Arid
DOI10.1007/s11104-014-2263-x
Effects of freeze-thaw cycles on the soil nutrient balances, infiltration, and stability of cyanobacterial soil crusts in northern China
Wang, Weibo1,2; Shu, Xiao1; Zhang, Quanfa1; Guenon, Rene2
通讯作者Zhang, Quanfa
来源期刊PLANT AND SOIL
ISSN0032-079X
EISSN1573-5036
出版年2015
卷号386期号:1-2页码:263-272
英文摘要

Freeze-thaw fluctuation is a natural phenomenon, which is frequently encountered by biological soil crusts (BSCs) in late autumn and early spring in cold deserts. The objective of our study was to investigate the effects of freeze-thaw cycles (FTCs) on the soil nutrient balances, infiltration, and stability of cyanobacterial soil crusts (CSCs) in the temperate desert region.


A controlled incubation experiment was carried out to study the effects of diurnal freeze-thaw cycles (FTCs) on total soil carbon (TC), total soil nitrogen (TN), soil TC/TN, hydraulic conductivity, and strength of light and dark cyanobacterial crusts, respectively. Six successive diurnal FTCs were applied as three temperature regimes (i.e., six successive mild FTCs (mild), six successive severe FTCs (severe), three successive mild FTCs followed by three successive severe FTCs (medium)). The experiment intended to simulate natural temperature changes in one of the temperate regions of northern China.


Compared with dark CSCs cores, light CSCs cores lost a greater proportion of nitrogen. For both crust cores, severe FTCs decreased TC and TN more than mild FTCs. However, TC and TN remained relative constant when CSCs cores were treated with severe FTCs after experiencing mild FTCs. TC and TN of both CSCs cores decreased in the earlier FTCs and then remained stable in the later FTCs. TC/TN increased significantly for light CSCs, but only changed slightly for dark CSCs after successive FTCs. The effects of FTCs on the hydraulic conductivity and strength of CSCs were not consistent with our expectations that FTCs would increase hydrological conductivity and decrease strength. These effects depended on crust type, FTC number, and freeze/thaw intensity. Increase in hydraulic conductivity and decrease in strength only occurred in severe treatment in the dark CSCs during the later FTCs.


Light CSCs are more sensitive to FTCs than dark CSCs. Mild FTCs decrease less TC and TN than severe FTCs and mostly increase the stability of the CSCs. However, severe FTCs may decrease TC and TN drastically, thereby, degrading the BSCs.


英文关键词Freeze-thaw cycles Desert ecosystems C and N balances Infiltration Stabilization
类型Article
语种英语
国家Peoples R China ; USA
收录类别SCI-E
WOS记录号WOS:000346491000019
WOS关键词CLIMATE-CHANGE ; CARBON ; SNOW ; MANIPULATION ; TEMPERATURE ; ADAPTATION ; RESPONSES ; DYNAMICS ; IMPACTS ; ROLES
WOS类目Agronomy ; Plant Sciences ; Soil Science
WOS研究方向Agriculture ; Plant Sciences
来源机构Arizona State University
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/189627
作者单位1.Chinese Acad Sci, Wuhan Bot Garden, Lab Aquat Bot & Watershed Ecol, Wuhan 430074, Peoples R China;
2.Arizona State Univ, Sch Life Sci, Tempe, AZ 85287 USA
推荐引用方式
GB/T 7714
Wang, Weibo,Shu, Xiao,Zhang, Quanfa,et al. Effects of freeze-thaw cycles on the soil nutrient balances, infiltration, and stability of cyanobacterial soil crusts in northern China[J]. Arizona State University,2015,386(1-2):263-272.
APA Wang, Weibo,Shu, Xiao,Zhang, Quanfa,&Guenon, Rene.(2015).Effects of freeze-thaw cycles on the soil nutrient balances, infiltration, and stability of cyanobacterial soil crusts in northern China.PLANT AND SOIL,386(1-2),263-272.
MLA Wang, Weibo,et al."Effects of freeze-thaw cycles on the soil nutrient balances, infiltration, and stability of cyanobacterial soil crusts in northern China".PLANT AND SOIL 386.1-2(2015):263-272.
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