title: [Crust development and subsurface soil properties under dominant shrubs in the process of dune restoration, Horqin Sand Land].
abstract: Soil crust is a common and widespread phenomenon in desert areas all over the world due to its extraordinary ability to survive desiccation and extreme temperatures, high pH and salinity. Despite its unassuming appearance, biological soil crusts play a significant role in desert ecosystems, including involvement in the process of formation, stability and fertility of soil, preventing soil erosion by water or wind, increasing the possibility of vascular plant colonization, and being responsible for the stabilization of sand dunes. This study taking Horqin Sand Land as research region, by field sampling, crust and topsoil (0-2.5 cm and 2.5-5 cm under crust) samples in different dune habitats and shrub communities were collected, and their physicochemical properties were analyzed, including particle size distribution, bulk density, total nutrients and available nutrients, pH, EC and CaCO3 content. The result revealed that Artemisia halodendron in semi-mobile dune, Caragana microphylla in semi-fix dune, Artemisia frigida in fix dune and Salix microstachya in interdunal lowland were respectively developed physical soil crust, algae crust, lichen crust and moss crust. Crust thickness, hardness, water content, fine fraction, total and available nutrients gradually increased by semi-mobile dune < semi-fix dune < fix dune < interdunal lowland in terms of different dune habitats, and by physical soil crust < algae crust < lichen crust < moss crust in terms of different crust types. There were significant differences among crust types on nutrient content and particle size distribution (p < 0.01). Meanwhile, crust enhanced the < 0.05 mm content and nutrient content of topsoil, following an increasing trend from semi-mobile dune to interdunal lowland. As to each crust, the parameters of 0-2.5 cm subsurface soil layer were higher than that in 2.5-5 cm soil layer. The result also showed that the fine fraction and nutrient content of moss crust under Salix microstachya in interdunal lowland were higher than others, so did the 0-5 cm subsurface soil under it.
authors.affiliation: Naiman Desertification Research Station, Cold and Arid Regions of Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China. guoyirui_gyr@163.com
authors.forename: Yi-rui
authors.initials: YR
authors.lastname: Guo
authors.forename: Ha-lin
authors.initials: HL
authors.lastname: Zhao
authors.forename: Xiao-an
authors.initials: XA
authors.lastname: Zuo
authors.forename: Yu-Lin
authors.initials: YL
authors.lastname: Li
authors.forename: Yin-xin
authors.initials: YX
authors.lastname: Huang
authors.forename: Shao-kun
authors.initials: SK
authors.lastname: Wang
mesh_terms: D019306:Artemisia / Q000254:growth & development; D032602:Caragana / Q000254:growth & development; D002681:China; D003247:Conservation of Natural Resources; D003889:Desert Climate; D017753:Ecosystem; D004784:Environmental Monitoring / Q000379:methods*; D032108:Salix / Q000254:growth & development; D012822:Silicon Dioxide / Q000032:analysis*; D012987:Soil / Q000032:analysis*; D014867:Water / Q000032:analysis
chemical_list: D012987:Soil; D014867:Water; D012822:Silicon Dioxide