるとともに、効率的な浚渫作業をすることができる箇所に土砂を集積することができる。
【図面の簡単な説明】
【図1】第1の実施の形態の集積構造の平面図である。
【図2】図1の縦断面図である。
【図3】(1)は図1の横断面図、(2)はシルトプロテクターの正面図である。
【図4】第2の実施の形態の集積構造の平面図である。
【図5】図2の断面図である。
【符号の説明】
1、17 集積構造
2 ダム湖
3 流入斜面路
4 導流路
5 集積部
6 分流堤
7 横導流堤
8 縦導流堤
9 シルトプロテクター
10a フロータ
10b カーテン
10c 隙間
12 濁水
13 流出口
14 集積エリア
15、16 堰堤
18 突起部
[0001]
BACKGROUND OF THE INVENTION
The present invention relates to an accumulation structure of earth and sand formed in a dam lake, a reservoir and a river.
[0002]
[Prior art]
In general, there is almost no flow of water in the dam lake, so sediments such as fine-grained soil called floating road and floating sand that have flowed along with muddy water accumulate on the bottom of the lake. When this amount of sediment is increased, the amount of stored water decreases and the original function of the dam cannot be exhibited, so dredging is performed by various methods.
[0003]
[Problems to be solved by the invention]
However, the wash road with an average particle size of about 0.017 mm and suspended sand with a particle size of 0.15 to 0.25 mm are deposited as a thin layer over the entire lake bottom, so the dredging area becomes wide. There was a problem that efficient dredging was not possible.
[0004]
The present invention has been made in view of the above problems, and an object of the present invention is to provide an integrated structure capable of efficient dredging of earth and sand.
[0005]
[Means for Solving the Problems]
The gist of the sediment accumulation structure of the present invention for solving the above-described problems is that an earth-and-sand channel is formed from the upstream portion of the inflow slope channel through which water flows to the bottom of the reservoir, and the earth-and-sand channel is inflow slope. A horizontal dike projecting laterally so as to block a part of the inflow slope road, and a vertical dike constructed along the inflow slope road from the tip of the horizontal dike to the reservoir bottom It consists of a dike. In addition, it included that a dike that crossed the inflow slope was built upstream of the horizontal dike. In addition, a sediment accumulation part is formed near the outflow port of the earth and sand conduit, and the sediment accumulation part is located at an appropriate distance from the sediment accumulation area near the outflow port and the tip of the longitudinal dike. Including the formation of a dam built across the river. In addition, the earth and sand guide channel is formed so as to be gradually widened from the upstream side to the downstream side. It also includes that a dam extending in the opposite direction to the outlet was built at the tip of the longitudinal dike. It also includes the formation of silt protectors on the longitudinal dike. Further Yokoshirube flow Tsutsumi, Tateshiruberyu Tsutsumi are those comprising been embankments in sediment discharged from the bottom of the lake.
[0006]
Since muddy water containing wash load and suspended sand flows into the dam lake (or reservoir) through the earth and sand conduit, there is no sediment such as wash load and suspended sand in the dam lake, that is, not the entire dam lake. It can be accumulated in some places. Moreover, these earth and sand can be accumulated in the place where the most efficient dredging can be made according to the shape of the dam lake. In addition, a large dike can be used to block large stones and tree branches. It is possible to accumulate earth and sand such as wash roads and floating sand that flowed into the dam lake together with muddy water in the sediment accumulation area at the bottom of the lake. In addition, turbid water can flow slowly from the upstream side to the downstream side by the earth and sand guide channel formed gradually wider from the upstream side to the downstream side, so sediment such as wash load and floating sand can be put into the sediment accumulation area. Can be integrated. In addition, from the dam provided at the tip of the longitudinal dike in the direction opposite to the outlet, it is possible to accumulate sediment in the sediment accumulation area without diffusing earth and sand such as wash load and floating sand. The sedimentary soil discharged from the bottom of the lake is used to build up the vertical dike and dam, so that the sediment can be effectively used. By collecting earth and sand such as wash roads and suspended sand at a certain location in the dam lake, it is possible to perform efficient dredging work at one place and wash roads where efficient dredging work can be performed. And sediment such as floating sand.
[0007]
DETAILED DESCRIPTION OF THE INVENTION
Hereinafter, an earth and sand accumulation structure (hereinafter referred to as an accumulation structure) according to the present invention will be described with reference to the drawings. In each embodiment, the same components are described with the same reference numerals, and only different components are described with different reference numerals. This accumulation structure is formed in a dam lake, a reservoir, and a river. In the following embodiment, an accumulation structure formed in a dam lake will be described.
[0008]
1 and 2 show an integrated structure 1 of the first embodiment. The integrated structure 1 includes an inflow slope 3 for flowing water into a dam lake 2, an earth-and-sand channel (hereinafter referred to as a channel) 4 for flowing muddy water containing earth and sand such as a wash road and floating sand, and the channel It is composed of an earth and sand accumulating portion (hereinafter referred to as an accumulating portion) 5 formed in the vicinity of the outlet of the passage 4. In addition, the above wash load refers to fine-grained soil having an average particle size of about 17 μm, and suspended sand refers to soil having a particle size of 0.15 to 0.25 mm.
[0009]
The diversion channel 4 includes a horizontal diversion channel 7 provided on the downstream side of the diversion dike 6 of the inflow slope channel 3 and a vertical diversion channel built on the inflow ramp channel 3 from the tip of the horizontal diversion channel 7 to the bottom of the lake. It is composed of the bank 8. The horizontal dike 7 and the vertical dike 8 are constructed by sedimentary soil discharged from the bottom of the lake. The former blocks a part of the inflow slope 3 from the right bank (toward the downstream side) to the left bank. In this way, the latter is constructed so that the conduit 4 gradually becomes wider from the front end of the lateral conduit 7 to the bottom of the lake. Further, a silt protector 9 is formed in a submerged dike portion from the submerged portion to the tip portion of the longitudinal dike 8.
[0010]
As shown in FIG. 3, the silt protector 9 is formed by fixing a lower end portion of a curtain 10b suspended by a floater 10a to a submerged dike portion 8a. Further, by providing a gap 10c of about 1 m between the floater 10a and the curtain 10b, the force acting on the silt protector 9 due to the water level difference between the inside of the lake and the guide channel 4 is reduced.
[0011]
Further, although the guide channel 4 is formed on the left bank side in FIG. 1, whether it is formed on the left or right side is determined in consideration of the hydraulic characteristics, topographic characteristics, etc. of the dam lake 2. Furthermore, when the water depth of the inflow slope 3 is shallow, the conduit 4 can be formed only by the silt protector 9 or by the longitudinal dike 8 alone.
[0012]
The channel 4 formed in this way, like a natural river, the muddy water 12 containing earth and sand such as a wash road and floating sand gradually flows from the upstream side to the downstream side, and the outlet corresponding to the estuary. The flow stops at around 13.
[0013]
On the other hand, the accumulation part 5 in the vicinity of the outlet 13 is composed of a sediment accumulation area (hereinafter referred to as an accumulation area) 14 and dams 15 and 16 constructed by sedimentary soil discharged from the lake bottom. In this way, the dams 15 and 16 formed around the accumulation area 14 form depressions in the vicinity of the outlet, that is, the accumulation portion 5. Therefore, the muddy water 12 containing the wash load and the floating sand separated from the large stones at the diversion bank 6 flows into the dam lake 2 from the channel 4 and is retained by the front dam 15. The other side is not diffused by the backside dam 16, and earth and sand settle here.
[0014]
4 and 5 show the integrated structure 17 of the second embodiment. The accumulation structure 17 is characterized in that the accumulation portion 5 is formed in a hollow portion where earth and sand such as a wash road and floating sand easily accumulate using the terrain of the dam lake 2 and is formed naturally in the vicinity of the outlet 13. The projection 18 thus formed replaces the front dam 15 and forms the accumulation portion 5 together with the rear dam 16. As described above, the accumulation structure 17 has the same configuration as the accumulation structure 1 of the first embodiment except that the accumulation portion 5 is formed using the topography of the dam lake 2. Therefore, as described above, the muddy water 12 separated from a large stone or the like by the diversion dike 6 flows into the dam lake 2 from the channel 4 and is stopped by the protrusions 18, and is otherwise separated by the rear dam 16. It does not spread.
[0015]
【The invention's effect】
Since muddy water containing earth and sand such as wash road and floating sand flows into the dam lake through the channel, the earth and sand can be accumulated at a certain place in the dam lake, not the whole dam lake. .
[0016]
It is possible to accumulate earth and sand such as wash roads and floating sand in the most efficient dredging area according to the shape of the dam lake.
[0017]
A large dike can be used to block large stones and tree branches.
[0018]
It is possible to accumulate earth and sand such as wash road and floating sand that flowed into the dam lake together with muddy water in the accumulation area of the lake bottom.
[0019]
Muddy water can flow gradually from the upstream side to the downstream side by the guide channel formed gradually wider from the upstream side to the downstream side, so that sediment such as wash load and floating sand can be accumulated in the accumulation area. .
[0020]
The dam can collect earth and sand such as wash roads and suspended sand in the accumulation area without spreading.
[0021]
The sedimentary soil discharged from the lake bottom can be used effectively because the horizontal and horizontal dike, vertical and horizontal dike and the dam are built.
[0022]
Since sediments such as wash roads and suspended sand can be accumulated at certain locations in the dam lake, sediment can be accumulated at locations where efficient dredging can be performed, as well as efficient dredging. be able to.
[Brief description of the drawings]
FIG. 1 is a plan view of an integrated structure according to a first embodiment.
FIG. 2 is a longitudinal sectional view of FIG.
3A is a cross-sectional view of FIG. 1, and FIG. 3B is a front view of a silt protector.
FIG. 4 is a plan view of an integrated structure according to a second embodiment.
FIG. 5 is a cross-sectional view of FIG.
[Explanation of symbols]
DESCRIPTION OF SYMBOLS 1, 17 Accumulation structure 2 Dam lake 3 Inflow slope road 4 Conduction flow path 5 Accumulation part 6 Split dike 7 Lateral dike 8 Vertical dike 9 Silt protector 10a Float 10b Curtain 10c Crevice 12 Muddy water 13 Outlet 14 Accumulation area 15 , 16 Weir 18 Projection

Claims (7)

水が流れ込む流入斜面路の上流部から貯水底にかけて土砂用導流路が形成され、該土砂用導流路は流入斜面路の上流部に、流入斜面路の一部を塞ぐように横方向に突出した横導流堤と、該横導流堤の先端部から貯水底までの流入斜面路に沿って築堤された縦導流堤とからなることを特徴とする土砂の集積構造。  An earth and sand channel is formed from the upstream part of the inflow slope path where water flows into the reservoir bottom, and the earth and sand channel is formed in the lateral direction so as to block a part of the inflow slope path in the upstream part of the inflow slope path. An earth and sand accumulation structure characterized by comprising a projecting horizontal dike and a vertical dike built along an inflow slope from the tip of the horizontal dike to the reservoir bottom. 横導流堤の上流側には流入斜面路を横断した分流堤が築堤されたことを特徴とする請求項1に記載の土砂の集積構造。  2. The earth and sand accumulation structure according to claim 1, wherein a diversion bank crossing the inflow slope road is built on the upstream side of the horizontal diversion bank. 土砂用導流路の流出口付近には土砂用集積部が形成され、該土砂用集積部は流出口付近の土砂用集積エリアと、縦導流堤の先端から適宜離れた箇所に流出口を横切るように築堤された堰堤とにより形成されたことを特徴とする請求項1または2に記載の土砂の集積構造。  A sediment accumulation part is formed near the outlet of the earth and sand conduit, and the sediment accumulation part has an outlet at an appropriate distance from the tip of the longitudinal dike and the sediment accumulation area near the outlet. 3. The earth and sand accumulation structure according to claim 1, wherein the earth and sand accumulation structure is formed by a dam built so as to cross. 土砂用導流路は上流側から下流側にかけて漸次幅広に形成されたことを特徴とする請求項1〜3のいずれかに記載の土砂の集積構造。  The earth and sand accumulation structure according to any one of claims 1 to 3, wherein the earth and sand guide channel is formed to be gradually wider from the upstream side to the downstream side. 縦導流堤の先端部には流出口と反対方向に伸びた堰堤が築堤されたことを特徴とする請求項1〜4のいずれかに記載の土砂の集積構造。  The sediment accumulation structure according to any one of claims 1 to 4, wherein a dam extending in a direction opposite to the outflow port is built at a front end portion of the longitudinal dike. 縦導流堤にはシルトプロテクターが形成されたことを特徴とする請求項1〜5のいずれかに記載の土砂の集積構造。  The sediment structure according to any one of claims 1 to 5, wherein a silt protector is formed on the longitudinal dike. 横導流堤、縦導流堤は湖底から排出された堆積土で築堤されたことを特徴とする請求項1〜6のいずれかに記載の土砂の集積構造。Yokoshiruberyutsutsumi, Tateshiruberyu Tsutsumi sediment integrated structure according to any one of claims 1 to 6, characterized in that it is the embankment in sediment discharged from the bottom of the lake.
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