JPH0627131A - Method and apparatus for measuring flow direction and flow velocity of underground water - Google Patents
Method and apparatus for measuring flow direction and flow velocity of underground waterInfo
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- JPH0627131A JPH0627131A JP18233092A JP18233092A JPH0627131A JP H0627131 A JPH0627131 A JP H0627131A JP 18233092 A JP18233092 A JP 18233092A JP 18233092 A JP18233092 A JP 18233092A JP H0627131 A JPH0627131 A JP H0627131A
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- Prior art keywords
- pipe
- flow direction
- packer
- groundwater
- flow
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Abstract
Description
【0001】[0001]
【産業上の利用分野】この発明は熱中性子法、熱量法あ
るいは電位差法等による地下水流向、流速計地下水の流
動方向、流速を測定する方法および装置に関する。BACKGROUND OF THE INVENTION 1. Field of the Invention The present invention relates to a method and an apparatus for measuring a groundwater flow direction, a velocity meter groundwater flow direction and a flow velocity by a thermal neutron method, a calorimetric method or a potentiometric method.
【0002】[0002]
【従来技術】建設工事等においては、伏流水をはじめ、
地下水の流動方向、流速を地層別に測定する必要があ
る。この測定方法の一つの手段として特公昭60−27
388号で提案されている熱中性子検出計を地下水流
向、流速計として用いる熱中性子法が知られている。2. Description of the Related Art In construction work, including underground water,
It is necessary to measure the flow direction and velocity of groundwater for each stratum. As one means of this measuring method, Japanese Examined Patent Publication No. 60-27
A thermal neutron method using the thermal neutron detector proposed in No. 388 as a groundwater flow direction and velocity meter is known.
【0003】熱中性子検出計により測定するには、対象
となる地盤に竪孔を穿孔し、この竪孔内にストレーナを
備えた測定用パイプを設置し、このパイプ内に熱中性子
検出計を挿入し、その周辺に中性子吸収断面積が大き
い、例えばほう素水溶液などのトレーサーを送給する。
トレーサーは地下水の流れに支配されて流れ、稀釈され
るので、各方位の熱中性子の計数率を熱中性子検出計で
検出することにより、トレーサーの濃度が測定でき、こ
の値から地下水の流向、流速を知ることができる。To measure with a thermal neutron detector, a vertical hole is drilled in the target ground, a measuring pipe equipped with a strainer is installed in the vertical hole, and the thermal neutron detector is inserted into this pipe. Then, a tracer having a large neutron absorption cross-section, for example, an aqueous solution of boron is fed to the periphery of the tracer.
Since the tracer flows under the control of the groundwater flow and is diluted, the concentration of the tracer can be measured by detecting the counting rate of thermal neutrons in each direction with a thermal neutron detector. You can know.
【0004】地下水の流向、流速を測定する手段として
は、上記の熱中性子法のほか、熱をトレーサーとする熱
量法、蒸留水をトレーサーとする電位差法が提案されて
いる。いずれの方法も竪孔内に設置した測定パイプ内に
流向、流速計を挿入し、流向、流速を測定する点では同
じである。As means for measuring the flow direction and flow velocity of groundwater, in addition to the above thermal neutron method, a calorimetric method using heat as a tracer and a potentiometric method using distilled water as a tracer have been proposed. Both methods are the same in that the flow direction and the flow velocity meter are inserted into the measuring pipe installed in the vertical hole and the flow direction and the flow velocity are measured.
【0005】[0005]
【発明が解決しようとする課題】ところが、被圧水地盤
では穿孔した竪孔内に縦方向の地下水の流れが生じ、流
向、流速の測定が困難となる。また、複数の被圧帯水層
が重なって存在する場合は、被圧帯水層の数の測定用竪
孔を穿孔して測定しなければならなかった。このため
に、調査測定に長い期間、広いスペースが必要となり、
コスト高となった。However, in the ground under pressure, vertical groundwater flows in the vertical holes, which makes it difficult to measure the flow direction and flow velocity. When a plurality of confined aquifers overlap each other, it is necessary to perforate the measurement vertical holes to measure the number of confined aquifers. This requires a large space for survey measurements for a long period of time,
The cost is high.
【0006】この発明は上記問題点に着目しなされたも
のである。その目的は複数の被圧帯水層がある地盤であ
っても、単一の竪孔を穿孔するのみで、正確に地下水の
流向、流速を測定できる方法、およびこの測定方法等で
用い好適な測定装置を提案するにある。The present invention has been made in view of the above problems. Even if the purpose is ground with multiple confined aquifers, it is suitable to use in a method that can accurately measure the flow direction and flow velocity of groundwater simply by drilling a single vertical hole, and this measurement method, etc. To propose a measuring device.
【0007】[0007]
【課題を解決するための手段】請求項1の地下水の流
向、流速の測定方法は地下水の流向、流速を地下水流向
・流速計を用い測定する方法であって、不透水層で仕切
られた複数の被圧帯水層が重なり存在する被圧帯水地盤
に竪孔を穿孔し、この竪孔内にストレーナ部を有する測
定用パイプを設置し、不透水層位置において竪孔とパイ
プとの間隙を止水材を填充して閉塞し、地下水流向・流
速計計と空気圧により膨張あるいは収縮する止水パッカ
が取付けてあるロッドをパイプ内に挿入し、止水パッカ
を膨張してパイプとロッド間の間隙を閉塞し不透水層で
仕切られた上下の被圧帯水層間の地下水の流れを止めて
流向、流速を測定し、止水パッカを収縮してロッドを上
下方向に移動させ複数の被圧帯水層の流向、流速を測定
することを特徴とする。請求項3の地下水の流向、流速
の測定装置は、地盤に穿孔した竪孔内にストレーナを備
えた測定用パイプを挿入し、このパイプ内に地下水流向
・流速計をロッドに取付けて挿入し地盤内の地下水の流
向、流速を測定する装置において、地下水流向・流速計
の上方および下方の両方あるいは片方の位置のロッドに
止水パッカを配してなり、この止水パッカは筒形をなし
ロッドを取り囲み、同心をなした内槽パッカと外槽パッ
カに隔壁で仕切られ、内外槽パッカはそれぞれ空気圧で
膨張あるいは収縮して、ロッド表面およびパイプ内面に
圧接あるいは脱離が自在となしてあることを特徴とす
る。A method for measuring the flow direction and flow velocity of groundwater according to claim 1 is a method for measuring the flow direction and flow velocity of groundwater by using a groundwater flow direction / velocimeter, and a plurality of layers are separated by an impermeable layer. A vertical hole is drilled in the confined aquifer where the confined aquifers overlap, and a measurement pipe with a strainer is installed in the vertical hole, and the gap between the vertical hole and the pipe at the impermeable layer position. Is filled with water-stopping material and blocked, and a rod with a groundwater flow direction / velocimeter and a water-stopper that expands or contracts due to air pressure is inserted into the pipe, and the water-stopper is expanded to expand the space between the pipe and the rod. Of the groundwater between the upper and lower confined aquifers, which are closed by the impermeable layer and block the gap, and measure the flow direction and flow velocity. Characterized by measuring the flow direction and velocity of the aquifer . The groundwater flow direction / velocity measuring device according to claim 3 is a ground pipe in which a measurement pipe equipped with a strainer is inserted into a vertical hole formed in the ground, and the groundwater flow direction / velocimeter is attached to the rod and inserted into the ground. In a device for measuring the flow direction and velocity of groundwater inside, a water stop packer is arranged on the rod above and / or below the ground water flow direction / velocity meter, and this water stop packer has a cylindrical shape. The inner and outer tank packers, which are concentric with each other, are partitioned by a partition wall, and the inner and outer tank packers are respectively expanded or contracted by air pressure so that they can be pressed into or released from the rod surface and the pipe inner surface. Is characterized by.
【0008】[0008]
【実施例】この実施例が測定の対象とする地盤は、図1
に示すように、第1、第2、第3の被圧帯水層1−1、
1−2、1−3が重なり存在する被圧帯水地盤であり、
帯水層間は不透水層2−12および2−23で仕切ら
れ、被圧帯水層1−1、1−2、1−3の地下水層3−
1、3−2、3−3は下層のものが順に高くなってい
る。EXAMPLE The ground to be measured in this example is shown in FIG.
As shown in, the first, second, and third confined aquifers 1-1,
1-2, 1-3 is a confined aquifer with overlapping layers,
The aquifers are separated by impermeable layers 2-12 and 2-23, and the aquifers 1-1, 1-2, 1-3 are groundwater layers 3-.
As for 1, 3-2 and 3-3, the lower layers are higher in order.
【0009】この地盤の地下水の流向、流速は以下の手
順で測定する。先ず図1に示すように、地盤をボーリン
グして1つの竪孔4を穿孔し、この竪孔4内に側面に透
孔のストレーナ部5を有する測定用パイプ6を挿入設置
する。竪孔4の外径は、パイプ6と孔壁との間にフィル
ター材や止水材を充分に詰込みできる程度に、パイプ6
の外径より大きくしてある(例えば、パイプφ80mm,
竪孔φ150mm)。The flow direction and flow velocity of groundwater on this ground are measured by the following procedure. First, as shown in FIG. 1, the ground is bored to form a single vertical hole 4, and a measuring pipe 6 having a through-hole strainer portion 5 is inserted and installed in the vertical hole 4. The outer diameter of the vertical hole 4 is such that the filter material and the water blocking material can be sufficiently packed between the pipe 6 and the hole wall.
Larger than the outer diameter of the pipe (for example, pipe φ80 mm,
Vertical hole φ150 mm).
【0010】次に不透水層2−12、2−23にあたる
位置において、孔壁とパイプとの間隙に止水材7(ベン
トナイトなど)を填充して閉塞し、孔壁とパイプとの間
の地下水の流れを止める。なお、止水材7を填充する位
置のパイプは盲パイプ6'となしてある。また、ストレー
ナ部5以外のパイプ部分において孔壁との間に止水材を
填充してもよい。Next, at the positions corresponding to the impermeable layers 2-12 and 2-23, the gap between the hole wall and the pipe is filled with water blocking material 7 (bentonite or the like) to close the gap, and the gap between the hole wall and the pipe is closed. Stop the flow of groundwater. The pipe at the position where the waterproof material 7 is filled is a blind pipe 6 '. Further, a water blocking material may be filled between the hole wall and the pipe portion other than the strainer portion 5.
【0011】この竪孔4内に熱中性子検出計8からなる
地下水流向・流速計を、ロッド9に取付けて挿入する。
この際、検出計8の上方および下方位置に止水パッカ1
0,10を取付けておく。熱中性子検出計8は、中性子
源、熱中性子検出管、およびほう素水溶液トレーサー注
入孔を備え、地上に設けたトレーサー注入装置、デジタ
ルカウントレートメータ等(図示せず)と組合せて地下
水の流向、流速を測定する。A groundwater flow direction / velocimeter composed of a thermal neutron detector 8 is attached to a rod 9 and inserted into the vertical hole 4.
At this time, the water blocking packer 1 should be placed above and below the detector 8.
Install 0 and 10. The thermal neutron detector 8 comprises a neutron source, a thermal neutron detector tube, and a boron aqueous solution tracer injection hole, and is combined with a tracer injection device, a digital count rate meter, etc. (not shown) provided on the ground, and the flow direction of groundwater, Measure the flow rate.
【0012】止水パッカ10は図2に示すごとく円筒形
をなし断面円形のロッド9を取り囲み、同心をなす内槽
パッカ10−1と外槽パッカ10−2に隔壁11で仕切
られている。内、外槽パッカ10−1、10−2はそれ
ぞれ圧縮空気の送給口12を備え、地上に設置してある
パッカ作動装置(図示せず)との間に圧気パイプが配設
してあり、別個に圧気の送給を受けて膨張、あるいは減
圧することにより収縮する。すなわち、内外槽パッカ1
0−1、10−2は圧気の送給により膨張してそれぞ
れ、ロッド9表面およびパイプ6内面に圧接して間隙を
閉塞し、同時に相互間を固定し、圧気を排出し収縮し、
ロッド9表面およびパイプ6内面から脱離し、相互間の
間隙を開放すると同時に相互間の移動が可能となる。As shown in FIG. 2, the water blocking packer 10 surrounds a rod 9 having a cylindrical shape and a circular cross section, and is partitioned by a partition wall 11 into a concentric inner tank packer 10-1 and an outer tank packer 10-2. The inner and outer tank packers 10-1 and 10-2 each have a compressed air supply port 12, and a compressed air pipe is provided between the packer operating device (not shown) installed on the ground. , Contracts by being separately supplied with compressed air and expanded or decompressed. That is, the inner and outer tank packer 1
0-1 and 10-2 are inflated by the feeding of the compressed air to press the rod 9 surface and the inner surface of the pipe 6 respectively to close the gap, and at the same time, fix each other, discharge the compressed air and contract.
The rod 9 is detached from the surface of the rod 9 and the inner surface of the pipe 6 to open the gap between them, and at the same time, the mutual movement becomes possible.
【0013】竪孔4内に検出計8を挿入するときは内槽
パッカ10−1を膨張させてロッド9と止水パッカ10
を固定した状態とする。固定する位置はパイプ6外周に
填充した止水材7にあたる位置とする。所定深度に達し
た時点で外槽パッカ10−2を膨張させ、止水材7を填
充した不透水層2−12、2−23位置において、パイ
プ6と止水パッカ10とを固定した後、内槽パッカ10
−1を収縮させてロッド9、すなわち検出計8の移動を
自由となし、測定深度に移動させる。When inserting the detector 8 into the vertical hole 4, the inner tank packer 10-1 is expanded to expand the rod 9 and the water blocking packer 10.
Is fixed. The fixing position is a position corresponding to the water blocking material 7 filled in the outer circumference of the pipe 6. After reaching the predetermined depth, the outer tank packer 10-2 is expanded to fix the pipe 6 and the water blocking packer 10 at the impermeable layers 2-12 and 2-23 positions filled with the water blocking material 7, Inner tank packer 10
-1 is contracted so that the rod 9, that is, the detector 8 is freely moved, and is moved to the measurement depth.
【0014】すなわち、ロッド,止水パッカ、流向・流
速計本体を移動するときは、外槽パッカの空気を減圧
し、止水パッカを測定用パイプに固定し、その間を深度
ごとに流向・流速を求めようとする場合には止水パッカ
ーの外槽パッカを加圧し、内槽パッカの空気を減圧させ
る。That is, when moving the rod, the water shut-off packer, and the flow direction / velocity meter body, the air in the outer tank packer is depressurized, the water shut-up packer is fixed to the measuring pipe, and the flow direction / velocity is varied depending on the depth. In order to obtain, the outer tank packer of the water blocking packer is pressurized and the air in the inner tank packer is depressurized.
【0015】検出計8の測定位置が決まったら、外槽パ
ッカ10−2はそのままにして、内槽パッカ10−1を
膨張させてロッド9に密着させて間隙を閉塞する。孔壁
とパイプ6との間隙は止水材7で、パイプ6とロッド9
との間隙は膨張した内外槽パッカ10−1、10−2で
それぞれ閉塞され被圧帯水層1−1、1−2、1−3間
の縦方向の地下水の流れはなくなり、被圧帯水層1−2
の地下水の流向、流速の測定が可能となる。When the measuring position of the detector 8 is determined, the outer tank packer 10-2 is left as it is and the inner tank packer 10-1 is expanded and brought into close contact with the rod 9 to close the gap. The gap between the hole wall and the pipe 6 is a water blocking material 7, and the pipe 6 and the rod 9
The gap between and is closed by the expanded inner and outer tank packers 10-1 and 10-2, respectively, and the vertical groundwater flow between the pressurized aquifers 1-1, 1-2, and 1-3 disappears. Water layer 1-2
It becomes possible to measure the flow direction and flow velocity of groundwater.
【0016】この操作を繰返し、1つの竪孔4を用いて
第1あるいは第3被圧帯水層1−1、1−3の流向、流
速を測定する。なお、第1被圧帯水層1−1の測定に際
しては上部位置に取付けた止水パッカ10は不要とな
る。By repeating this operation, the flow direction and the flow velocity of the first or third pressure-bearing aquifers 1-1, 1-3 are measured using one vertical hole 4. In addition, in the case of measuring the first pressurized aquifer 1-1, the water blocking packer 10 attached at the upper position is unnecessary.
【0017】上記実施例の熱中性子検出計に代り、熱量
法あるいは電位差法の地下水流向・流速計を用いること
ができる。この場合も、ロッドに取付けた流向、流速計
の上下両方あるいは片方位置に止水パッカを配して、地
下水の縦方向の流れを止め、1つの竪孔を用いて複数の
被圧帯水層の流向、流速を測定できる。In place of the thermal neutron detector of the above embodiment, a calorimetric or potentiometric groundwater flow / velocimeter can be used. In this case as well, a water stop packer is installed at the flow direction attached to the rod, at the top and bottom of the current meter, or at one position to stop the vertical flow of groundwater and use a single pit to form multiple confined aquifers. The flow direction and flow velocity of can be measured.
【0018】[0018]
【発明の効果】この発明は以上の通りであり、この測定
方法によると複数の被圧帯水層がある地盤の地下水の流
向、流速を単一の竪孔を用いて能率よく測定できる。The present invention is as described above, and according to this measuring method, the flow direction and flow velocity of groundwater in the ground having a plurality of confined aquifers can be efficiently measured using a single vertical hole.
【0019】この測定装置は、地下水流向・流速計を取
付けたロッドの上方あるいは下方位置に配置した止水パ
ッカは、パイプとロッドとの間隙を閉塞あるいは開放
し、地下水の測定位置を自由に選択して固定でき、か
つ、地下水の縦方向の流れを止めることができるので、
複数の被圧帯水層が存在する地盤の地下水の流向、流速
を1つの竪孔で測定するのに好適である。In this measuring device, the water blocking packer arranged above or below the rod on which the groundwater flow direction / velocimeter is attached closes or opens the gap between the pipe and the rod, and freely selects the groundwater measuring position. Since it can be fixed and stopped the vertical flow of groundwater,
It is suitable for measuring the flow direction and flow velocity of groundwater in the ground where a plurality of confined aquifers exist, with one vertical hole.
【図1】実施例の地下水の流向、流速の測定方法を説明
する断面図である。FIG. 1 is a cross-sectional view illustrating a method for measuring a flow direction and a flow velocity of groundwater according to an embodiment.
【図2】図1の止水パッカ部分の拡大断面図である。FIG. 2 is an enlarged sectional view of a water blocking packer portion of FIG.
1…被圧帯水層、2…不透水層、3…地下水位、4…竪
孔、5…ストレーナ部、6…測定用パイプ、6’盲パイ
プ、7…止水材、8…熱中性子検出計、9…ロッド、1
0…止水パッカ、10−1…内槽パッカ、10−2…外
槽パッカ、11…隔壁、12…圧気の送給口。1 ... Confined aquifer, 2 ... Impermeable layer, 3 ... Groundwater level, 4 ... Vertical hole, 5 ... Strainer part, 6 ... Measuring pipe, 6'blind pipe, 7 ... Water blocking material, 8 ... Thermal neutron Detector, 9 ... Rod, 1
0 ... Water-stopper packer, 10-1 ... Inner tank packer, 10-2 ... Outer tank packer, 11 ... Partition wall, 12 ... Pressure air supply port.
Claims (3)
流速計を用い測定する方法であって、不透水層で仕切ら
れた複数の被圧帯水層が重なり存在する被圧帯水地盤に
竪孔を穿孔し、この竪孔内にストレーナ部を有する測定
用パイプを設置し、不透水層位置において竪孔とパイプ
との間隙を止水材を填充して閉塞し、地下水流向・流速
計と空気圧により膨張あるいは収縮する止水パッカが取
付けてあるロッドをパイプ内に挿入し、止水パッカを膨
張してパイプとロッド間の間隙を閉塞し不透水層で仕切
られた上下の被圧帯水層間の地下水の流れを止めて流
向、流速を測定し、止水パッカを収縮して、ロッドを上
下方向に移動させ複数の被圧帯水層の流向、流速を測定
することを特徴とする地下水の流向、流速の測定方法。1. The flow direction and flow velocity of groundwater are
It is a method of measuring using a current meter, and a pit is bored in the confined aquifer ground where a plurality of confined aquifers separated by impermeable layers overlap, and a strainer part is provided in this pit. A rod with a measuring pipe installed and a gap between the vertical hole and the pipe filled with a waterproof material at the impermeable layer position to block it, and a groundwater flow direction / velocimeter and a waterproof packing that expands or contracts by air pressure. Inserted into the pipe, expand the water stop packer to close the gap between the pipe and the rod, stop the flow of groundwater between the upper and lower pressurized aquifers separated by the impermeable layer, and measure the flow direction and velocity. A method for measuring groundwater flow direction and flow velocity, which comprises contracting a water-stopping packer and moving a rod in the vertical direction to measure the flow direction and flow velocity of a plurality of confined aquifers.
速計を用いることを特徴とする請求項1記載の地下水の
流向、流速の測定方法。2. The groundwater flow direction and flow velocity measuring method according to claim 1, wherein a groundwater flow direction / velocity meter comprising a thermal neutron detector is used.
えた測定用パイプを挿入し、このパイプ内に地下水流向
・流速計をロッドに取付けて挿入し地盤内の地下水の流
向、流速を測定する装置において、地下水流向・流速計
の上方および下方の両方あるいは片方の位置のロッドに
止水パッカを配してなり、この止水パッカは筒形をなし
ロッドを取り囲み、同心をなした内槽パッカと外槽パッ
カに隔壁で仕切られ、内外槽パッカはそれぞれ空気圧で
膨張あるいは収縮して、ロッド表面およびパイプ内面に
圧接、あるいは脱離が自在となしてあることを特徴とす
る地下水の流向、流速の測定装置。3. A measurement pipe equipped with a strainer is inserted into a vertical hole drilled in the ground, and a groundwater flow direction / velocity meter is attached to a rod in the pipe to measure the flow direction and velocity of groundwater in the ground. In this device, a water stop packer is arranged on the rod at one or both positions above and below the groundwater flow direction / velocimeter, and this water stop packer has a cylindrical shape and surrounds the rod to form a concentric inner tank. The packer and the outer tank packer are partitioned by a partition wall, and the inner and outer tank packers are expanded or contracted by air pressure, respectively, and can be pressed against the rod surface and the pipe inner surface, or can be detached freely. Flow velocity measuring device.
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
JP18233092A JP2586735B2 (en) | 1992-07-09 | 1992-07-09 | Measuring method and measuring device for groundwater flow direction and flow velocity |
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
JP18233092A JP2586735B2 (en) | 1992-07-09 | 1992-07-09 | Measuring method and measuring device for groundwater flow direction and flow velocity |
Publications (2)
Publication Number | Publication Date |
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JPH0627131A true JPH0627131A (en) | 1994-02-04 |
JP2586735B2 JP2586735B2 (en) | 1997-03-05 |
Family
ID=16116425
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Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
JP18233092A Expired - Fee Related JP2586735B2 (en) | 1992-07-09 | 1992-07-09 | Measuring method and measuring device for groundwater flow direction and flow velocity |
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JP (1) | JP2586735B2 (en) |
Cited By (2)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
JP2007309712A (en) * | 2006-05-17 | 2007-11-29 | Kajima Corp | Method of evaluating ground water flow |
CN113739844A (en) * | 2021-08-02 | 2021-12-03 | 重庆交通大学 | Dilution method based underground water layering monitoring device and monitoring method |
Citations (3)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
JPS5510548A (en) * | 1978-07-10 | 1980-01-25 | Kajima Corp | Method and apparatus for measurment of flow speed and direction of ground water |
JPS61161760U (en) * | 1985-03-29 | 1986-10-07 | ||
JPS62198782A (en) * | 1986-02-27 | 1987-09-02 | Taisei Kiso Sekkei Kk | Method for measuring extremely slow velocity and direction of flow of ground water |
-
1992
- 1992-07-09 JP JP18233092A patent/JP2586735B2/en not_active Expired - Fee Related
Patent Citations (3)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
JPS5510548A (en) * | 1978-07-10 | 1980-01-25 | Kajima Corp | Method and apparatus for measurment of flow speed and direction of ground water |
JPS61161760U (en) * | 1985-03-29 | 1986-10-07 | ||
JPS62198782A (en) * | 1986-02-27 | 1987-09-02 | Taisei Kiso Sekkei Kk | Method for measuring extremely slow velocity and direction of flow of ground water |
Cited By (3)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
JP2007309712A (en) * | 2006-05-17 | 2007-11-29 | Kajima Corp | Method of evaluating ground water flow |
CN113739844A (en) * | 2021-08-02 | 2021-12-03 | 重庆交通大学 | Dilution method based underground water layering monitoring device and monitoring method |
CN113739844B (en) * | 2021-08-02 | 2024-04-16 | 重庆交通大学 | Underground water layering monitoring device and method based on dilution method |
Also Published As
Publication number | Publication date |
---|---|
JP2586735B2 (en) | 1997-03-05 |
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