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DOI10.1016/j.ecolind.2021.108362
Alpine shrub had a stronger soil water retention capacity than the alpine meadow on the northeastern Qinghai-Tibetan Plateau
Dai, Licong; Fu, Ruiyu; Guo, Xiaowei; Du, Yangong; Hu, Zhongmin; Cao, Guangmin
通讯作者Dai, LC ; Guo, XW (通讯作者),Chinese Acad Sci, Qinghai Prov Key Lab Restorat Ecol Cold Reg, Northwest Inst Plateau Biol, Xining 810001, Peoples R China.
发表日期2021
ISSN1470-160X
EISSN1872-7034
卷号133
英文摘要Soil water retention capacity is an essential component of the land surface processes and hydrological cycles. Although the effect of grassland degradation on soil water retention capacity have been well documented, few studies have focused on how soil hydrological properties vary between different vegetation types on the QinghaiTibet Plateau (QTP). This study selected three vegetation types: Potentilla fruticosa shrub (PFS), Kobresia pygmaca meadow (KPM), and Kobresia humilis meadow (KHM), and aimed to explore the variations and factors controlling soil water retention capacity across the three types. Results showed that the soil water retention capacity was higher in PFS than in KPM and KHM across 0-40 cm, whereas the 0-30 cm plant available water content was much lower in PFS than in KPM and KHM. Meanwhile, the soil properties within the different soil layers varied significantly between vegetation types. The 0-10 cm clay and silt contents were significantly higher in PFS than in the other two vegetation types, whereas the soil bulk density (BD) was lower in PFS than in KHM and KPM. Furthermore, the 0-50 cm soil capillary porosity (CP) was significantly higher in PFS than in KPM and KHM, except at 0-10 cm. Besides, the 0-10 cm soil organic matter (SOM) was significantly higher in KPM than in PFS and KHM, owing to its highest root biomass. Overall, the soil water retention capacity was most strongly influenced by CP, followed by BD, TP, SOM and root biomass, whereas the soil non-capillary porosity and soil particle size distribution exerted no significant impact on soil water retention capacity. Our results suggested that the alpine shrub had a stronger soil water retention capacity than the alpine meadow.
关键词PARTICLE-SIZE DISTRIBUTIONSPATIAL VARIABILITYLOESS PLATEAUORGANIC-MATTERDEGRADATIONVEGETATIONGRASSLANDMOISTUREINFILTRATIONPATTERNS
英文关键词Qinghai-Tibet Plateau; Soil water retention; Plant available water content; Vegetation types; Soil properties
语种英语
WOS研究方向Biodiversity & Conservation ; Environmental Sciences & Ecology
WOS类目Biodiversity Conservation ; Environmental Sciences
WOS记录号WOS:000719748000004
来源期刊ECOLOGICAL INDICATORS
来源机构中国科学院西北生态环境资源研究院
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/254289
作者单位[Dai, Licong; Hu, Zhongmin] Hainan Univ, Coll Ecol & Environm, Haikou 570228, Hainan, Peoples R China; [Dai, Licong; Guo, Xiaowei; Du, Yangong; Cao, Guangmin] Chinese Acad Sci, Qinghai Prov Key Lab Restorat Ecol Cold Reg, Northwest Inst Plateau Biol, Xining 810001, Peoples R China; [Dai, Licong; Guo, Xiaowei; Du, Yangong; Cao, Guangmin] Chinese Acad Sci, Key Lab Adaptat & Evolut Plateau Biota, Northwest Inst Plateau Biol, Xining 810001, Qinghai, Peoples R China; [Fu, Ruiyu] Hainan Acad Mangrove, Hainan Acad Forestry, Haikou 571100, Hainan, Peoples R China
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GB/T 7714
Dai, Licong,Fu, Ruiyu,Guo, Xiaowei,et al. Alpine shrub had a stronger soil water retention capacity than the alpine meadow on the northeastern Qinghai-Tibetan Plateau[J]. 中国科学院西北生态环境资源研究院,2021,133.
APA Dai, Licong,Fu, Ruiyu,Guo, Xiaowei,Du, Yangong,Hu, Zhongmin,&Cao, Guangmin.(2021).Alpine shrub had a stronger soil water retention capacity than the alpine meadow on the northeastern Qinghai-Tibetan Plateau.ECOLOGICAL INDICATORS,133.
MLA Dai, Licong,et al."Alpine shrub had a stronger soil water retention capacity than the alpine meadow on the northeastern Qinghai-Tibetan Plateau".ECOLOGICAL INDICATORS 133(2021).
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