Spatial Variations of Soil Moisture under Caragana korshinskii Kom. from Different Precipitation Zones: Field Based Analysis in the Loess Plateau, China

dc.contributor.authorLiu, Yuanxin
dc.contributor.authorZhao, Wenwu
dc.contributor.authorWang, Lixin
dc.contributor.authorZhang, Xiao
dc.contributor.authorDaryanto, Stefani
dc.contributor.authorFang, Xuening
dc.contributor.departmentDepartment of Earth Sciences, School of Scienceen_US
dc.date.accessioned2016-10-28T12:57:17Z
dc.date.available2016-10-28T12:57:17Z
dc.date.issued2016-02
dc.description.abstractSoil moisture scarcity has become the major limiting factor of vegetation restoration in the Loess Plateau of China. The aim of this study is: (i) to compare the spatial distribution of deep (up to 5 m) soil moisture content (SMC) beneath the introduced shrub Caragana korshinskii Kom. under different precipitation zones in the Loess Plateau and (ii) to investigate the impacts of environmental factors on soil moisture variability. Soil samples were taken under C. korshinskii from three precipitation zones (Semiarid-350, Semiarid-410, Semiarid-470). We found that the highest soil moisture value was in the 0–0.1 m layer with a large coefficient of variation. The soil water storage under different precipitation zones increased following the increase of precipitation (i.e., Semiarid-350 < Semiarid-410 < Semiarid-470), although the degree of SMC variation was different for different precipitation zones. The SMC in the Semiarid-350 zone initially increased with soil depth, and then decreased until it reached the depth of 2.8-m. The SMC in the Semiarid-410 zone showed a decreasing trend from the top soil to 4.2-m depth. The SMC in the Semiarid-470 zone firstly decreased with soil depth, increased, and then decreased until it reached 4.6-m depth. All SMC values then became relatively constant after reaching the 2.8-m, 4.2-m, and 4.6-m depths for Semiarid-350, Semiarid-410, and Semiarid-470, respectively. The low but similar SMC values at the stable layers across the precipitation gradient indicate widespread soil desiccation in this region. Our results suggested that water deficit occurred in all of the three precipitation zones with precipitation, latitude, field capacity, and bulk density as the main environmental variables affecting soil moisture. Considering the correlations between precipitation, SMC and vegetation, appropriate planting density and species selection should be taken into account for introduced vegetation management.en_US
dc.eprint.versionFinal published versionen_US
dc.identifier.citationLiu, Y., Zhao, W., Wang, L., Zhang, X., Daryanto, S., & Fang, X. (2016). Spatial Variations of Soil Moisture under Caragana korshinskii Kom. from Different Precipitation Zones: Field Based Analysis in the Loess Plateau, China. Forests, 7(2), 31.en_US
dc.identifier.urihttps://hdl.handle.net/1805/11273
dc.language.isoenen_US
dc.publisherMDPIen_US
dc.relation.isversionof10.3390/f7020031en_US
dc.relation.journalForestsen_US
dc.rightsAttribution 3.0 United States
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/
dc.sourcePublisheren_US
dc.subjectsoil moistureen_US
dc.subjectprecipitation zonesen_US
dc.subjectspatial distributionen_US
dc.titleSpatial Variations of Soil Moisture under Caragana korshinskii Kom. from Different Precipitation Zones: Field Based Analysis in the Loess Plateau, Chinaen_US
dc.typeArticleen_US
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