Comparison of Methods for Soil Moisture Content Measurement Based on Field and Laboratory Data

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F15%3A00235381" target="_blank" >RIV/68407700:21110/15:00235381 - isvavai.cz</a>

Výsledek na webu

<a href="http://cest.gnest.org/cest15proceedings/public_html/papers/cest2015_00161_poster_paper.pdf" target="_blank" >http://cest.gnest.org/cest15proceedings/public_html/papers/cest2015_00161_poster_paper.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Comparison of Methods for Soil Moisture Content Measurement Based on Field and Laboratory Data

Popis výsledku v původním jazyce

Application of rainfall simulations is one of the most important experiments for purposes of a detail description of runoff and soil erosion processes. Both mentioned types of processes are highly dependent on initial soil moisture content which affectsmainly infiltration rate and stability of aggregates. It is therefore crucial to measure the initial soil moisture content before each simulation in order to evaluate measured data correctly. Additionally, the record of changes in soil moisture content in time can be very helpful for purposes of detail description of mentioned processes or for purposes of calibration of different models. In this paper, different procedures and types of sensors are discussed from the point of view of its accuracy and applicability. In detail, gravimetric method which is considered as the most accurate is compared to measurements using two different types of sensors and measurement techniques. These are ThetaProbe ML2x and TMS3 sensors. The comparison is

Název v anglickém jazyce

Comparison of Methods for Soil Moisture Content Measurement Based on Field and Laboratory Data

Popis výsledku anglicky

Application of rainfall simulations is one of the most important experiments for purposes of a detail description of runoff and soil erosion processes. Both mentioned types of processes are highly dependent on initial soil moisture content which affectsmainly infiltration rate and stability of aggregates. It is therefore crucial to measure the initial soil moisture content before each simulation in order to evaluate measured data correctly. Additionally, the record of changes in soil moisture content in time can be very helpful for purposes of detail description of mentioned processes or for purposes of calibration of different models. In this paper, different procedures and types of sensors are discussed from the point of view of its accuracy and applicability. In detail, gravimetric method which is considered as the most accurate is compared to measurements using two different types of sensors and measurement techniques. These are ThetaProbe ML2x and TMS3 sensors. The comparison is

Druh

D - Stať ve sborníku

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název statě ve sborníku

Proceedings of the 14th International Conference on Environmental Science and Technology

ISBN

978-960-7475-52-7

ISSN

1106-5516

e-ISSN

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Počet stran výsledku

5

Strana od-do

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Název nakladatele

University of the Aegean

Místo vydání

Aegean

Místo konání akce

Rhodos

Datum konání akce

3. 9. 2015

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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