Počet záznamů: 1
Grass cover influences hydrophysical parameters and heterogeneity of water flow in a sandy soil
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SYSNO ASEP 0366295 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Grass cover influences hydrophysical parameters and heterogeneity of water flow in a sandy soil Tvůrce(i) Lichner, Ľ. (SK)
Eldridge, D. J. (AU)
Schacht, K. (DE)
Zhukova, N. (GE)
Holko, L. (SK)
Šír, Miloslav (UH-J) ORCID, RID, SAI
Pecho, Jozef (UFA-U) RIDZdroj.dok. Pedosphere. - : Elsevier - ISSN 1002-0160
Roč. 21, č. 6 (2011), s. 719-729Poč.str. 11 s. Jazyk dok. eng - angličtina Země vyd. CN - Čína Klíč. slova dye tracing ; grassland soil ; hydrophobicity ; infiltration ; preferential flow Vědní obor RIV DA - Hydrologie a limnologie CEP SP/1A6/151/07 GA MŽP - Ministerstvo životního prostředí CEZ AV0Z20600510 - UH-J (2005-2011) AV0Z30420517 - UFA-U, BC-A (2005-2011) UT WOS 000297600300005 DOI 10.1016/S1002-0160(11)60175-6 Anotace Two sites were selected to quantify the influence of grass cover on hydrophysical parameters and heterogeneity of water flow in a sandy soil emerging during a heavy rain following a long hot, dry period. A control soil (pure sand) with limited impact of vegetation or organic matter was obtained by sampling at 50 cm depth beneath a glade area, and a grassland soil was covered in a 10 cm thick humic layer and colonised by grasses. The persistence of water repellency was measured using the water drop penetration time test, sorptivity and unsaturated hydraulic conductivity using a mini disk infiltrometer, and saturated hydraulic conductivity using a double-ring infiltrometer. Dye tracer experiments were used to assess the heterogeneity of water flow, and both the modified method for estimating effective cross section and an original method for assessing the degree of preferential flow were used to quantify this heterogeneity from the images of dyed soil profiles. Pracoviště Ústav pro hydrodynamiku Kontakt Soňa Hnilicová, hnilicova@ih.cas.cz, Tel.: 233 109 003 Rok sběru 2012
Počet záznamů: 1