Arid
DOI10.1515/johh-2016-0006
Linking surface and subsurface properties of biocrusted and non-biocrusted habitats of fine-grained fluvial sediments (playas) from the Negev Desert
Kidron, Giora J.
通讯作者Kidron, Giora J.
来源期刊JOURNAL OF HYDROLOGY AND HYDROMECHANICS
ISSN0042-790X
EISSN1338-4333
出版年2016
卷号64期号:2页码:141-149
英文摘要

With biocrusts playing a cardinal role in C and N fixation in arid zones, information regarding the factors that determine their limits of growth is of uttermost importance for the study of ecosystem structure and function. This is also the case in the western Negev dunefields, where although abundant on the sandy surfaces, biocrusts are scarce on fine-grained (mainly loessial) sediments, termed playas. In the Nizzana research site (NRS), visibly distinct surfaces, with and without biocrusts were noted within a single playa. In an attempt to characterize these distinct surfaces, a set of random measurements were carried out, which included measurements of crack density, microrelief and chlorophyll content of the upper 0-1 cm. Following a cluster analysis, four distinct types of surfaces (hereafter habitats) were defined, one with substantial amount of chlorophyll content which can be regarded as biocrust (P4), and three non-crusted surfaces (P1-P3). Within each type, two 50 cm-deep pits were dug and the pH, electrical conductivity (EC) and fine (silt and clay) content (FC) of samples collected at 1-5, 5-10, 10-20, 20-30, 30-40 and 40-50 cm-depth were analyzed. In addition, periodical moisture measurements were carried out (in pairs) to a depth of 0-20 cm at each surface type during 2013/14. All non-crusted habitats (P1-P3) were characterized by loessial subsurface sediments. Conversely, P4 was either characterized by loessial subsurface sediments (and in this case it was characterized by a slightly concave surface) or having a sandy subsurface (at similar to 5-10 cm depth). While the non-crusted surfaces exhibited low moisture content, P4 exhibited deeper and higher moisture content explained either by the more sandy sediments or by lower water loss through runoff. The findings point to the close link between surface and subsurface properties and indicate that water availability may explain biocrust establishment and growth also at the loessial playa surfaces. Biocrusts may thus serve as bioindicators for habitats with high moisture content.


英文关键词Available water content Loess Soil moisture
类型Article
语种英语
国家Israel
收录类别SCI-E
WOS记录号WOS:000375744800006
WOS关键词BIOLOGICAL SOIL CRUSTS ; MICROBIOTIC CRUSTS ; NORTHWESTERN CHINA ; CHIHUAHUAN DESERT ; MOJAVE DESERT ; DUNE SLOPES ; WATER ; LAKE ; ISRAEL ; LAND
WOS类目Water Resources
WOS研究方向Water Resources
来源机构Hebrew University of Jerusalem
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/194554
作者单位Hebrew Univ Jerusalem, Inst Earth Sci, Givat Ram Campus, IL-91904 Jerusalem, Israel
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Kidron, Giora J.. Linking surface and subsurface properties of biocrusted and non-biocrusted habitats of fine-grained fluvial sediments (playas) from the Negev Desert[J]. Hebrew University of Jerusalem,2016,64(2):141-149.
APA Kidron, Giora J..(2016).Linking surface and subsurface properties of biocrusted and non-biocrusted habitats of fine-grained fluvial sediments (playas) from the Negev Desert.JOURNAL OF HYDROLOGY AND HYDROMECHANICS,64(2),141-149.
MLA Kidron, Giora J.."Linking surface and subsurface properties of biocrusted and non-biocrusted habitats of fine-grained fluvial sediments (playas) from the Negev Desert".JOURNAL OF HYDROLOGY AND HYDROMECHANICS 64.2(2016):141-149.
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