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荒漠草原灌丛转变过程土壤水分亏缺空间特征及影响因素

赵亚楠 王红梅 李志丽 张振杰 陈彦硕 苏荣霞

草业学报2024,Vol.33Issue(4):22-34,13.
草业学报2024,Vol.33Issue(4):22-34,13.DOI:10.11686/cyxb2023209

荒漠草原灌丛转变过程土壤水分亏缺空间特征及影响因素

Responses of spatial pattern and driving factors for soil water deficit of desert grassland-shrubland transition sites

赵亚楠 1王红梅 2李志丽 3张振杰 3陈彦硕 3苏荣霞3

作者信息

  • 1. 宁夏大学林业与草业学院,宁夏 银川 750021||中国科学院地理科学与资源研究所,北京 100101
  • 2. 宁夏大学林业与草业学院,宁夏 银川 750021||宁夏大学西北退化生态系统恢复与重建教育部重点实验室,宁夏 银川 750021
  • 3. 宁夏大学林业与草业学院,宁夏 银川 750021
  • 折叠

摘要

Abstract

Shrub encroachment has an important impact on ecosystem structure,function and services,and its adverse impact on soil water has been recognized,but there is still a lack of quantitative assessment and research into its driving mechanisms at a regional scale.In the Ningxia desert steppe,43 paired sample sites of desert grassland and of shrubland were selected,and a'plot compared soil water deficit index'(PCSWDI)was introduced to evaluate the spatial pattern of soil water deficit and its drivers after the transition from desert steppe to shrubland.Results showed that the soil water content of 0-100 cm and 100-200 cm strata decreased significantly by 27.80%and 57.92%,respectively,after the transition from desert grassland to shrubland.Also,the PCSWDI of shrubland from 0-100 cm was significantly lower than that of desert grassland,indicating that there is no soil water deficit in the 0-100 cm layer of shrubland.Geostatistical analysis showed that the structural variance ratios of the PCSWDI of desert grassland and shrubland were 94.73%and 95.29%,respectively,which indicate strong spatial autocorrelation and were mainly controlled by structural factors.Furthermore,the geographic detector method found that soil water storage,aspect and field capacity were the dominant factors affecting the PCSWDI of the shrubland;The interactive detection showed that the spatial differentiation of the PCSWDI of the 0-100 cm soil layer of shrubland was the result of the interaction of multiple factors.In conclusion,our results show that although there was no soil water deficit in the 0-100 cm soil layer of shrubland,a significant decrease in the 100-200 cm soil water content indicating the depletion of deep soil water was observed.Therefore,vegetation restoration in arid and semi-arid regions must take into account the carrying capacity and water threshold of vegetation,and a nature-based solution may be the main focus of vegetation restoration in the future.

关键词

荒漠草原/人为灌丛化/土壤水分/地理探测器/样地土壤水分相对亏缺指数

Key words

desert steppe/anthropogenic shrub encroachment/soil water/geographic detector method/plot compared soil water deficit index

引用本文复制引用

赵亚楠,王红梅,李志丽,张振杰,陈彦硕,苏荣霞..荒漠草原灌丛转变过程土壤水分亏缺空间特征及影响因素[J].草业学报,2024,33(4):22-34,13.

基金项目

国家自然科学基金(31860677,32260348)和宁夏高等学校一流学科建设项目(NXYLXK2017A01)资助. (31860677,32260348)

草业学报

OA北大核心CSTPCD

1004-5759

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