CN113624634B - Method for estimating content of metal elements in buried environment - Google Patents

Method for estimating content of metal elements in buried environment Download PDF

Info

Publication number
CN113624634B
CN113624634B CN202110916447.3A CN202110916447A CN113624634B CN 113624634 B CN113624634 B CN 113624634B CN 202110916447 A CN202110916447 A CN 202110916447A CN 113624634 B CN113624634 B CN 113624634B
Authority
CN
China
Prior art keywords
slag
soil
buried
concentration
area
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.)
Active
Application number
CN202110916447.3A
Other languages
Chinese (zh)
Other versions
CN113624634A (en
Inventor
张金亮
李娜
栾旭伟
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.)
Beijing Normal University
Original Assignee
Beijing Normal University
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 Beijing Normal University filed Critical Beijing Normal University
Priority to CN202110916447.3A priority Critical patent/CN113624634B/en
Publication of CN113624634A publication Critical patent/CN113624634A/en
Application granted granted Critical
Publication of CN113624634B publication Critical patent/CN113624634B/en
Active legal-status Critical Current
Anticipated expiration legal-status Critical

Links

Images

Classifications

    • GPHYSICS
    • G01MEASURING; TESTING
    • G01NINVESTIGATING OR ANALYSING MATERIALS BY DETERMINING THEIR CHEMICAL OR PHYSICAL PROPERTIES
    • G01N5/00Analysing materials by weighing, e.g. weighing small particles separated from a gas or liquid

Landscapes

  • Physics & Mathematics (AREA)
  • Health & Medical Sciences (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Chemical & Material Sciences (AREA)
  • Analytical Chemistry (AREA)
  • Biochemistry (AREA)
  • General Health & Medical Sciences (AREA)
  • General Physics & Mathematics (AREA)
  • Immunology (AREA)
  • Pathology (AREA)
  • Geophysics And Detection Of Objects (AREA)

Abstract

The embodiment of the specification discloses a method for estimating the content of metal elements in a burial environment, which comprises the following steps: collecting underground buried soil in a buried area, and calculating the total mass of the underground soil; obtaining the slag concentration in the soil by an induced polarization method; determining the quality of the slag according to the total soil mass and the slag concentration; determining a first correlation between slag quality and metal yield; and determining the metal yield of the underground buried soil according to the first correlation and the slag quality. The invention realizes the calculation of the yield of the metal smelting products in the soil buried in the underground stratum, realizes the estimation of the yield of the metal smelting site, applies the geophysical method to the measurement of the metal content of the soil, widens the application of the geophysical exploration to the soil measurement, and has high accuracy, wide application range and great significance compared with a manual picking method.

Description

Method for estimating content of metal elements in buried environment
Technical Field
The application relates to the technical field of stratum detection, in particular to a method for estimating content of metal elements in a buried environment.
Background
In general, scientific researchers adopt a method for manually picking up slag by a designated sampling party, the method is only suitable for a research area with slag exposed on the ground surface and a small distribution range, large deviation is not avoided in manual picking, omission is easy, and a new method is urgently needed to be added. The former introduces the induced polarization method into the research of smelting site, but the method is used for detecting the specific position of the site, and the related research of quantitative calculation is not introduced.
Disclosure of Invention
In order to solve the above technical problem, the embodiments of the present specification are implemented as follows:
the embodiment of the specification provides a method for estimating the content of a metal element in a burial environment, which comprises the following steps:
collecting underground buried soil in a buried area, and calculating the total mass of the underground soil;
obtaining the slag concentration in the soil by an induced polarization method;
determining the quality of the slag according to the total soil mass and the slag concentration;
determining a first correlation between slag quality and metal yield;
and determining the metal yield of the underground buried soil according to the first correlation and the slag quality.
Optionally, the calculating the total mass of the underground soil specifically includes:
solving the volume of the soil in the buried area by using a volume formula;
and (4) solving the total soil mass by using a mass calculation formula.
Optionally, the obtaining of the slag concentration in the soil by the induced polarization method specifically includes:
carrying out induced polarization geophysical exploration on the buried region, and acquiring the chargeability of underground buried soil of the buried region;
determining a second correlation of chargeability and slag concentration;
and determining the slag concentration in the underground buried soil of the buried area according to the second correlation and the chargeability parameter.
Optionally, the performing induced polarization geophysical prospecting on the buried region specifically includes:
and (3) carrying out induced polarization geophysical exploration on the buried region by adopting a spectrum induced polarization instrument or a resistivity exploration instrument.
Optionally, determining the slag quality according to the total soil mass and the slag concentration specifically includes:
and calculating the quality of the slag in the buried area by using a slag quality formula and applying mathematical integral operation.
Optionally, the average polarizability value of the research area can be selected from the buried area with uniformly distributed slag, the slag concentration of the area is obtained according to the correlation function of polarizability and slag concentration, and then the total slag mass of the buried area is calculated by using the slag concentration.
Optionally, for a buried area with unevenly distributed slag, the polarizability of each coordinate point is different, so that the corresponding slag concentration is also different according to the correlation, the polarizability is a variable related to the coordinate, the corresponding slag concentration is also a variable related to the coordinate, and the slag quality in the whole research area is obtained according to an integral method.
Optionally, the second association relationship is expressed as follows: the formula is as follows:
p (x, y, z) ═ α C (x, y, z) + β or
C(x,y,z)=(P(x,y,z)-β)/α
Wherein, P is chargeability, is a variable related to coordinate points, P values corresponding to different coordinate points are different, the P values are obtained by measurement of an induced polarization method, C is the slag concentration, and alpha and beta are constants. Can be obtained by laboratory fitting.
Optionally, the acquisition manner of α and β is as follows:
sampling in a research area, and fitting the measured slag concentration of a sampling point with charging performance by using statistical software to obtain alpha and beta;
or making soil with different slag concentrations in a laboratory, measuring corresponding chargeability values under different slag concentrations, and fitting the measured values by using statistical software to obtain alpha and beta.
Optionally, the first association relationship is: the slag yield is 3-5 times the metal yield by mass.
The embodiment of the specification adopts at least one technical scheme which can achieve the following beneficial effects:
the invention realizes the calculation of the yield of the metal smelting products in the soil buried in the underground stratum, realizes the estimation of the yield of the metal smelting site, applies the geophysical method to the measurement of the metal content of the soil, widens the application of the geophysical exploration to the soil measurement, and has high accuracy, wide application range and great significance compared with a manual picking method.
Drawings
The accompanying drawings, which are included to provide a further understanding of the application and are incorporated in and constitute a part of this application, illustrate embodiment(s) of the application and together with the description serve to explain the application and not to limit the application. In the drawings:
fig. 1 is a schematic flow chart of a method for estimating the content of a metal element in a sequestration environment according to an embodiment of the present disclosure.
Detailed Description
In order to make the objects, technical solutions and advantages of the present application more apparent, the technical solutions of the present application will be described in detail and completely with reference to the following specific embodiments of the present application and the accompanying drawings. It should be apparent that the described embodiments are only some of the embodiments of the present application, and not all of the embodiments. All other embodiments, which can be derived by a person skilled in the art from the embodiments given herein without making any creative effort, shall fall within the protection scope of the present application.
The method quantitatively calculates the concentration of the slag by using an induced polarization method and supplements a research method of metal smelting sites. Aiming at ancient metal smelting sites buried deeply underground, the technology needs to estimate the smelting scale of the ancient smelting sites, namely the metal production amount, due to the requirements of scientific research.
The technical solutions provided by the embodiments of the present application are described in detail below with reference to the accompanying drawings.
Fig. 1 is a schematic flow chart of a method for estimating the content of a metal element in a sequestration environment according to an embodiment of the present disclosure. From the viewpoint of a program, the execution subject of the flow may be a program installed in an application server or an application client.
As shown in fig. 1, the process may include the following steps:
step 110: underground buried soil of the buried area is collected, and the total mass of the underground soil is calculated.
Optionally, the calculating the total mass of the underground soil specifically may include:
solving the volume of the soil in the buried area by using a volume formula;
and (4) solving the total soil mass by using a mass calculation formula.
And calculating the total volume of the soil in the buried area, wherein the length, the width and the exploration depth of the buried area are required to be measured, and the total volume of the soil in the buried area is obtained by multiplying the length, the width and the exploration depth.
And calculating the total soil mass of the buried area, wherein the total volume value is required to be utilized, and the total soil mass of the buried area is obtained by multiplying the total volume value by the soil density of the area. Wherein, the soil density can be obtained by looking up related geological data or measuring a soil sample in a laboratory.
Step 120: and obtaining the slag concentration in the soil by an induced polarization method.
Optionally, the obtaining of the slag concentration in the soil by the induced polarization method specifically includes:
carrying out induced polarization geophysical exploration on the buried region, and acquiring the chargeability of underground buried soil of the buried region;
determining a second correlation of chargeability and slag concentration;
and determining the slag concentration in the underground buried soil of the buried area according to the second correlation and the chargeability parameter.
Optionally, the second association relationship is expressed as follows: the formula is as follows:
p (x, y, z) ═ α C (x, y, z) + β or
C(x,y,z)=(P(x,y,z)-β)/α
Wherein, P is chargeability, is a variable related to coordinate points, P values corresponding to different coordinate points are different, the P values are obtained by measurement of an induced polarization method, C is the slag concentration, and alpha and beta are constants. Can be obtained by laboratory fitting.
Optionally, the acquisition manner of α and β is as follows:
sampling in a research area, and fitting the measured slag concentration of a sampling point with charging performance by using statistical software to obtain alpha and beta;
or making soil with different slag concentrations in a laboratory, measuring corresponding chargeability values under different slag concentrations, and fitting the measured values by using statistical software to obtain alpha and beta.
The method comprises the steps of self-preparing a soil sample, formulating soil samples with different slag concentrations by using slag and soil in a research area, measuring the chargeability (polarizability) of the soil with fixed slag concentration by using an induced polarization method testing instrument (such as a spectrum induced polarization instrument or a resistivity exploration instrument), and fitting a linear correlation relationship between a plurality of groups of chargeability and slag concentration data in statistical software.
Optionally, the performing induced polarization geophysical prospecting on the buried region specifically includes:
and (3) carrying out induced polarization geophysical exploration on the buried region by adopting a spectrum induced polarization instrument or a resistivity exploration instrument.
An exploration area and an exploration depth are determined before exploration, the used exploration instruments comprise but are not limited to a spectrum excitation polarimeter and a resistivity exploration instrument, the geophysical parameter required to be obtained by exploration is the chargeability (polarizability) of soil, the parameter is discrete data, numerical values of all points in the ground are different, and for a buried area with more uniform slag distribution, an average value can be selected for subsequent calculation. Data acquired by field exploration also needs to be imported with professional software for processing and removing useless information, and the software used comprises but is not limited to RES3DINV software.
Step 130: and determining the quality of the slag according to the total soil mass and the slag concentration.
Optionally, determining the slag quality according to the total soil mass and the slag concentration specifically includes:
and calculating the quality of the slag in the buried area by using a slag quality formula and applying mathematical integral operation.
Optionally, the average polarizability value of the research area can be selected from the buried area with uniformly distributed slag, the slag concentration of the area is obtained according to the correlation function of polarizability and slag concentration, and then the total slag mass of the buried area is calculated by using the slag concentration.
Optionally, for a buried area with unevenly distributed slag, the polarizability of each coordinate point is different, so that the corresponding slag concentration is also different according to the correlation, the polarizability is a variable related to the coordinate, the corresponding slag concentration is also a variable related to the coordinate, and the slag quality in the whole research area is obtained according to an integral method.
Step 140: a first correlation of slag quality and metal production is determined.
Optionally, the first association relationship is: the output of slag is 3-5 times of the metal output by mass, and smelting technology, raw materials and the like influence the ratio.
Step 150: and determining the metal yield of the underground buried soil according to the first correlation and the slag quality.
Based on the method of fig. 1, the embodiments of the present specification also provide some specific implementations of the method, which are described below.
The invention relates to a novel method for estimating metal yield in stratum burial by utilizing a geophysical theory, which introduces an induced polarization method geophysical exploration means to estimate the metal yield of an ancient metal smelting site. The calculation method mainly comprises the steps of measuring the induced polarization parameter charging rate of a soil sample and the concentration of the residual smelting slag in the soil sample in a laboratory, and fitting to generate a linear correlation relationship between the induced polarization parameter charging rate and the concentration of the residual smelting slag in the soil sample; carrying out induced polarization geophysical exploration on a slag buried area of the whole research area, and collecting chargeability parameters of underground buried soil of the buried area; solving the volume of the soil in the buried area by using a volume formula; calculating the total soil mass by using a mass calculation formula; calculating the quality of the smelting slag in the buried area by using a slag quality formula and applying mathematical integral operation; based on the correlation between slag quality and total metal production (Eschenlohr, 1991; Senneels, 1993; Leroy, 2001), the metal yield of the ancient metal smelting site in the year can be estimated and the production scale thereof can be evaluated.
The key technology of the scheme comprises the following two points:
(1) fitting to obtain a linear correlation between polarizability and slag concentration
And measuring the induced polarization parameter charging rate of the soil sample and the concentration of the residual smelting slag in the soil sample in a laboratory, and fitting to generate a linear correlation relationship between the induced polarization parameter charging rate and the concentration of the residual smelting slag in the soil sample. The method comprises the steps of self-preparing a soil sample, formulating the soil sample with different slag concentrations by using slag and soil in a research area, measuring the chargeability (polarizability) of the soil with fixed slag concentration by using an induced polarization method testing instrument (such as a spectrum induced polarization instrument or a resistivity exploration instrument), and fitting a linear correlation relationship between a plurality of groups of chargeability and slag concentration data in statistical software.
(2) Calculating the total mass of the slag
The average polarizability value of the research area can be selected from the buried area with uniformly distributed slag, the slag concentration (which is a constant value) of the area is obtained according to the correlation function of polarizability and slag concentration, and then the total slag mass of the buried area is calculated by using the constant value. For the buried areas with unevenly distributed slag, the polarizability of each coordinate point is different, so the corresponding slag concentration is different according to the correlation relationship, the polarizability is a variable related to the coordinate, the corresponding slag concentration is a variable related to the coordinate, and the slag quality in the whole research area needs to be obtained according to an integral method.
The specific implementation mode is as follows:
1. estimating metal production capacity of a smelting site
For ancient smelting sites, the metal yield cannot be directly obtained, and most of the metal yield can be directly found at present as smelting residual substances, such as smelting slag. Generally, the output of the slag is about 3 to 5 times of the metal by mass, and smelting technology, raw materials and the like influence the ratio, or international smelting standards can be directly referred to (Eschenlohr, 1991; Senneels, 1993; Leroy, 2001), so that the metal output (production scale) of the site in the current year can be indirectly obtained by checking the quality of the slag remained in the site.
The problem is shifted to finding out the mass M of slag remaining in the site.
2. Obtaining the mass M of the slag in the underground soil
The calculation formula of the total mass M of the slag in the soil is as follows:
m is C M formula (1)
Wherein C is the slag concentration in the soil, and m is the total mass of the soil.
The total soil mass m calculation formula is as follows:
formula (2) where m is ρ ═ V
Wherein rho is the soil density, the densities of different research areas are different, and the density can be obtained by looking up geological data or by using the soil density under the general condition. And V is the soil volume of the research area.
V ═ a ═ b ═ c formula (3)
Wherein, a, b and c are respectively the length, width and depth of the calculated soil body, and can be obtained by field measurement.
The problem is shifted to finding out the slag concentration C of the slag remaining in the underground site.
3. Obtaining the slag concentration C in the soil
The physical parameter obtained by the induced polarization method through direct measurement is chargeability parameter, P for short.
There is a linear correlation between chargeability P and slag concentration C (Florsch, 2011) with the following formula:
p (x, y, z) ═ α ═ C (x, y, z) + β formula (4) or
C (x, y, z) ═ P (x, y, z) - β)/α formula (5)
Wherein, P is chargeability, is a variable related to coordinate points, P values corresponding to different coordinate points are different, and the P values are obtained by measurement of an induced polarization method; c is the slag concentration; the constants α and β can be obtained by laboratory fitting.
4. Fitting constants alpha and beta
Sampling in a research area, measuring the slag concentration C and the chargeability P of a sampling point, fitting by using statistical software to obtain a linear correlation relation between P and C, and substituting the values of alpha and beta in the relation into a formula (5).
Or directly setting the soil with different slag concentrations in a laboratory, measuring corresponding chargeability values under different slag concentrations, and fitting the measured values by using statistical software.
5. Determining the mass M of the slag
Since P is a variable related to coordinates (x, y, z) and the concentration C is also a variable related to (x, y, z), finding the slag mass in the investigation region requires using an integral form to convert equation (1) to an integral form related to (x, y, z) as follows:
m (x, y, z) ═ z ^ c integral whole number of events (6)
Substituting the formula (5) C into the formula (6), substituting the formula (2) obtained M into the formula (6), and integrating to obtain the total slag mass M of the research area. And comparing M with the international standard to obtain the total metal smelting amount in ancient times of the research area.
It should also be noted that the terms "comprises," "comprising," or any other variation thereof, are intended to cover a non-exclusive inclusion, such that a process, method, article, or apparatus that comprises a list of elements does not include only those elements but may include other elements not expressly listed or inherent to such process, method, article, or apparatus. Without further limitation, an element defined by the phrase "comprising an … …" does not exclude the presence of other like elements in a process, method, article, or apparatus that comprises the element.
The embodiments in the present specification are described in a progressive manner, and the same and similar parts among the embodiments are referred to each other, and each embodiment focuses on the differences from the other embodiments. In particular, for the system embodiment, since it is substantially similar to the method embodiment, the description is simple, and for the relevant points, reference may be made to the partial description of the method embodiment.
The above description is only an example of the present application and is not intended to limit the present application. Various modifications and changes may occur to those skilled in the art. Any modification, equivalent replacement, improvement, etc. made within the spirit and principle of the present application should be included in the scope of the claims of the present application.

Claims (10)

1. A method of estimating the content of metallic elements in a sequestration environment, said method comprising:
collecting underground buried soil in a buried area, and calculating the total mass of the underground soil;
obtaining the slag concentration in the soil by an induced polarization method;
determining the quality of the slag according to the total soil mass and the slag concentration;
determining a first correlation between slag quality and metal yield;
and determining the metal yield of the underground buried soil according to the first correlation and the slag quality.
2. The method of claim 1, wherein the calculating the total mass of the subsurface soil comprises:
solving the volume of the soil in the buried area by using a volume formula;
and (4) solving the total soil mass by using a mass calculation formula.
3. The method according to claim 1, wherein the obtaining of the slag concentration in the soil by the induced polarization method specifically comprises:
carrying out induced polarization geophysical exploration on the buried region, and acquiring the chargeability of underground buried soil of the buried region;
determining a second correlation of chargeability and slag concentration;
and determining the slag concentration in the underground buried soil of the buried area according to the second correlation and the chargeability parameter.
4. The method of claim 3, wherein the performing induced polarization geophysical surveys of the buried region comprises:
and (3) carrying out induced polarization geophysical exploration on the buried region by adopting a spectrum induced polarization instrument or a resistivity exploration instrument.
5. The method of claim 1, wherein determining the slag mass from the total soil mass and the slag concentration comprises:
and calculating the quality of the slag in the buried area by using a slag quality formula and applying mathematical integral operation.
6. The method of claim 1, wherein the average polarizability value of the area under investigation is selected from a buried area having a uniform slag distribution, the slag concentration in the area is obtained as a function of polarizability with respect to slag concentration, and the slag concentration is used to calculate the total mass of slag in the buried area.
7. The method of claim 1, wherein for a buried area with unevenly distributed slag, the polarizability of each coordinate point is different, and therefore the corresponding slag concentration is also different according to the correlation, the polarizability is a variable with respect to the coordinate, and the corresponding slag concentration is also a variable with respect to the coordinate, and the quality of the slag in the entire area of interest is determined by an integral method.
8. The method of claim 3, wherein the second association is represented as follows: the formula is as follows:
p (x, y, z) ═ α C (x, y, z) + β or
C(x,y,z)=(P(x,y,z)-β)/α
Wherein, P is chargeability, is a variable related to coordinate points, P values corresponding to different coordinate points are different, the P values are obtained by measurement of an induced polarization method, C is the slag concentration, and alpha and beta are constants which can be obtained by fitting in a laboratory.
9. The method of claim 8, wherein α and β are obtained as follows:
sampling in a research area, and fitting the measured slag concentration of a sampling point with charging performance by using statistical software to obtain alpha and beta;
or making soil with different slag concentrations in a laboratory, measuring corresponding chargeability values under different slag concentrations, and fitting the measured values by using statistical software to obtain alpha and beta.
10. The method of claim 1, wherein the first correlation is: the slag yield is 3-5 times the metal yield by mass.
CN202110916447.3A 2021-08-11 2021-08-11 Method for estimating content of metal elements in buried environment Active CN113624634B (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN202110916447.3A CN113624634B (en) 2021-08-11 2021-08-11 Method for estimating content of metal elements in buried environment

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN202110916447.3A CN113624634B (en) 2021-08-11 2021-08-11 Method for estimating content of metal elements in buried environment

Publications (2)

Publication Number Publication Date
CN113624634A CN113624634A (en) 2021-11-09
CN113624634B true CN113624634B (en) 2022-04-22

Family

ID=78384157

Family Applications (1)

Application Number Title Priority Date Filing Date
CN202110916447.3A Active CN113624634B (en) 2021-08-11 2021-08-11 Method for estimating content of metal elements in buried environment

Country Status (1)

Country Link
CN (1) CN113624634B (en)

Citations (8)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US6147497A (en) * 1998-06-29 2000-11-14 The Regents Of The University Of California Using electrical impedance tomography to map subsurface hydraulic conductivity
CN103995301A (en) * 2014-05-07 2014-08-20 中国石油天然气集团公司 Method and device for evaluating total organic carbon content in shale gas reservoir
CN104190698A (en) * 2014-08-21 2014-12-10 中国科学院南京土壤研究所 Method for restoring clayed soil of high-load heavy metal polluted site
CN105652329A (en) * 2016-02-04 2016-06-08 中国科学院地质与地球物理研究所 Method and device for evaluating apparent water inflow of coal seam roof
CN110068867A (en) * 2019-05-08 2019-07-30 桂林理工大学 A kind of induced polarization method monitoring heavy metal containing sewage leakage method of pre-buried measuring electrode
CN110836923A (en) * 2019-11-26 2020-02-25 暨南大学 Soil heavy metal concentration estimation method
CN111239851A (en) * 2020-03-18 2020-06-05 西安西北有色物化探总队有限公司 Northern bauxite positioning method and device
CN113204905A (en) * 2021-05-08 2021-08-03 桂林理工大学 Contact induced polarization finite element numerical simulation method

Patent Citations (8)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US6147497A (en) * 1998-06-29 2000-11-14 The Regents Of The University Of California Using electrical impedance tomography to map subsurface hydraulic conductivity
CN103995301A (en) * 2014-05-07 2014-08-20 中国石油天然气集团公司 Method and device for evaluating total organic carbon content in shale gas reservoir
CN104190698A (en) * 2014-08-21 2014-12-10 中国科学院南京土壤研究所 Method for restoring clayed soil of high-load heavy metal polluted site
CN105652329A (en) * 2016-02-04 2016-06-08 中国科学院地质与地球物理研究所 Method and device for evaluating apparent water inflow of coal seam roof
CN110068867A (en) * 2019-05-08 2019-07-30 桂林理工大学 A kind of induced polarization method monitoring heavy metal containing sewage leakage method of pre-buried measuring electrode
CN110836923A (en) * 2019-11-26 2020-02-25 暨南大学 Soil heavy metal concentration estimation method
CN111239851A (en) * 2020-03-18 2020-06-05 西安西北有色物化探总队有限公司 Northern bauxite positioning method and device
CN113204905A (en) * 2021-05-08 2021-08-03 桂林理工大学 Contact induced polarization finite element numerical simulation method

Non-Patent Citations (2)

* Cited by examiner, † Cited by third party
Title
深穿透地球化学方法对比研究――以内蒙古花敖包特铅锌矿为例;聂兰仕等;《地质通报》;20071215(第12期);第1574-1578页 *
激发极化和化探方法寻找锡多金属矿的效果;李建勋;《物探与化探》;19840820(第04期);第223-226页 *

Also Published As

Publication number Publication date
CN113624634A (en) 2021-11-09

Similar Documents

Publication Publication Date Title
CN105221133B (en) A kind of method and apparatus that content of organic carbon of hydrocarbon source rock is determined based on well logging multi-parameter
Webster et al. Soil transect correlograms of north Oxfordshire and their interpretation
Rhoades et al. Determining salinity in field soils with soil resistance measurements
Horne et al. Integrated single crystal laser ablation U/Pb and (U–Th)/He dating of detrital accessory minerals–Proof-of-concept studies of titanites and zircons from the Fish Canyon tuff
CN110531054B (en) Soil organic carbon prediction uncertainty estimation method based on Bootstrap sampling
CN102265188B (en) Method for quantitatively separating the effects of electromagnetic induction and induced polarization
McKinnon Analysis of stress measurements using a numerical model methodology
Salter et al. THE INFLUENCE OF TEXTURE ON THE MOISTURE CHARACTERISTICS OF SOILS: IV. A METHOD OF ESTIMATING THE AVAILABLE‐WATER CAPACITIES OF PROFILES IN THE FIELD
Nagy et al. Continuous field soil moisture content mapping by means of apparent electrical conductivity (ECa) measurement
Jaumann et al. Soil hydraulic material properties and layered architecture from time-lapse GPR
CN110793923A (en) Hyperspectral soil data acquisition and analysis method based on mobile phone
CN115292890A (en) Site soil pollutant concentration three-dimensional space prediction method based on multi-source auxiliary data development
Li et al. Characterizing soil losses in China using data of 137Cs inventories and erosion plots
Marsch et al. Comparative evaluation of statistical and fractal approaches for JRC calculation based on a large dataset of natural rock traces
CN113624634B (en) Method for estimating content of metal elements in buried environment
Biswas et al. Curvelet transform to study scale-dependent anisotropic soil spatial variation
CN109143405B (en) A kind of observation system efficiently sampling uniformity quantitative evaluation method
Beardsmore et al. A fourier spectral method to measure the thermal diffusivity of soil
Selzer et al. RaDeCC Reader: Fast, accurate and automated data processing for Radium Delayed Coincidence Counting systems
CN105653854A (en) Method and apparatus for calculating organic carbon content of carbonate source rock
CN113552075A (en) Gold geochemical element inversion method and system
CN111221043B (en) Working parameter optimization method of passive source electric field method
CN113590733A (en) Method for estimating biomass on land by using regional herbaceous swamp vegetation
Stephan et al. Adding realistic noise models to synthetic ground‐penetrating radar data
CN114199856A (en) Method for rapidly calibrating element content ratio of laser-induced breakdown spectroscopy

Legal Events

Date Code Title Description
PB01 Publication
PB01 Publication
SE01 Entry into force of request for substantive examination
SE01 Entry into force of request for substantive examination
GR01 Patent grant
GR01 Patent grant