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Identifying the plough pan position on cultivated soils by measurements of electrical resistivity and penetration resistance

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F17%3A00312697" target="_blank" >RIV/68407700:21110/17:00312697 - isvavai.cz</a>

  • Výsledek na webu

    <a href="http://www.sciencedirect.com/science/article/pii/S0167198717301356" target="_blank" >http://www.sciencedirect.com/science/article/pii/S0167198717301356</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.still.2017.07.008" target="_blank" >10.1016/j.still.2017.07.008</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Identifying the plough pan position on cultivated soils by measurements of electrical resistivity and penetration resistance

  • Popis výsledku v původním jazyce

    Long term tillage has led to soil profile degradation in many cultivated fields. The topsoil is disturbed by plowing. The movement of fine particles from the topsoil to the subsoil and direct pressure from agricultural machinery create an abrupt delineation in the form of a plough pan with very low permeability. The plough pan prevents water infiltrating deeper into the soil profile and reduces the water supply to the lower layers. The plough pan also has a negative effect on the root growth of the crop, leading to a reduced yield. In this paper we discuss the feasibility of using electrical resistivity tomography and penetrometry to identify the presence and the position of plough pans, and also their spatial uniformity, on two fields with different tillage depths. Electrical resistivity measurements were subjected to a comparison with soil physical characteristics, such as soil water content, porosity and bulk density. Standard statistical and geostatistical methods were used. Electrical resistivity tomography seems to be an attractive method that offers a faster and more efficient method than standard invasive soil sampling for obtaining continuous information about the plough pan. It has been shown that the position of a compacted layer within the soil profile can be identified reasonably well by combining electrical resistivity data and penetration resistance data. The semivariogram showed higher variation by orders of magnitude in the topsoil than in the subsoil. This suggests macroscopic homogeneity of the compacted layer formatted in the subsoil in two differently tilled fields. We conclude that a short span between the electrodes should be used (app 10 cm) in order to observe the shallow positioned plough pan clearly.

  • Název v anglickém jazyce

    Identifying the plough pan position on cultivated soils by measurements of electrical resistivity and penetration resistance

  • Popis výsledku anglicky

    Long term tillage has led to soil profile degradation in many cultivated fields. The topsoil is disturbed by plowing. The movement of fine particles from the topsoil to the subsoil and direct pressure from agricultural machinery create an abrupt delineation in the form of a plough pan with very low permeability. The plough pan prevents water infiltrating deeper into the soil profile and reduces the water supply to the lower layers. The plough pan also has a negative effect on the root growth of the crop, leading to a reduced yield. In this paper we discuss the feasibility of using electrical resistivity tomography and penetrometry to identify the presence and the position of plough pans, and also their spatial uniformity, on two fields with different tillage depths. Electrical resistivity measurements were subjected to a comparison with soil physical characteristics, such as soil water content, porosity and bulk density. Standard statistical and geostatistical methods were used. Electrical resistivity tomography seems to be an attractive method that offers a faster and more efficient method than standard invasive soil sampling for obtaining continuous information about the plough pan. It has been shown that the position of a compacted layer within the soil profile can be identified reasonably well by combining electrical resistivity data and penetration resistance data. The semivariogram showed higher variation by orders of magnitude in the topsoil than in the subsoil. This suggests macroscopic homogeneity of the compacted layer formatted in the subsoil in two differently tilled fields. We conclude that a short span between the electrodes should be used (app 10 cm) in order to observe the shallow positioned plough pan clearly.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    40104 - Soil science

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Ostatní

  • Rok uplatnění

    2017

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Soil & Tillage Research

  • ISSN

    0167-1987

  • e-ISSN

    1879-3444

  • Svazek periodika

    174

  • Číslo periodika v rámci svazku

    December

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    10

  • Strana od-do

    231-240

  • Kód UT WoS článku

    000412265800024

  • EID výsledku v databázi Scopus

    2-s2.0-85027881738