CN201156028Y - Pneumatic water head excitation device for drilling oscillating permeability coefficient test - Google Patents
Pneumatic water head excitation device for drilling oscillating permeability coefficient test Download PDFInfo
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- CN201156028Y CN201156028Y CNU2008200309829U CN200820030982U CN201156028Y CN 201156028 Y CN201156028 Y CN 201156028Y CN U2008200309829 U CNU2008200309829 U CN U2008200309829U CN 200820030982 U CN200820030982 U CN 200820030982U CN 201156028 Y CN201156028 Y CN 201156028Y
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Abstract
本实用新型是钻孔振荡式渗透系数取值试验气压式水头激发装置,其结构是在进气管上装有减压阀、进气阀门,进气阀门的出气口接入密封腔体,密封腔体上装有井内压力显示表、电缆线密封口,密封腔体的出气管上装有排气阀门。优点:测定水文地质参数成本低。不需要安装永久监测井。消除了由钻探、处置钻探切割物、建设监测井带来的庞大费用以及洗井水对环境的污染。测试可以在含水层不同深度和不同位置迅速实施,从而确定K值的垂直和水平变量。在大部分松散地层中获得不同深度高质量渗透系数的离散数据。达到最高的数据质量。在高K值到中等K值的地层中,可提供较低噪音或无噪音的高质量数据。可确定其它方法不适用的高渗透性含水层的渗透系数。
The utility model is a drilling oscillation type permeability coefficient value test pneumatic water head excitation device. It is equipped with a pressure display gauge in the well, a sealing port for cables, and an exhaust valve is installed on the air outlet pipe of the sealed cavity. Advantages: The cost of determining hydrogeological parameters is low. There is no need to install permanent monitoring wells. It eliminates the huge cost caused by drilling, disposal of drilling cuttings, construction of monitoring wells and the pollution of well washing water to the environment. Testing can be performed rapidly at different depths and locations in the aquifer to determine vertical and horizontal variations in K values. Discrete data of high quality permeability coefficients at different depths are obtained in mostly unconsolidated formations. Achieve the highest data quality. Provides high quality data with little or no noise in formations with high to medium K values. Permeability coefficients can be determined for highly permeable aquifers for which other methods are not applicable.
Description
技术领域 technical field
本实用新型涉及的是用于钻孔振荡式渗透系数取值试验系统中的气压式水头激发装置。属于仪器测试技术领域。The utility model relates to a pneumatic water head excitation device used in a drilling oscillation type permeability coefficient value test system. It belongs to the technical field of instrument testing.
背景技术 Background technique
渗透系数的确定是地下水资源评价、数值模拟、开发利用、环境保护以及科学管理的基础,通常通过现场抽水试验或压水试验获取。现场抽水试验即利用抽水设备(如量桶、空气压缩机和水泵)在井孔中产生一定水位降深,记录井孔中水位随时间变化数据,根据地下水动力学理论(如泰斯公式、裘布依公式等)计算得到渗透系数。The determination of hydraulic conductivity is the basis of groundwater resource evaluation, numerical simulation, development and utilization, environmental protection and scientific management, and is usually obtained through on-site pumping or pressure tests. The field pumping test is to use pumping equipment (such as measuring barrels, air compressors and water pumps) to generate a certain water level drawdown in the wellbore, and record the water level in the wellbore with time. Bouy formula, etc.) to calculate the permeability coefficient.
抽水试验持续时间长、所需设备及操作人员多、费用高、对场地及井孔要求苛刻且极易对含水层造成污染。现场试验时,多采用测绳来测量动水位,而试验初始阶段水位变化极快,人工测量不可避免的会造成误差,从而降低了计算结果的可靠性。压水试验方法主要有单孔压水试验法和三段压水试验法。这些试验方法都是通过观测恒定压力条件下压入水量来评价裂隙岩体的透水性能,不能直接计算渗透系数等水文地质参数,信息利用率低。为改变这一状况,国内外不少学者先后提出了一些基于稳定流理论的求参公式,但是压水试验试段短、历时短,只有在极少数情况下才是稳定流,因而求出的渗透系数误差较大。此外,压水试验对场地及设备的要求均较高,可操作性不强。The pumping test lasts a long time, requires a lot of equipment and operators, is expensive, has strict requirements on the site and well holes, and easily pollutes the aquifer. In the field test, the measuring rope is often used to measure the dynamic water level, but the water level changes very fast in the initial stage of the test, and manual measurement will inevitably cause errors, thereby reducing the reliability of the calculation results. The pressure water test methods mainly include the single hole pressure water test method and the three-stage pressure water test method. These test methods evaluate the water permeability of the fractured rock mass by observing the amount of water injected under constant pressure conditions, and cannot directly calculate the hydrogeological parameters such as the permeability coefficient, and the information utilization rate is low. In order to change this situation, many scholars at home and abroad have successively proposed some parameter calculation formulas based on the steady flow theory, but the test section of the pressurized water test is short and the duration is short, and only in rare cases is the steady flow, so the obtained The permeability coefficient error is large. In addition, the pressure water test has high requirements on the site and equipment, and the operability is not strong.
现有的水头激发装置,需要安装永久监测井。这就由钻探、处置钻探切割物、建设监测井带来的庞大费用以及洗井水对环境的污染。测试无法在站点周围的不同深度和不同位置迅速实施,因此不能确定K值的垂直和水平变量。在大部分松散地层中得不到不同深度高质量渗透系数的离散数据。达不到最高的数据质量。在高K值到中等K值的地层中,对较低噪音或无噪音的高质量数据无法提供。Existing head excitation devices require the installation of permanent monitoring wells. This is caused by the huge cost of drilling, disposal of drilling cuttings, construction of monitoring wells, and environmental pollution of well washing water. Testing could not be performed rapidly at different depths and locations around the site, so vertical and horizontal variations in K values could not be determined. Discrete data of high-quality hydraulic conductivity at different depths are not available in most unconsolidated formations. The highest data quality is not achieved. In formations with high to medium K values, high quality data with little or no noise cannot be provided.
发明内容 Contents of the invention
本实用新型的目的旨在克服现有技术所存在的缺陷,提出一种气压式水头激发装置用于钻孔振荡式渗透系数取值试验系统,可确定其它方法不适用的高渗透性含水层的渗透系数。The purpose of this utility model is to overcome the existing defects of the prior art, and to propose a pneumatic hydraulic head excitation device for the drilling oscillation type permeability coefficient value test system, which can determine the high permeability aquifer that other methods are not suitable for. permeability coefficient.
本发明的技术解决方案:其结构是在进气管上装有减压阀、进气阀门,进气阀门的出气口接入密封腔体,密封腔体上装有井内压力显示表、电缆线密封口,密封腔体的出气管上装有排气阀门。The technical solution of the present invention: the structure is that a decompression valve and an air intake valve are installed on the air intake pipe, and the air outlet of the air intake valve is connected to a sealed cavity, and the sealed cavity is equipped with an internal pressure indicator and a cable sealing port. An exhaust valve is arranged on the air outlet pipe of the sealed cavity.
本实用新型的优点:快速测定水文地质参数,可节省大量时间和经费。主要表现在:1)不需要安装永久监测井,这就消除了由钻探、处置钻探切割物、建设监测井带来的庞大费用以及洗井水对环境的污染。2)测试可以在含水层的不同深度和不同位置迅速实施,从而确定K值的垂直和水平变量。3)可以在大部分松散地层中获得不同深度高质量渗透系数的离散数据。4)在高K值到中等K值的地层中,可提供较低噪音或无噪音的高质量数据。5)只有电缆和传感器与地下水接触,对于测试设备只要求最低的净化。6)气压振荡试验时,井内不加水或抽出地下水,对含水层扰动极小,数据精度高。7)可确定其它方法不适用的高渗透性含水层的渗透系数。The utility model has the advantages of quickly measuring hydrogeological parameters, which can save a lot of time and money. Mainly manifested in: 1) There is no need to install a permanent monitoring well, which eliminates the huge costs brought by drilling, disposal of drilling cuttings, construction of monitoring wells and the pollution of well washing water to the environment. 2) The test can be performed rapidly at different depths and locations in the aquifer to determine the vertical and horizontal variation of the K value. 3) Discrete data of high-quality permeability coefficients at different depths can be obtained in most unconsolidated formations. 4) In formations with high K value to medium K value, it can provide high-quality data with low noise or no noise. 5) Only the cables and sensors are in contact with groundwater, requiring only minimal decontamination of the test equipment. 6) During the air pressure oscillation test, no water is added to the well or ground water is pumped out, so the disturbance to the aquifer is minimal and the data accuracy is high. 7) It can determine the permeability coefficient of highly permeable aquifers for which other methods are not applicable.
通过在含水层布置的钻孔中激发水头变化,实时测量水头随时间的变化规律,利用地下水动力学原理,现场计算得到不同含水层介质中渗透系数。By stimulating the change of water head in the boreholes arranged in the aquifer, the change law of the water head with time is measured in real time, and the permeability coefficient in different aquifer media is calculated on site by using the principle of groundwater dynamics.
附图说明 Description of drawings
附图1是本实用新型的结构示意图Accompanying
具体实施方式 Detailed ways
对照附图1,其结构是进气管1上装有减压阀2、进气阀门3,进气阀门3的出气口接入密封腔体,密封腔体上装有井内压力显示表5、电缆线密封口6,密封腔体的出气管上装有排气阀门4。Comparing with accompanying
工作时,压缩空气通过进气管1进入,通过减压阀2调整进气压力,当密封腔体内的压力达到预置压力值时,关闭进气阀门3,同时开启排气阀门4激发水头变化,通过该水头变化计算得到渗透系数。When working, the compressed air enters through the
该装置是通过一定的激发方式,如可以瞬时抽取一定量的水,瞬时注入一定量的水,使用一定体积的柱状物体瞬时插入水中或提出水面,利用空气压缩机产生气压在钻孔中产生一定的压力等,使钻孔中水头产生振荡效应,利用测试系统记录水头随时间变化所对应的压力值,以供计算渗透系数。The device uses a certain excitation method, such as extracting a certain amount of water instantaneously, injecting a certain amount of water instantaneously, inserting a certain volume of columnar objects into the water or lifting the water surface instantaneously, and using an air compressor to generate air pressure to generate a certain amount of water in the borehole. The pressure, etc., causes the water head in the borehole to oscillate, and the test system is used to record the pressure value corresponding to the change of the water head with time for the calculation of the permeability coefficient.
当井内空气压力增加,水平面下降直到水压“上升”与气压“下降”压力相等时为止。一旦水平面稳定后,快速打开释放阀门,瞬间释放了井内空气压力。从而在没有水花飞溅的的情况下,水平面恢复至原位,同时压力传感器和数据记录仪记录了水平面的变化和时间。气压冲击测试可以提供非常高质量的数据,该数据没有“噪声”或因机械冲击方法而产生的水花飞溅的干扰。As the air pressure in the well increases, the water level drops until the water pressure "rises" equals the air pressure "falls". Once the water level stabilized, the release valve was quickly opened, instantly releasing the air pressure in the well. Thus, without splashing water, the water level returns to its original position, while the pressure sensor and data logger record the change and time of the water level. Pneumatic shock testing can provide very high quality data that is free from the "noise" or interference of water splashes that result from mechanical shock methods.
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| Application Number | Priority Date | Filing Date | Title |
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| CNU2008200309829U CN201156028Y (en) | 2008-01-17 | 2008-01-17 | Pneumatic water head excitation device for drilling oscillating permeability coefficient test |
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| CNU2008200309829U CN201156028Y (en) | 2008-01-17 | 2008-01-17 | Pneumatic water head excitation device for drilling oscillating permeability coefficient test |
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Cited By (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN106869909A (en) * | 2017-01-11 | 2017-06-20 | 河海大学 | It is determined that inclining the test device and its method of testing of filled opening hydrogeological parameter |
| CN109958434A (en) * | 2017-12-25 | 2019-07-02 | 核工业北京地质研究院 | Borehole hydrogeological test method for constant pressure and unsteady flow |
| CN111766189A (en) * | 2020-06-08 | 2020-10-13 | 重庆交通大学 | A three-dimensional tomographic scanning method for hidden seepage channels in embankments based on hydraulic stimulation |
| CN117761280A (en) * | 2023-11-30 | 2024-03-26 | 河海大学 | Device and method for testing hydrogeological parameters of aquifer under multi-field coupling effect |
-
2008
- 2008-01-17 CN CNU2008200309829U patent/CN201156028Y/en not_active Expired - Fee Related
Cited By (7)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN106869909A (en) * | 2017-01-11 | 2017-06-20 | 河海大学 | It is determined that inclining the test device and its method of testing of filled opening hydrogeological parameter |
| CN106869909B (en) * | 2017-01-11 | 2019-12-10 | 河海大学 | Testing device and testing method for determining hydrogeological parameters of inclined filling fracture |
| CN109958434A (en) * | 2017-12-25 | 2019-07-02 | 核工业北京地质研究院 | Borehole hydrogeological test method for constant pressure and unsteady flow |
| CN109958434B (en) * | 2017-12-25 | 2022-11-22 | 核工业北京地质研究院 | Drilling hydrogeological test method for drilling hole under constant pressure and unsteady flow |
| CN111766189A (en) * | 2020-06-08 | 2020-10-13 | 重庆交通大学 | A three-dimensional tomographic scanning method for hidden seepage channels in embankments based on hydraulic stimulation |
| CN111766189B (en) * | 2020-06-08 | 2023-11-17 | 重庆交通大学 | Three-dimensional chromatographic scanning method for embankment hidden seepage channel based on hydraulic stimulation |
| CN117761280A (en) * | 2023-11-30 | 2024-03-26 | 河海大学 | Device and method for testing hydrogeological parameters of aquifer under multi-field coupling effect |
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Granted publication date: 20081126 Termination date: 20100220 |