中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Temporal stability of soil water storage in multiple soil layers in high-elevation forests

文献类型:期刊论文

作者He, Zhi-Bin1; Zhao, Min-Min1,2; Zhu, Xi1; Du, Jun1; Chen, Long-Fei1; Lin, Peng-Fei1; Li, Jing1,2
刊名JOURNAL OF HYDROLOGY
出版日期2019-02-01
卷号569页码:532-545
关键词Soil water storage Temporal stability Representative location Plot hydrology Picea crassifolia Qilian Mountains
ISSN号0022-1694
DOI10.1016/j.jhydrol.2018.12.024
通讯作者He, Zhi-Bin(hzbmail@lzb.ac.cn)
英文摘要Understanding soil water storage (SWS) dynamics in soil profiles is important for hydrological modeling and restoration of vegetation in semi-arid areas. Using the temporal stability method, we aimed to investigate the temporal stability of SWS at 0-40, 40-80, and 80-120 cm depth, and to identify representative sites for reliable estimates of the mean SWS in the permanent forest plot in the Qilian Mountains of China. Further, we wanted to identify correlations between temporal stability of SWS and soil, topography, and properties of the vegetation. Soil water content at soil depths 0-120 (for locations 1-40) and 0-70 cm (for locations 41-60) were measured using time-domain reflectometry (TDR) on 52 dates from 2016 to 2017. Results revealed that time-averaged mean SWS for the three layers differed significantly (P < 0.05), and the temporal changes and spatial variations of the mean SWS all decreased with increasing soil depth. Based on either the Spearman correlation coefficient or the standard deviation of relative difference (SDRD) index, the temporal stability of SWSs within the soil profiles under different soil layers were strong, and the number of time-stable locations increased with increasing soil depth, indicating that the SWS intended to be more temporally stable in deeper soil. One time-stable site can be representative of the mean SWS for multiple soil layers for the whole plot, and can accurately estimate the mean SWS for the three soil layers (R-2 > 0.86, P < 0.001). Moreover, these time-stable locations should be those having average LAI, SBD or relatively low canopy interception loss compared to the corresponding field means. Soil bulk density, canopy interception rate, and aboveground biomass of mosses can significantly (P < 0.05) affect the stability of SWSs in this high-elevation forests. Such effects, however, differed among the different soil layers due to different conditions of soil characteristics, distribution of root biomass, and freeze-thawing processes. These results suggest that the influence of vegetation properties of the temporal stability of SWS should attract more attention and that both the relative importance of and interactions among different determining factors is helpful for better understanding the mechanistic determinants of SWS temporal stability in these areas.
收录类别SCI
WOS关键词TIME-STABILITY ; LOESS PLATEAU ; SPATIAL-PATTERNS ; HILLSLOPE SCALE ; NEUTRON PROBE ; DESERT AREA ; MOISTURE ; SURFACE ; VARIABILITY ; CANOPY
WOS研究方向Engineering ; Geology ; Water Resources
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
语种英语
WOS记录号WOS:000457952900040
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2558179
专题寒区旱区环境与工程研究所
通讯作者He, Zhi-Bin
作者单位1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Ecohydrol Inland River Basin, Linze Inland River Basin Res Stn,Chinese Ecosyst, Lanzhou 730000, Gansu, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
He, Zhi-Bin,Zhao, Min-Min,Zhu, Xi,et al. Temporal stability of soil water storage in multiple soil layers in high-elevation forests[J]. JOURNAL OF HYDROLOGY,2019,569:532-545.
APA He, Zhi-Bin.,Zhao, Min-Min.,Zhu, Xi.,Du, Jun.,Chen, Long-Fei.,...&Li, Jing.(2019).Temporal stability of soil water storage in multiple soil layers in high-elevation forests.JOURNAL OF HYDROLOGY,569,532-545.
MLA He, Zhi-Bin,et al."Temporal stability of soil water storage in multiple soil layers in high-elevation forests".JOURNAL OF HYDROLOGY 569(2019):532-545.

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来源:寒区旱区环境与工程研究所

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