CN102735819A - Infiltrometer - Google Patents
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- CN102735819A CN102735819A CN2012102106035A CN201210210603A CN102735819A CN 102735819 A CN102735819 A CN 102735819A CN 2012102106035 A CN2012102106035 A CN 2012102106035A CN 201210210603 A CN201210210603 A CN 201210210603A CN 102735819 A CN102735819 A CN 102735819A
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- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 claims abstract description 135
- 239000002689 soil Substances 0.000 claims abstract description 89
- 238000003860 storage Methods 0.000 claims abstract description 44
- 238000005213 imbibition Methods 0.000 claims abstract description 25
- 238000002347 injection Methods 0.000 claims abstract description 16
- 239000007924 injection Substances 0.000 claims abstract description 16
- 238000002474 experimental method Methods 0.000 abstract description 2
- 238000001764 infiltration Methods 0.000 description 34
- 230000008595 infiltration Effects 0.000 description 34
- 238000000034 method Methods 0.000 description 19
- 230000008569 process Effects 0.000 description 8
- 238000009736 wetting Methods 0.000 description 8
- 229920006395 saturated elastomer Polymers 0.000 description 6
- 230000007423 decrease Effects 0.000 description 3
- 238000013459 approach Methods 0.000 description 2
- 230000008859 change Effects 0.000 description 2
- 230000001186 cumulative effect Effects 0.000 description 2
- 238000013508 migration Methods 0.000 description 2
- 230000005012 migration Effects 0.000 description 2
- 230000035699 permeability Effects 0.000 description 2
- 238000012360 testing method Methods 0.000 description 2
- 238000010521 absorption reaction Methods 0.000 description 1
- 230000009471 action Effects 0.000 description 1
- 230000009286 beneficial effect Effects 0.000 description 1
- 238000004364 calculation method Methods 0.000 description 1
- 238000001704 evaporation Methods 0.000 description 1
- 238000013401 experimental design Methods 0.000 description 1
- 238000007716 flux method Methods 0.000 description 1
- 238000012625 in-situ measurement Methods 0.000 description 1
- 238000003973 irrigation Methods 0.000 description 1
- 230000002262 irrigation Effects 0.000 description 1
- 238000005259 measurement Methods 0.000 description 1
- 238000000691 measurement method Methods 0.000 description 1
- 230000000704 physical effect Effects 0.000 description 1
- 239000008400 supply water Substances 0.000 description 1
- 239000012780 transparent material Substances 0.000 description 1
- 238000013022 venting Methods 0.000 description 1
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Abstract
本发明公开了一种渗吸仪,包括在水平板面上端面设置有土筒,靠水平板面一边沿固定有垂直面板,垂直面板正面安装有储水箱,储水箱的上方连接有注水槽,注水槽向下与储水箱的底部联通,储水箱侧面上段设置有排气阀,储水箱侧面下段设有出水阀;土筒的侧面上段设置有进水口,进水口与储水箱的出水阀联通,土筒的内腔设置有水平的多孔板,多孔板将土筒内腔分为装土层和盛水层,土筒的另一侧面设置有出水口。本发明的装置,体积小且易于移动,操作简便,适合推广于实验室内测定土壤渗吸速度及其相关参数的教学和试验中使用。
The invention discloses an imbibition meter, which comprises a soil cylinder arranged on the end surface of a horizontal plate surface, a vertical panel fixed on one edge of the horizontal plate surface, a water storage tank installed on the front of the vertical panel, and a water injection tank connected above the water storage tank. The water injection tank communicates downward with the bottom of the water storage tank, the upper part of the side of the water storage tank is provided with an exhaust valve, the lower part of the side of the water storage tank is provided with a water outlet valve; the upper part of the side of the soil cylinder is provided with a water inlet, and the water inlet is connected with the outlet valve of the water storage tank. The inner cavity of the soil cylinder is provided with a horizontal porous plate, which divides the inner cavity of the soil cylinder into a soil layer and a water storage layer, and the other side of the soil cylinder is provided with a water outlet. The device of the invention is small in size, easy to move and easy to operate, and is suitable for popularization and use in the teaching and experiment of measuring soil imbibition velocity and related parameters in a laboratory.
Description
技术领域 technical field
本发明属于水在土壤中入渗测量仪器技术领域,涉及一种渗吸仪。The invention belongs to the technical field of measuring instruments for water infiltration in soil, and relates to an imbibition instrument.
背景技术 Background technique
土壤水分运动是土壤内部能量循环的研究基础。宏观上饱和与非饱和土壤水运动均服从达西定律,在非饱和状态下,渗吸速度是变量,其值随土壤含水率变化,含水率越低,渗吸速度越大;在饱和状态下,渗吸速度是常量。渗吸速度是土壤的一个重要物理指标,反映了土壤的吸水性和透水性,测定此参数对研究土壤物理性质具有重要意义,对准确指导农业田间灌溉,更好确定土地利用方式等方面有重要的作用。Soil water movement is the basis of the study of soil internal energy cycle. Macroscopically, both saturated and unsaturated soil water movement obey Darcy's law. In the unsaturated state, the imbibition rate is a variable, and its value changes with the soil moisture content. The lower the moisture content, the greater the imbibition rate; in the saturated state , the imbibition rate is constant. The imbibition rate is an important physical index of the soil, which reflects the water absorption and water permeability of the soil. The determination of this parameter is of great significance to the study of soil physical properties, and it is important to accurately guide agricultural field irrigation and better determine land use methods. role.
目前测定土壤渗吸速度的方法很多,例如:双环法、环刀法、人工降雨法、圆盘入渗仪法、单环定量加水法、瞬时剖面法、垂直下渗通量法、垂直土柱稳定蒸发法、水平土柱吸渗法等。在众多测量方法中,田间原位测定广泛采用的测定仪器体积较大,限定了实验场地,有些仪器的价格昂贵。常用的实验室测定土壤渗吸速度的实验装置体积也较大,不能在短历时内测定渗吸速度随时间的变化规律及湿润锋在土壤标本中的运移规律,也不宜用于实验室教学使用。At present, there are many methods for measuring soil imbibition rate, such as: double-ring method, ring-knife method, artificial rainfall method, disc infiltration meter method, single-ring quantitative water addition method, instantaneous profile method, vertical infiltration flux method, vertical soil column method, etc. Stable evaporation method, horizontal soil column imbibition method, etc. Among the many measurement methods, the measurement instruments widely used in field in situ measurement are large in size, which limits the experimental site, and some instruments are expensive. The commonly used experimental device for measuring soil imbibition velocity in the laboratory is also relatively large in volume, and cannot measure the variation of imbibition velocity with time and the migration law of the wetting front in soil samples in a short period of time, and is not suitable for laboratory teaching. use.
发明内容 Contents of the invention
本发明的目的是提供一种渗吸仪,解决了现有技术中存在实验装置体积也较大,不能在短历时内测定所需参数的问题。The purpose of the present invention is to provide a kind of osmosis instrument, which solves the problem in the prior art that the volume of the experimental device is relatively large and the required parameters cannot be measured in a short period of time.
本发明所采用的技术方案是,一种渗吸仪,包括水平板面,在水平板面上端面设置有土筒,靠水平板面一边沿固定连接有垂直面板,垂直面板正面安装有储水箱,储水箱的上方连接有注水槽,注水槽向下通过进气管与储水箱的底部联通,储水箱侧面上段设置有排气阀,储水箱侧面下段设有出水阀;The technical scheme adopted in the present invention is that a kind of imbibition instrument comprises a horizontal plate surface, a soil cylinder is arranged on the end surface of the horizontal plate surface, a vertical panel is fixedly connected to one edge of the horizontal plate surface, and a water storage tank is installed on the front of the vertical panel surface , the top of the water storage tank is connected with a water injection tank, and the water injection tank is downwardly connected with the bottom of the water storage tank through the intake pipe, the upper part of the side of the water storage tank is provided with an exhaust valve, and the lower part of the side of the water storage tank is provided with a water outlet valve;
土筒的侧面上段设置有进水口,进水口通过软管与储水箱的出水阀联通,土筒的内腔靠下位置设置有水平的多孔板,多孔板将土筒内腔分为上层的装土层和下层的盛水层,土筒的另一侧面下段靠近盛水层底部位置设置有出水口。The upper part of the side of the soil cylinder is provided with a water inlet, which communicates with the water outlet valve of the water storage tank through a hose, and a horizontal perforated plate is installed at the lower part of the inner cavity of the soil cylinder, and the perforated plate divides the inner cavity of the soil cylinder into upper chambers. The soil layer and the water holding layer of the lower layer, and the lower part of the other side of the soil cylinder is provided with a water outlet near the bottom of the water holding layer.
本发明的有益效果是,通过改进后的自动供水装置模拟恒定积水水头条件下垂直土柱的土壤水分入渗,可在短历时内观测到土壤水分入渗的整个过程,包括自由入渗过程、顶托入渗过程和渗透过程,及测定渗吸速度随时间的变化规律,可延伸测定土壤渗透系数,同时也可观测土壤湿润锋的推进过程,仪器结构简单,体积小且易于移动,操作简便,可多台仪器同时试验,适合推广于实验室内对土壤渗吸速度的教学和试验测量。The beneficial effect of the present invention is that, through the improved automatic water supply device simulating the soil moisture infiltration of the vertical soil column under the condition of constant accumulated water head, the whole process of soil moisture infiltration, including the free infiltration process, can be observed in a short period of time , jacking infiltration process and infiltration process, and the determination of the variation of imbibition speed with time, which can be extended to measure the soil permeability coefficient, and can also observe the advancement process of the soil wetting front. The instrument is simple in structure, small in size and easy to move, easy to operate It is simple and can be tested by multiple instruments at the same time. It is suitable for teaching and testing the soil imbibition rate in the laboratory.
附图说明 Description of drawings
图1是本发明渗吸仪测定装置实施例的结构示意图。Fig. 1 is a schematic structural view of an embodiment of the osmometer measuring device of the present invention.
图中,1.土筒;2.垂直面板;3.水平板面;4.注水槽;5.进气管;6.储水箱;7.排气阀;8.螺帽;9.出水阀;10.多孔板;11.土筒进水口;12.土筒出水口;13.装土层;14.盛水层;15.支座;16.固定螺栓一;17.固定螺栓二。In the figure, 1. soil cylinder; 2. vertical panel; 3. horizontal panel; 4. water injection tank; 5. air intake pipe; 6. water storage tank; 7. exhaust valve; 8. nut; 9. outlet valve; 10. Perforated plate; 11. Water inlet of soil cylinder; 12. Water outlet of soil cylinder; 13. Loading soil layer; 14. Water holding layer; 15. Support; 16. One fixing bolt;
具体实施方式 Detailed ways
下面结合附图和具体实施方式对本发明进行详细说明。The present invention will be described in detail below in conjunction with the accompanying drawings and specific embodiments.
如图1所示,为本发明实施例的渗吸仪的结构示意图,该装置结构是,包括水平板面3,在水平板面3上端面设置有土筒1,水平板面3底端四个角分别设有支座15,靠水平板面3一边沿固定连接有垂直面板2,垂直面板2正面靠上段安装有储水箱6,储水箱6通过固定螺栓二17支撑在垂直面板2正面,储水箱6的上方连接有注水槽4,注水槽4通过固定螺栓一16固定在垂直面板2正面和储水箱6上,注水槽4向下通过进气管5与储水箱6的底部联通,储水箱6侧面上段设置有排气阀7,排气阀7上设有放气螺栓及匹配的螺帽8,螺帽8上设有圆孔,储水箱6侧面下段设有出水阀9;As shown in Fig. 1, it is the structural representation of the imbibition instrument of the embodiment of the present invention, and this device structure is, comprises horizontal plate surface 3, is provided with soil tube 1 on the upper end surface of horizontal plate surface 3, and horizontal plate surface 3 bottom four Two angles are respectively provided with bearing 15, and vertical panel 2 is fixedly connected with one edge by horizontal panel surface 3, and vertical panel 2 front is equipped with water storage tank 6 by upper section, and water storage tank 6 is supported on vertical panel 2 front by fixing bolt 2 17, The top of the water storage tank 6 is connected with a water injection tank 4, and the water injection tank 4 is fixed on the vertical panel 2 front and the water storage tank 6 by fixing bolts 16, and the water injection tank 4 is downwardly connected with the bottom of the water storage tank 6 through the air intake pipe 5, and the water storage tank 6. An exhaust valve 7 is provided on the upper section of the side. The exhaust valve 7 is provided with a venting bolt and a matching nut 8. The nut 8 is provided with a round hole. The lower section of the side of the water storage tank 6 is provided with a water outlet valve 9;
土筒1的侧面上段设置有进水口11,进水口11通过软管与储水箱6的出水阀9联通,土筒1的内腔靠下位置设置有水平的多孔板10,多孔板10将土筒1内腔分为上层的装土层13和下层的盛水层14,土筒1的另一侧面下段靠近盛水层14底部位置设置有出水口12。The upper part of the side of the soil cylinder 1 is provided with a water inlet 11, and the water inlet 11 communicates with the water outlet valve 9 of the water storage tank 6 through a hose. The inner cavity of the cylinder 1 is divided into an upper soil-loading layer 13 and a lower water-holding layer 14, and the lower part of the other side of the soil cylinder 1 is provided with a water outlet 12 near the bottom of the water-holding layer 14.
实施例1Example 1
按照以下参数进行设置:Set according to the following parameters:
土筒1高度20cm,内圆直径为5cm,土筒1内部由下向上3cm处设有多孔板10(板厚度1cm),装土层13高度为12cm,盛水层14高度为3cm,进水口11设置在土筒1从上至下4cm处,出水口12设置在土筒1从下向上0.6cm处,相当于盛水层14的最低处。The height of soil cylinder 1 is 20cm, and the diameter of the inner circle is 5cm. The inside of soil cylinder 1 is provided with perforated plate 10 (plate thickness 1cm) from bottom to top at 3cm. 11 is arranged at 4cm from top to bottom of soil cylinder 1, and water outlet 12 is arranged at 0.6cm from bottom to top of soil cylinder 1, which is equivalent to the lowest point of water-holding layer 14.
注水槽4为无盖方形槽或圆形槽,注水槽4底板设置有圆口,该圆口与进气管5直径一致并联通。The water injection groove 4 is a square groove or a circular groove without a cover, and the bottom plate of the water injection groove 4 is provided with a round mouth, which is consistent with the diameter of the air intake pipe 5 and communicates.
进气管5底端设有拐角,进气管5底端的拐点高于储水箱6出水阀9的高度2cm。Air intake pipe 5 bottoms are provided with corner, and the inflection point of air intake pipe 5 bottoms is higher than the height 2cm of water storage tank 6 outlet valves 9.
储水箱6横截面积为15cm2,高为25cm,并且储水箱6为透明材质制作的容器,其上设置有观测水位读数的量尺。The water storage tank 6 has a cross-sectional area of 15 cm 2 and a height of 25 cm, and the water storage tank 6 is a container made of transparent material, on which a ruler for observing the water level reading is arranged.
本发明的渗吸仪,用于测定土壤渗吸速度以及湿润锋运移规律,操作步骤是:The imbibition meter of the present invention is used for measuring soil imbibition speed and wetting front migration law, and the operation steps are:
步骤1)储水箱6注水。打开储水箱6的出水阀9和排气阀7,排气阀7上的圆孔与大气相通,使储水箱6中的余水全部流出,关闭出水阀9。用盛满水的量杯向注水槽4内注水,这时,水将通过注水槽4底板上的圆孔流入进气管5,通过进气管5拐角进入到储水箱6中。加水过程中,不可使注水槽4中出现断流现象。注水到储水箱6内水面略低于排气阀7高度时为止,关闭排气阀7。缓慢打开出水阀9,记录储水箱6的初始水位。Step 1) Water storage tank 6 is filled with water. Open the water outlet valve 9 and the exhaust valve 7 of the water storage tank 6, the circular hole on the exhaust valve 7 communicates with the atmosphere, so that the remaining water in the water storage tank 6 is all flowed out, and the water outlet valve 9 is closed. With the measuring cup filled with water, fill water in the water injection tank 4, at this moment, water will flow into the air intake pipe 5 by the circular hole on the water injection tank 4 bottom plates, and enter in the water storage tank 6 by the air intake pipe 5 corners. In the process of adding water, the phenomenon of flow interruption can not occur in the water injection tank 4 . Water filling until when the water surface in the water storage tank 6 is slightly lower than the exhaust valve 7 height, close the exhaust valve 7. Slowly open the water outlet valve 9, and record the initial water level of the water storage tank 6.
步骤2)制作土壤标本。首先在多孔板10上垫一层与土筒1内径相同大小的定性滤纸,防止在装土时有土漏出。将扰动土按容重要求分层装进土筒1中,装土高度为12cm,刚好低于土筒1的进水口11位置。当土筒1装好土后,用软管将储水箱6出水口9和土筒1进水口11相连。Step 2) Make a soil sample. At first put a layer of qualitative filter paper with the same size as the inner diameter of the soil cylinder 1 on the perforated plate 10 to prevent soil from leaking out when loading the soil. The disturbed soil is packed into the soil barrel 1 layer by layer according to the bulk density requirement, and the soil filling height is 12 cm, which is just lower than the water inlet 11 of the soil barrel 1. After the soil cylinder 1 has installed the soil, the water outlet 9 of the water storage tank 6 is connected to the water inlet 11 of the soil cylinder 1 with a flexible pipe.
步骤3)开始试验。在土面上覆盖一层滤纸。用量杯量出与土筒内2cm高体积相同的水量,迅速倒入土筒,并随即打开储水箱6出水阀9,储水箱6中水量通过出水口向土筒1供水,供水量可通过储水箱6上的标尺读出数据,直到土壤标本底部开始出水达到渗透状态,及土筒1出水口12有水流出并达到稳定为止,即可测得土壤渗吸速度的变化规律。在测定入渗水量的同时,记录土壤湿润锋在土体内的推进过程,直到湿润锋到达土壤标本底部为止,则可测得土壤浸润速度的变化规律。Step 3) Start the experiment. Cover the soil surface with a layer of filter paper. Use a measuring cup to measure the same amount of water as the 2cm high volume in the soil cylinder, quickly pour it into the soil cylinder, and then open the water outlet valve 9 of the water storage tank 6, and the water in the water storage tank 6 will supply water to the soil cylinder 1 through the water outlet. The scale on the water tank 6 reads the data until the bottom of the soil sample begins to flow out of water and reaches the infiltration state, and the water outlet 12 of the soil cylinder 1 has water flowing out and reaches stability, then the variation law of the soil imbibition rate can be measured. While measuring the amount of infiltration water, record the advance process of the soil wetting front in the soil until the wetting front reaches the bottom of the soil sample, then the change rule of the soil infiltration speed can be measured.
渗吸仪测定原理:利用等压原理,根据等压面的平衡条件,通过改进后的马里奥特供水装置,自动向土壤标本供水,达到既连续供水又维持一定高度的积水入渗水头。在土水势梯度作用下水分渗入土壤,随着观测时间的增加,土壤水分入渗先后经过自由入渗阶段、顶托入渗阶段和渗透阶段,直到有水透过土壤标本渗出,并落入土筒1下端的盛水层14,由出水口12流出,在试验设计观测时间内称量流出的水的重量。Measuring principle of the imbibition meter: Using the principle of equal pressure, according to the equilibrium condition of the isobaric surface, water is automatically supplied to the soil sample through the improved Marriott water supply device, so as to achieve continuous water supply and maintain a certain height of stagnant water infiltration head. Under the action of the soil water potential gradient, water infiltrates into the soil. As the observation time increases, the soil water infiltration successively goes through the free infiltration stage, the jacking infiltration stage and the infiltration stage, until water seeps through the soil sample and falls into the soil. The water holding layer 14 at the lower end of the soil cylinder 1 flows out from the water outlet 12, and the weight of the water flowing out is weighed within the experimental design observation time.
在试验过程中随着入渗的进行,相应读取渗入土壤表面以下的累积入渗量和湿润锋向下推进的距离,将累积入渗量与时间的关系求导后,即为土壤入渗率随时间的变化关系。根据具有物理意义的Philip入渗公式(1):During the test, as the infiltration progresses, the cumulative infiltration below the soil surface and the distance of the wetting front are read accordingly, and the relationship between the cumulative infiltration and time is derived, which is the soil infiltration rate change over time. According to the Philip infiltration formula (1) with physical meaning:
式中,i为入渗率,S为吸渗率,t为入渗时间,if为稳定入渗率,公式表明,在入渗初期(t较小时),土壤远未饱和,具有较大的吸力,水势梯度远大于1,则入渗率i较大,且i远大于if;随着入渗时间增加,表土含水率增加,土壤吸力减小,i呈指数线型迅速减小;当入渗一定时间后,吸力为零时,水势梯度约等于1,入渗速度就会减小并接近一个定值,并将接近此定值的入渗率作为稳定入渗率if。In the formula, i is the infiltration rate, S is the infiltration rate, t is the infiltration time, and if is the stable infiltration rate. The formula shows that at the initial stage of infiltration (when t is small), the soil is far from saturated and has a large If the water potential gradient is much larger than 1, the infiltration rate i is larger, and i is much larger than if ; as the infiltration time increases, the water content of the topsoil increases, the soil suction decreases, and i decreases rapidly in an exponential linear fashion; After a certain period of infiltration, when the suction is zero and the water potential gradient is approximately equal to 1, the infiltration velocity will decrease and approach a constant value, and the infiltration rate close to this constant value is taken as the stable infiltration rate if .
稳定入渗率if也就是土壤饱和时的渗吸速度K,已知土壤标本高度L,土筒横截面积A,t时间内渗过土壤标本的水量V,常水头的高度h,根据达西定律,饱和渗吸速度的计算如下式(2)所示:The stable infiltration rate if is the imbibition rate K when the soil is saturated, the height of the soil sample is known L, the cross-sectional area of the soil cylinder is A, the amount of water infiltrated into the soil sample in time t is V, and the height of the constant water head is h. West's law, the calculation of saturated imbibition velocity is shown in the following formula (2):
计算出一系列渗吸速度,当这些值趋近于一个常数,就假定此常数为垂向的饱和渗吸速度。A series of imbibition velocities are calculated, and when these values approach a constant, it is assumed that this constant is the vertical saturated imbibition velocity.
通过对土壤湿润锋的推进过程的观测,将湿润锋位置与时间的关系求导,可得到水分在土体中的浸润速度。By observing the advancement process of the soil wetting front, and deriving the relationship between the position of the wetting front and time, the infiltration speed of water in the soil can be obtained.
Claims (6)
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
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CN106033046A (en) * | 2015-03-12 | 2016-10-19 | 西北农林科技大学 | An automatic measuring device for soil saturated hydraulic conductivity |
CN108226008A (en) * | 2018-01-18 | 2018-06-29 | 西安理工大学 | Self-loopa varying head darcy permeability test instrument |
CN110082272A (en) * | 2019-04-30 | 2019-08-02 | 中国地质大学(北京) | The device and method of the spontaneous imbibition of rock core under a kind of evaluation formation condition |
CN110376114A (en) * | 2019-08-27 | 2019-10-25 | 石河子大学 | Integrated soil infiltration rate measurement combination unit and measuring method |
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CN117169089A (en) * | 2023-11-03 | 2023-12-05 | 东北农业大学 | Tension infiltration instrument for detecting soil permeability |
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CN104458528A (en) * | 2014-11-05 | 2015-03-25 | 中国电建集团贵阳勘测设计研究院有限公司 | Method and device for measuring field slope earth surface infiltration performance and permeability coefficient |
CN106033046A (en) * | 2015-03-12 | 2016-10-19 | 西北农林科技大学 | An automatic measuring device for soil saturated hydraulic conductivity |
CN106033046B (en) * | 2015-03-12 | 2019-05-17 | 西北农林科技大学 | A kind of saturated hydraulic conductivity in soil apparatus for automatically measuring |
CN105547779A (en) * | 2015-12-24 | 2016-05-04 | 辽宁省水文局 | Soil field water capacity soil sample manufacturing method and device and measuring method |
CN105547779B (en) * | 2015-12-24 | 2018-07-31 | 辽宁省水文局 | Water-retaining quantity among field of soil soil sample production method, device and measurement method |
CN108226008A (en) * | 2018-01-18 | 2018-06-29 | 西安理工大学 | Self-loopa varying head darcy permeability test instrument |
CN110082272A (en) * | 2019-04-30 | 2019-08-02 | 中国地质大学(北京) | The device and method of the spontaneous imbibition of rock core under a kind of evaluation formation condition |
CN110376114A (en) * | 2019-08-27 | 2019-10-25 | 石河子大学 | Integrated soil infiltration rate measurement combination unit and measuring method |
CN111413263A (en) * | 2020-05-06 | 2020-07-14 | 西安理工大学 | Triaxial instrument for joint determination of water-vapor movement in unsaturated soil |
CN117169089A (en) * | 2023-11-03 | 2023-12-05 | 东北农业大学 | Tension infiltration instrument for detecting soil permeability |
CN117169089B (en) * | 2023-11-03 | 2024-01-26 | 东北农业大学 | A tension infiltrometer for detecting soil permeability |
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Effective date of registration: 20190320 Address after: 710000 Jadeite International Building 2 21406, Fengcheng Second Road, Xi'an Economic and Technological Development Zone, Xi'an City, Shaanxi Province Patentee after: Xi'an Hongertai Hydropower New Technology Co.,Ltd. Address before: 710048 No. 5 Jinhua South Road, Shaanxi, Xi'an Patentee before: Xi'an University of Technology |
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Correction item: Patentee|Address Correct: Xi'an Hongertai Hydropower New Technology Co., Ltd.|710000 Jadeite International Building 2 21406, Fengcheng Second Road, Xi'an Economic and Technological Development Zone, Xi'an City, Shaanxi Province False: Xi'an Hongertai Hydropower New Technology Co., Ltd.|710000 Jadeite International Building 2 21406, Fengcheng Second Road, Xi'an Economic and Technological Development Zone, Xi'an City, Shaanxi Province Number: 15-01 Volume: 35 |