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геофизическое оборудование

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Объекты и методы

Объектами исследования послужили  различные почвенные массивы  (рис.1)  пахотных супесчаных почв Дмитровского района Московской области, расположенных на небольшом удалении друг от друга в пределах II–III ярусов  макросклона северной экспозиции Клинско-Дмитровской гряды, ограниченной уступом к древнеозерному расширению  долины пр. Яхрома (Яхромская пойма). Площадь ключевых массивов варьировала от десятых долей га до 20 га. 

ОЦЕНКА ОКУЛЬТУРЕННОСТИ ЛЕГКИХ ПОЧВ ГУМИДНОЙ ЗОНЫ ЕВРОПЕЙСКОЙ ЧАСТИ РОССИИ ЭЛЕКТРОФИЗИЧЕСКИМИ МЕТОДАМИ

ПОЗДНЯКОВ А.И., ЕЛИСЕЕВ П.И., ГОЛОВКО Л.А., ПОЗДНЯКОВ Л.А., ДУБРОВА М.С., МАКАРОВА Е.П.

Электрическое сопротивление  легких антропогенно-преобразованных почв  гумидной зоны - комплексный показатель, который в основном зависит от трех  базовых свойств, характеризующих твердую фазу почв – гранулометрического состава (содержания физической глины), содержания общего углерода и емкости катионного обмена.

Местоположение

Yahroma Valley Dmitrov, MOS
Russia
56° 23' 26.0808" N, 37° 20' 49.1712" E

Evaluating cultivation level of sandy soils in European Russia with electro-geophysical methods

Electrical resistivity vs cultivation degree of sandy soils Update: Full PDF of the paper is now available!

Electrical resistivity of cultivated sandy soils of humid areas is a complex characteristic based on three fundamental properties of soil matrix, such as soil texture, total organic matter (carbon content) and cation exchange capacity (CEC). Relationship of electrical resistivity (ER) with those properties has been approximated with exponential equation ER=a*exp(-b*x), where x is any of the properties above. The correlation coefficients for ER as function of CEC, texture, or organic matter were between 0.82 and 0.91 for the soils of Klin-Dmitrov watershed near Moscow and Kirov, which suggests their applicability for other humid areas. We present a new approach to approximate exponential relationship ER=a*exp(b*x) with a linear “piece-wise” function based on the age of cultivation for each field.This approach was used to develop management zones based on ER to separate uniform areas of similar organic matter, CEC and clay content. Those basic properties are the foundation of soil fertility in humid areas. They influence biomass and bioactivity of soil microorganisms, thus the exponential relationship between ER and soil microorganisms was also observed. The approach based of electrical resistivity or conductivity was used to evaluate fertility and degree of cultivation of sandy soils in humid areas and for detail soil mapping and delineation of management zones in adaptive precision agriculture. The field and laboratory electrical geophysical methods are recommended for quick and accurate soil mapping and management in sustainable farming.

*at SAGEEP 2013, March 17-21 in Denver, CO, Larisa Golovko, Ph.D. will also present "Basic Theory of Measuring Electrical Resistivity, Conductivity and Self-Potential in Soils and Plants" with LandMapper ERM-02 and other commercially available geophysical equipment at post-conference workshop "Agricultural Geophysics: Theory and Methods".
SAGEEP 2013 logo
Cite this presentation as:

Anatoly Pozdnyakov, P.I. Eliseev, Larisa Golovko, Lev A. Pozdnyakov, Maria S. Dubrova, and E.P. Makarova. “Evaluating Cultivation Level of Sandy Soils in European Russia with Electro-geophysical Methods.” In New Views of the Earth. Denver, CO: Environmental and Engineering Geophysical Society, 2013. http://www.eegs.org/AnnualMeetingSAGEEP/SAGEEP2013/SessionsAbstracts.aspx

 

Locations

Denver 39° 44' 15.2412" N, 104° 59' 4.9848" W
Klin, MOS 56° 19' 18.5304" N, 36° 42' 30.8772" E
KIR 58° 36' 16.8984" N, 49° 39' 58.5504" E

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Online Manuals and Textbooks on Electrical Geophysics

LandMapper ERM-01 holiday sale - while supplies last!

We wish all our customers, friends, and collegues Merry Christmas, Happy New Year and wonderful holiday season!LandMapper is portable and scalable geophysical device

It has been a remarkable year for Landviser! We’ve completed several exciting projects with the focus on expanding capabilities of our LandMapper geophysical devices and helped many of our customers with their research. Our LandMapper geophysical devices have been gaining popularity around the globe. To extend our warmest Holiday wishes we are offering unprecidented discount of 20% on basic ERM-01 model from the current price of $1579. The new reduced price for ERM-01 of $1263 will be in effect until December 31, 2012 or while supplies last. Regular educational and dealers's discounts are still apply on the top of newly reduced price as stated in 

Current complete catalog of Landviser, LLC

To claim your ERM-01 now at a discounted price, email or call us (+1-609-412-0555) and mention promotion code 2012-12-ERM01. This offer is "first come, first serve" and is only available on pre-paid terms via credit card or wire transfer.Tax Deduction Info on www.Section179.Org!

Special Note for USA customers: Landviser's equipment and software qualify for tax deduction under Section 179. You still have time to purchase ERM-01, ERM-02 or RES2DINV/RES3DINV in 2012, before this deduction expires!

Landviser, LLC develops and sells portable handheld geophysical devices, Landmapper ERM-01 and ERM-02 for measuring electrical properties (electrical resistivity, conductivity, and potential)  in soils, plants and other semisolid and liquid media since 2003. This equipment is small, fully computer-integrated, and easy to use. It is very competitively priced and come handy many environmental, archaeological and agricultural applications, especially mapping and monitoring soil salinity and pollution. Information flyers can be downloaded from the links below:

More information on applications of both models is available in free publication in FastTIMES magazine:

Golovko, Larisa, Anatoly Pozdnyakov, and Antonina Pozdnyakova. “LandMapper ERM-02: Handheld Meter for Near-Surface Electrical Geophysical Surveys.” FastTIMES (EEGS) 15, no. 4 - Agriculture: A Budding Field in Geophysics (December 2010): 85–93. http://www.landviser.net/webfm_send/69

Местоположение

Landviser LLC Houston 29° 45' 36.6948" N, 95° 22' 9.804" W

LandMapper ERM-02: handheld meter for near-surface electrical geophysical surveys (FastTIMES December 2010)

was published in December, 2010 issue of FastTIMES, online peer-reviewed journal of EEGS. To cite this publication use:FastTIMES dec 2010 Agriculture: A budding field in Geophysics

Golovko, Larisa, Anatoly Pozdnyakov, and Antonina Pozdnyakova. “LandMapper ERM-02: Handheld Meter for Near-Surface Electrical Geophysical Surveys.” FastTIMES (EEGS) 15, no. 4 - Agriculture: A Budding Field in Geophysics (December 2010): 85–93. http://www.landviser.net/webfm_send/69

Registered users can download PDF of full text of proceedings paper from our website. Or browse online version below and leave your comments. You might also like to go to EEGS website to get PDFs of other publications on applications of geophysics to near-surface environmental problems published in this popular FREE online scientific magazine.

Abstract

On-the-go sensors, designed to measure soil electrical resistivity (ER) or electrical conductivity (EC) are vital for faster non-destructive soil mapping in precision agriculture, civil and environmental engineering, archaeology and other near-surface applications. Compared with electromagnetic methods and ground penetrating radar, methods of EC/ER measured with direct current and four-electrode probe have fewer limitations and were successfully applied on clayish and saline soils as well as on highly resistive sandy soils, such as Alfisols and Spodosols. However, commercially available contact devices, which utilize a four-electrode principle, are bulky, very expensive, and can be used only on fallow fields. Multi-electrode ER-imaging systems applied in deep geophysical explorations are heavy, cumbersome and their use is usually cost-prohibited in many near-surface applications, such as forestry, archaeology, environmental site assessment and cleanup, and in agricultural surveys on farms growing perennial horticultural crops, vegetables, or turf-grass. In such applications there is a need for accurate, portable, low-cost device to quickly check resistivity of the ground on-a-spot, especially on the sites non-accessible with heavy machinery.

Местоположение

Laramie, WY 41° 18' 40.9212" N, 105° 35' 27.9636" W

Электрофизика почв и не только - лекция

Лопата иногда представляется неотъемлемым атрибутом практикующего почвоведа. Однако почвовед может выглядеть и по-другому.

В этом случае его инструментом становится электронный прибор и моток проводов. В своей лекции я постараюсь рассказать, какие возможности открывают перед почвоведом электрофизические методы, где-то дополняя уже ставшие классическими способы обследования почв, а где-то являющиеся и единственным методом, которым можно решить поставленные задачи.

References

Bedmar, A.P., and Araguás, L.A., 2002, Detection and prevention of leaks from dams: Taylor & Francis, Exton, PA.

Carrow, R.N., and Duncan, R.R., 2004, Soil salinity monitoring: present and future: Golf course management, no. November, p. 89-92.

Corwin, R., 1990, The self-potential method for environmental and engineering applications: Geotechnical and Environmental Geophysics, Soc. Expl. Geophysics, Tulsa, OK, p. 127-143.

Electrical potential differences between soil horizons

The natural electrical potentials (stationary and fluctuating) in soils were studied by our group for last 40 years and the results were summarized and presented on 17th World Congress of Soil Science (Pozdnyakov and Pozdnyakova, 2002). The largest electrical potential differences were observed between soil horizons drastically different in physical and chemical properties. In most soils topsoil has higher electrical potentials than subsoil.

Special instrumentation for soil SP method is needed

solid state Ag-AgCl electrodesLandMapper ERM-02, in addition to electrical conductivity and resistivity measurements also allows non-invasively measure natural electrical potentials in soils and plants when two special non-polarizing electrodes are connected to MN terminals (Figure 3).

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