中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hydrological behaviour of microbiotic crusts on sand dunes: Example from NW China comparing infiltration in crusted and crust-removed soil

文献类型:期刊论文

作者Coppola, A.1,3; Basile, A.3; Wang, X.2; Comegna, V.1; Tedeschi, A.3; Mele, G.3; Comegna, A.1
刊名SOIL & TILLAGE RESEARCH
出版日期2011-12-01
卷号117页码:34-43
关键词Microbiotic crusts Hydraulic properties Sand dune erosion Tension infiltrometer method Numerical simulations
ISSN号0167-1987
DOI10.1016/j.still.2011.08.003
通讯作者Coppola, A.(antonio.coppola@unibas.it)
英文摘要Biological soil crusts are important microbiotic communities which are considered a key factor in combating desertification in terms of sand dune remobilitation. Because of their greater concentration of clay, silt and hydrophobic organic matter, they create a physical discontinuity in surface profile which potentially contribute to variability in soil hydrology of arid and semiarid land and should be considered in the development of hydrological and erosion models. However, until recently limited inconclusive research has been conducted to determine the functional relationship between soil and microbiotic crusts. We investigated the influence of microbiotic crust on hydrological behaviour of crusted sand dunes in NW China. The infiltration data on a crusted and crust-removed sand dune were obtained with dish permeameter which was not moved during the measurement at a sequence of nominal pressure head values, h, of -1, -4, -7, -10, -18 cm. Hydraulic conductivity K(h) was measured by steady-state infiltration experiments and piece-wise application of the exponential relation between K and h, according to Wooding's analytical solution of a three-dimensional flow field. The transient experimental infiltration data, along with initial and final water contents were used for numerical analysis within sand profiles without and with microbiotic crust. Specifically, we provided evidences that the main physical and hydrological consequences occurring locally, always cause lower unsaturated fluxes in the sand beneath the crusted layer. Nevertheless, due to the effective rainfalls regime, it has insignificant effects on the local soil water regimes with unchanged storage and deep fluxes. (C) 2011 Elsevier B.V. All rights reserved.
收录类别SCI
WOS关键词UNSATURATED HYDRAULIC CONDUCTIVITY ; TENGGER DESERT ; MICROSTRUCTURE ; INFILTROMETERS ; MORPHOLOGY ; IMAGES ; WATER
WOS研究方向Agriculture
WOS类目Soil Science
语种英语
WOS记录号WOS:000298895100005
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2556475
专题寒区旱区环境与工程研究所
通讯作者Coppola, A.
作者单位1.Univ Basilicata, Dept Agr & Forestry Syst Management DITEC, I-85100 Potenza, Italy
2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
3.Inst Mediterranean Agro Forestry Syst, CNR ISAFOM, I-80056 Ercolano Naples, Italy
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GB/T 7714
Coppola, A.,Basile, A.,Wang, X.,et al. Hydrological behaviour of microbiotic crusts on sand dunes: Example from NW China comparing infiltration in crusted and crust-removed soil[J]. SOIL & TILLAGE RESEARCH,2011,117:34-43.
APA Coppola, A..,Basile, A..,Wang, X..,Comegna, V..,Tedeschi, A..,...&Comegna, A..(2011).Hydrological behaviour of microbiotic crusts on sand dunes: Example from NW China comparing infiltration in crusted and crust-removed soil.SOIL & TILLAGE RESEARCH,117,34-43.
MLA Coppola, A.,et al."Hydrological behaviour of microbiotic crusts on sand dunes: Example from NW China comparing infiltration in crusted and crust-removed soil".SOIL & TILLAGE RESEARCH 117(2011):34-43.

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