CN201724984U - Device of measuring electrical conductivity of cross section of soil - Google Patents

Device of measuring electrical conductivity of cross section of soil Download PDF

Info

Publication number
CN201724984U
CN201724984U CN2010202276494U CN201020227649U CN201724984U CN 201724984 U CN201724984 U CN 201724984U CN 2010202276494 U CN2010202276494 U CN 2010202276494U CN 201020227649 U CN201020227649 U CN 201020227649U CN 201724984 U CN201724984 U CN 201724984U
Authority
CN
China
Prior art keywords
soil
gear
conductivity
fixed
separately
Prior art date
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
Application number
CN2010202276494U
Other languages
Chinese (zh)
Inventor
史舟
李洪义
郭燕
饶秀勤
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.)
Zhejiang University ZJU
Original Assignee
Zhejiang University ZJU
Priority date (The priority date 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 date listed.)
Filing date
Publication date
Application filed by Zhejiang University ZJU filed Critical Zhejiang University ZJU
Priority to CN2010202276494U priority Critical patent/CN201724984U/en
Application granted granted Critical
Publication of CN201724984U publication Critical patent/CN201724984U/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

Links

Images

Landscapes

  • Investigating Or Analyzing Materials By The Use Of Electric Means (AREA)

Abstract

The utility model discloses a device of measuring the electrical conductivity of the cross section of the soil. The measuring method comprises the following steps of: moving the device which can be horizontally and vertically moved to the surface of the soil to be measured; automatically recording the geographical position information by GPS equipment on the device; lifting up the device to the place which is higher than the ground surface at 1.5m by a first stepping motor; controlling the horizontal position and the vertical position of the device by a second stepping motor to perform the correction program by means of returning to zero; acquiring the electrical conductivity under the horizontal mode and the vertical mode at N heights from 0.05 to 1.5m (the height of a trundle of the device is 5cm), wherein the height and the angle of the device are respectively determined by a plurality of pulse signals which are applied to the first stepping motor and the second stepping motor; controlling the measuring and the data recording of the device by a trigger switch; and transmitting the GPS data, the height value of the device which is far away from the ground surface and the electrical conductivity measuring date at the corresponding height to a data storage. The device can accurately inverse the electrical conductivity of the cross section by the means that an electromagnetic inductive linear model is combined with the Tikhonov regularization method.

Description

A kind of conductivity of soil profile measurement mechanism
Technical field
The utility model relates to conductivity measuring apparatus, especially relates to a kind of conductivity of soil profile measurement mechanism.
Background technology
Salinity is the material impact factor of salt affected soil quality and crop yield, causes leaving uncultivated of agricultural soil when serious.The marine solonchak of enclosing and cultivating for management and use effectively for soil management provides the decision-making foundation of science, need carry out frequent monitoring to soil salt.The sampling pattern of intrusive moods such as similar excavation, boring and cone penetrometer is the most frequently used method of soil profile sampling, but can only gather limited sampled point because unfavorable factors such as time-consuming and expense height have limited these class methods, be not suitable for carrying out large-area soil profile salinity investigation.Therefore, be badly in need of the cheap of a kind of non-intrusion type and section Detection Techniques easily.
Traditional section conductivity measuring method is measured after excavating the soil section, and main method has: (1) gathers pedotheque, measures conductivity value through chemical experiment; (2) adopt the soil conductivity proving installation to carry out in-site measurement.Such device is based on the contact design of " current-voltage four-end method ", Veris3100 soil conductivity detector as the production of U.S. VerisTechnology company, when measuring, do not need sampling, more convenient relatively (Jabro J D, Evans R G, Stevens W B, et al.Repeatability of SoilApparent Electrical Conductivity Measured by the Veris 3100 Sensor.Soil Science, 2008,173:35-45).Waste time and energy but excavate the preliminary work of section the early stage of these two kinds of methods, in order to raise the efficiency, researchers have developed new method.
Utilization is obtained the section soil conductivity based on the non-intrusion type design of electromagnetic induction principle, promptly the transmitting coil to instrument internal feeds alternating flow, and respond to the variation in magnetic field in the soil with receiving coil, variation by institute's measuring magnetic field characterize soil conductivity (Soil Apparent Electrical Conductivity, ECa).The typical representative products of the type equipment is the EM38 that Canadian Geonics company produces, this instrument profile is bar shaped, weight is lighter, is connected with high-precision differential GPS, the face of land is just scanned can be obtained the conductivity of soil profile that has the two-dimensional space coordinate fast.The investigation depth of EM38 under horizontal pattern is 0.75m, investigation depth under the vertical mode reaches 1.50m, but the conductivity that records is the situation of whole 1.5 meters conductivity of soil profile, has only a measured value, can not obtain in 1.5 meters soil profiles a series of conductivity parameters (McNeill J D.Electromagnetic terrain conductivity measurementat low induction numbers.Tech.Note TN-6.Geonics that soil conductivity successively changes, ON, Canada, 1980).
Therefore, the empirical model that has the scholar to survey conductivity by the soil conductivity ECa that sets up the face of land and measure and the different soil degree of depth obtains section conductivity (Slavich P G Determining ECa depth profilesfrom electromagnetic induction measurements.Aust.J.Soil Res, 1990,28:443-452).Although the precision of prediction of the type model is higher, but facts have proved when the type model is generalized to the different field piece section conductivity prediction of soil attribute and need proofread and correct (Borchers B again, Uram T, Hendrickx J MH.Tikhonov regularization of electrical conductivity depth profiles in field soils.SoilSci.Soc.Am.J, 1997,61:1004-1009).Therefore, be necessary to set up a kind of general conductivity of soil profile forecast model, and design the soil conductivity ECa that new device comes quick measuring distance table soil differing heights, adopt EM38 conductivity profile electromagnetic induction response model to predict conductivity by the method for separating least square problem.
In above-mentioned research, the research of similar measuring device of soil conductivity and section conductivity Forecasting Methodology is not appeared in the newspapers as yet.
Summary of the invention
Can not directly measure the defective of three-dimensional section conductivity in order to overcome existing soil conductivity detector, the purpose of this utility model is to provide a kind of conductivity of soil profile measuring method and device.
The technical solution adopted in the utility model is:
One, a kind of conductivity of soil profile measuring method, the step of this method is as follows:
1) device location: device is moved to the soil to be measured face of land, and by the automatic recording geographical position information of GPS equipment on the soil conductivity detector;
2) soil conductivity detector zero-in: the soil conductivity detector is lifted to the position high apart from ground 1.5m by first stepper motor on the device, again by second stepper motor, control the horizontal and vertical position of soil conductivity detector, carry out the zero-in program;
3) automatic lifting and record data: by the conductivity of lifting soil conductivity detector under N height level of collection, vertical mode between 0.05~1.5m, the height of soil conductivity detector and angle are determined by the pulse signal that is applied on first stepper motor and second stepper motor respectively, and control the test and the data recording of soil conductivity detector by trigger switch.At last gps data, soil conductivity detector all are transferred in the computer from face of land height value and differing heights conductivity measurement certificate.
The step of its data processing is as follows:
1) with in the data importing computer in the data-carrier store, N the level, the conductivity value under the vertical mode and the soil conductivity detector that obtain the above differing heights in the face of land leave in the computer from the height value on the face of land;
2) the theoretical conductivity of a calculating face of land N height and position: suppose soil is divided into the M layer, bottom M extends to the earth's core degree of depth.According to the sensitivity model under soil conductivity detector level, the vertical mode, calculate the h that gathers 1, h 2... h NDeng N theoretical conductivity m (σ) that highly locates, leave in the computer;
3) inverting section conductivity value: select best Tikhonov regularization parameter λ by L-curve rule, with λ substitution Tikhonov regularization equation, inverting section conductivity is left in the computer;
4) whole calculating adopts the Matlab programming to realize.
Two, a kind of conductivity of soil profile measurement mechanism:
The framework of forming pick-up unit by four connecting links and two end plates, two rhizoid bars respectively by clutch shaft bearing up and down and up and down the clutch shaft bearing seat be installed on separately the end plate, two worm gears are separately fixed at screw mandrel top separately, two slide blocks are installed in respectively on the two rhizoid bars of two worm gear belows, one end of two fixed blocks is rotationally connected by coupling shaft and separately the 3rd bearing and slide block respectively, the soil conductivity detector is installed between the other end of two fixed blocks, fix with adjusting knob, worm screw respectively by second bearing separately and separately second bearing seat be installed between the two end plates, second gear is fixed on the worm screw of first screw mandrel, one side, worm gear is meshed with worm screw, first stepper motor is fixed on the end plate of first screw mandrel, one side by the first stepping electric machine support, first gear is fixed on the turning axle of first stepper motor, first gear is meshed with second gear, second stepper motor is fixed on the slide block of first screw mandrel, one side, the 3rd gear is fixed on the turning axle of second stepper motor, the 4th gear is fixed on the slide block of a side, the 3rd gear and the 4th gear are meshed, driving the soil conductivity detector rotates, four castors are installed in the end plate bottom, and computer links to each other with the soil conductivity detector.
The beneficial effect that the utlity model has is:
Utilize the electromagnetic induction linear model to come inverting section conductivity, need not excavate soil profile, can fast predict the section conductivity of soil exactly in conjunction with the Tikhonov regularization method.
Description of drawings
Fig. 1 is a measurement mechanism structural representation of the present utility model.
Fig. 2 is the sectional view of Fig. 1.
Fig. 3 is the soil layering model.
Fig. 4 is the section conductivity inversion result of sampling point 1.
Fig. 5 is the section conductivity inversion result of sampling point 2.
Among the figure: 1, castor, 2, the clutch shaft bearing seat, 3, clutch shaft bearing, 4, screw mandrel, 5, slide block, 6, coupling shaft, 7, fixed block, 8, knob, 9, soil conductivity detector, 10, worm screw, 11, worm gear, 12, second bearing seat, 13, second bearing, 14, first stepper motor, 15, first gear, 16, second gear, 17, connecting link, 18, end plate, 19, the first stepping electric machine support, the 20, the 3rd gear, 21, second stepper motor, the 22, the 3rd bearing, the 23, the 4th gear.
Embodiment
The utility model is described in further detail below in conjunction with drawings and Examples.
As Fig. 1, shown in Figure 2, the utility model is made of the framework of pick-up unit four connecting links 17 and two end plates 18, two rhizoid bars 4 respectively by clutch shaft bearing 3 up and down and up and down clutch shaft bearing seat 2 be installed on separately the end plate 18, two worm gears 11 are separately fixed at screw mandrel 4 tops separately, two slide blocks 5 are installed in respectively on the two rhizoid bars 4 of two worm gear belows, one end of two fixed blocks 7 is rotationally connected with slide block 5 by coupling shaft 6 and the 3rd bearing 22 separately respectively, soil conductivity detector 9 is installed between the other end of two fixed blocks 7, fixing with adjusting knob 8, worm screw 10 respectively by second bearing 13 separately and separately second bearing seat 12 be installed between the two end plates 18, second gear 16 is fixed on the worm screw 10 of first screw mandrel, 4 one sides, worm gear 11 is meshed with worm screw 10, first stepper motor 14 is fixed on the end plate 18 of first screw mandrel, 4 one sides by the first stepping electric machine support 19, first gear 15 is fixed on the turning axle of first stepper motor 14, first gear 15 is meshed with second gear 16, second stepper motor 21 is fixed on the slide block 5 of first screw mandrel, 4 one sides, the 3rd gear 20 is fixed on the turning axle of second stepper motor 21, the 4th gear 23 is fixed on the slide block 5 of a side, the 3rd gear 20 and the 4th gear 23 are meshed, driving soil conductivity detector 9 rotates, four castors 1 are installed in the end plate bottom, and computer links to each other with soil conductivity detector 9.
The step of this method is as follows:
1) device location: device is moved to the soil to be measured face of land, and by the automatic recording geographical position information of GPS equipment on the soil conductivity detector;
2) soil conductivity detector zero-in: the soil conductivity detector is lifted to the position high apart from ground 1.5m by first stepper motor on the device, again by second stepper motor, control the horizontal and vertical position of soil conductivity detector, carry out the zero-in program;
3) automatic lifting and record data: by the conductivity of lifting soil conductivity detector under N height of level of collection, vertical mode between 0.05~1.5m (device castor height is 5cm), the height of soil conductivity detector and angle are determined by the pulse signal that is applied on first stepper motor and second stepper motor respectively, and control the test and the data recording of soil conductivity detector by trigger switch.At last gps data, soil conductivity detector all are transferred in the computer from face of land height value and differing heights conductivity measurement data.
During measurement, give first stepper motor 14 certain pulse signal, first stepper motor 14 rotates motion, and will rotatablely move and be delivered to respectively on the 2 rhizoid bars 4 through second gear 16, worm screw 10, worm gear 11 by being fixed on first gear 15 on its turning axle, rotatablely moving of screw mandrel 4 makes slide block 5 that lengthwise movement take place, and pass to soil conductivity detector 9 by driving coupling shaft 6, the 3rd bearing 22 and fixed block 7, the height of soil conductivity detector 9 is changed.
Give second stepper motor 21 certain pulse signal, second stepper motor 21 rotates motion, and will rotatablely move and give soil conductivity detector 9 through the 4th gear 23, slide block 5 by being fixed on the 3rd gear 20 on its turning axle, the angle of soil conductivity detector 9 is changed.
The height of soil conductivity detector 9 and angle are respectively by the pulse signal decision that is applied on first stepper motor 14 and second stepper motor 21.
The soil conductivity detector is 5,10,20,30,40,50,60,75,90,100,120, the conductivity under 12 height such as 150cm collection level, the vertical mode, and promptly each section is gathered 24 conductivity data altogether
Figure BSA00000160044500051
And gps data, electric conductivity detector are recorded in the computer from face of land height value.
The step of data processing is as follows:
1) with in the data importing computer in the data-carrier store, N the level, the conductivity value under the vertical mode and the soil conductivity detector that obtain the above differing heights in the face of land leave in the computer from the height value on the face of land;
With the soil N height and position that collects (be designated as hi, i<N, the conductivity ECa under hi≤1.50m) level, the vertical mode is designated as vectorial d:
d = [ m 1 v , v 2 v , . . . , m N v , m 1 H , m 2 H , . . . , m N H ] T - - - ( 1 )
In the formula
D---N height and position level, vertical mode are surveyed the conductivity vector down,
Figure BSA00000160044500053
---the actual measurement conductivity under height hi place vertical mode,
Figure BSA00000160044500054
---the actual measurement conductivity under height hi place horizontal pattern,
2) the theoretical conductivity of a calculating face of land N height and position: suppose soil is divided into the M layer, bottom M extends to the earth's core degree of depth, and the soil layering model is seen Fig. 3.According to the sensitivity model under soil conductivity detector level, the vertical mode, calculate the h that gathers 1, h 2... h NDeng N theoretical conductivity m (σ) that highly locates, leave in the computer;
Predict conductivity meter at sampling point 5,10,20,30,40,50,60,75,90,100,120 by the linear model of formula (2)~(4), the level at 150cm equal altitudes place, the theoretical conductivity under the vertical mode are designated as m (σ).In the soil layering model, m (σ) can be expressed as formula (7)~(9).
φ H ( z ) = 2 - 4 z ( 4 z 2 + 1 ) 1 / 2 - - - ( 2 )
φ V ( z ) = 4 z ( 4 z 2 + 1 ) 3 / 2 - - - ( 3 )
σ H ( h ) = ∫ 0 ∞ φ H ( z + h ) σ ( z ) dz - - - ( 4 )
σ V ( h ) = ∫ 0 ∞ φ V ( z + h ) σ ( z ) dz - - - ( 5 )
m(σ)=[m V(h 1),m V(h 2),…,m V(h n),m H(h 1),m H(h 2),…,m H(h n)] T (6)
m(σ)=Kσ (7)
σ=[σ 1,σ 2…σ M-1,σ M] T (8)
K = ∫ 0 t 1 φ V ( z + h 1 ) dz . . . ∫ t 1 + t 2 + . . . t M - 1 ∞ φ V ( z + h 1 ) dz . . . . . . . . . ∫ 0 t 1 φ V ( z + h n ) dz . . . ∫ t 1 + t 2 + . . . t M - 1 ∞ φ V ( z + h n ) dz ∫ 0 t 1 φ H ( z + h 1 ) dz . . . ∫ t 1 + t 2 + t M - 1 ∞ φ H ( z + h 1 ) dz . . . . . . . . . ∫ 0 t 1 φ H ( z + h n ) dz . . . ∫ t 1 + t 2 + . . . t M - 1 ∞ φ H ( z + h n ) dz - - - ( 9 )
Z---soil depth,
φ H(z)---the sensitivity function under the conductivity meter horizontal pattern,
φ V(z)---the sensitivity function under the conductivity meter vertical mode,
H---conductivity meter is from the height on the face of land,
M (σ) is illustrated in the true soil conductivity at depth z place,
σ H(h)---under the horizontal pattern conductivity meter from the conductivity predicted value at height h place, the face of land,
σ V(h)---under the vertical mode conductivity meter from the conductivity predicted value at height h place, the face of land,
The actual conductivity vector of σ---a soil M different depth soil layer,
K---the integral equation of linear model relative measurement height;
3) inverting section conductivity value: select best Tikhonov regularization parameter λ by L-curve rule, with λ substitution Tikhonov regularization equation, inverting section conductivity is left in the computer.
Because conductivity can not be negative value,, therefore, can be reduced to Xie Fei and bear least square problem for the conductivity theoretical value m (σ) that makes the linear model prediction and the difference minimum of measured value d.Because K is ill-condition matrix, the least square problem of separating ill-condition matrix can cause the bigger deviation of parameter estimation for the tiny error of d, can address the above problem preferably by formula (11) Tikhonov regularization method.Calculate the curvature of L curve by formula (13), and select " flex point " of curvature maximum to determine optimal T ikhonov regularization parameter λ automatically.In optimized parameter λ substitution formula (11), inverting section conductivity again.
min‖Kσ-d‖ 22‖Lσ‖ 2,(σ>=0) (11)
L = 1 - 2 1 1 - 2 1 . . . . . . 1 - 2 1 - - - ( 12 )
k ( λ ) = 2 p ′ q ′ ′ - p ′ ′ q ′ ( ( p ′ ) 2 + ( q ′ ) 2 ) 3 / 2 ) - - - ( 13 )
D---5,10,20,30,40,50,60,75,90,100,120, the actual measurement conductivity value of 150cm equal altitudes place conductivity meter,
λ---Tikhonov regularization parameter,
K (λ)---the curvature of L-curve,
p——p=Ln(‖Kσ-d‖2),
q——q=Ln(‖Lσ‖2),
The first order derivative of p '---p,
The first order derivative of q '---q,
P "---the second derivative of p,
Q "---the second derivative of q;
The model prediction precision analysis, with model inversion 5,15,25,35,45,55,67.5,82.5,95, the conductivity at 110cm degree of depth place is example, with each soil layer EC of WET Sensor actual measurement bConductivity is estimated the entire profile precision of prediction by formula (14).To predict the outcome and measured value be plotted in Fig. 4, on the chart shown in Figure 5.The transverse axis of Fig. 4 and Fig. 5 is a soil depth, longitudinal axis conductivity.
The test that above-mentioned 2 samples are carried out shows that the predicated error of model is respectively: 28.35% and 31.03%, and precision of prediction is higher, can better prediction go out the section conductivity.
Figure BSA00000160044500073
4) whole calculating adopts the Matlab programming to realize, has applied for national computer software copyright registration certificate (registration number 2008SR17746).

Claims (1)

1. conductivity of soil profile measurement mechanism, it is characterized in that: the framework of forming pick-up unit by four connecting links and two end plates, two rhizoid bars respectively by clutch shaft bearing up and down and up and down the clutch shaft bearing seat be installed on separately the end plate, two worm gears are separately fixed at screw mandrel top separately, two slide blocks are installed in respectively on the two rhizoid bars of two worm gear belows, one end of two fixed blocks is rotationally connected by coupling shaft and separately the 3rd bearing and slide block respectively, the soil conductivity detector is installed between the other end of two fixed blocks, fix with adjusting knob, worm screw respectively by second bearing separately and separately second bearing seat be installed between the two end plates, second gear is fixed on the worm screw of first screw mandrel, one side, worm gear is meshed with worm screw, first stepper motor is fixed on the end plate of first screw mandrel, one side by the first stepping electric machine support, first gear is fixed on the turning axle of first stepper motor, first gear is meshed with second gear, second stepper motor is fixed on the slide block of first screw mandrel, one side, the 3rd gear is fixed on the turning axle of second stepper motor, the 4th gear is fixed on the slide block of a side, the 3rd gear and the 4th gear are meshed, driving the soil conductivity detector rotates, four castors are installed in the end plate bottom, and computer links to each other with the soil conductivity detector.
CN2010202276494U 2010-06-13 2010-06-13 Device of measuring electrical conductivity of cross section of soil Expired - Lifetime CN201724984U (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN2010202276494U CN201724984U (en) 2010-06-13 2010-06-13 Device of measuring electrical conductivity of cross section of soil

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN2010202276494U CN201724984U (en) 2010-06-13 2010-06-13 Device of measuring electrical conductivity of cross section of soil

Publications (1)

Publication Number Publication Date
CN201724984U true CN201724984U (en) 2011-01-26

Family

ID=43493324

Family Applications (1)

Application Number Title Priority Date Filing Date
CN2010202276494U Expired - Lifetime CN201724984U (en) 2010-06-13 2010-06-13 Device of measuring electrical conductivity of cross section of soil

Country Status (1)

Country Link
CN (1) CN201724984U (en)

Cited By (3)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN101871972A (en) * 2010-06-13 2010-10-27 浙江大学 Method and device for measuring conductivity of soil profile
CN104192182A (en) * 2014-07-12 2014-12-10 浙江大学 Lifting platform trolley system for containing EM38
CN113435640A (en) * 2021-06-24 2021-09-24 中国科学院东北地理与农业生态研究所 Method for predicting in-situ EC (soil EC) of soil in different plough layers of main growth period of rice in soda saline-alkali soil

Cited By (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN101871972A (en) * 2010-06-13 2010-10-27 浙江大学 Method and device for measuring conductivity of soil profile
CN104192182A (en) * 2014-07-12 2014-12-10 浙江大学 Lifting platform trolley system for containing EM38
CN104192182B (en) * 2014-07-12 2016-04-13 浙江大学 Place the lifting platform trolley system of EM38
CN113435640A (en) * 2021-06-24 2021-09-24 中国科学院东北地理与农业生态研究所 Method for predicting in-situ EC (soil EC) of soil in different plough layers of main growth period of rice in soda saline-alkali soil
CN113435640B (en) * 2021-06-24 2022-07-26 中国科学院东北地理与农业生态研究所 Method for predicting in-situ EC (environmental impact) of soils with different plough layers in main growth period of rice in soda saline-alkali soil

Similar Documents

Publication Publication Date Title
Cui et al. Modeling tree root diameter and biomass by ground-penetrating radar
CN102998029B (en) Multi-field information monitoring method for physical model of landslide evolution process
CN101344474B (en) Method for measuring porosity of soil
CN103174122B (en) Lateral stress pore pressure probe used for testing soil static lateral pressure coefficient
Donohue et al. Detection of soil compaction using seismic surface waves
CN102508303A (en) Advanced detection method for focusing chromatography induced polarization of underground engineering
CN201724984U (en) Device of measuring electrical conductivity of cross section of soil
CN110988999A (en) Detection method and system for analyzing pile foundation based on cross-hole resistivity method CT inversion imaging
CN206378448U (en) Polluted Soil detection arrangement of measuring-line structure based on comprehensive geophysical prospecting methods
CN101871972B (en) Method and device for measuring conductivity of soil profile
CN113267612B (en) Soil moisture content detection method, detection system and penetration device
CN113176337B (en) In-situ monitoring method, testing system and testing equipment for rigidity of soil body around pile
CN107462146B (en) Underground three-dimensional displacement measurement system and method based on multi-mutual inductance mechanism
CN107884015B (en) Lateral pipe soil action testing system and method with soil surface leveling device
CN103526736B (en) Foundation dynamic compaction strengthening quality three-dimensional continuous detection method
CN109868803B (en) Frost heaving stress detection device and detection method thereof
CN111521159B (en) Multifunctional sounding rod
CN102944607B (en) Rolling type movement transverse wave sensor and use method thereof
CN202645547U (en) High-resolution azimuthal resistivity dual laterolog tool
CN102507301A (en) Horizontal penetration type detecting and testing method of soil compaction degree
RU70995U1 (en) PROBE FOR MEASURING TEMPERATURE PROFILE
CN111257947B (en) Cross-hole resistivity karst cave detection method
CN110346247B (en) Mesoscale test determination method for bottom mud salt diffusion coefficient of hydraulic reclamation area
De Lara et al. Characterizing spatial variability in soil water content for precision irrigation management
Acworth et al. Monitoring soil moisture status in a Black Vertosol on the Liverpool Plains, NSW, using a combination of neutron scattering and electrical image methods

Legal Events

Date Code Title Description
C14 Grant of patent or utility model
GR01 Patent grant
AV01 Patent right actively abandoned

Granted publication date: 20110126

Effective date of abandoning: 20120104