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应用生态学报 ›› 2025, Vol. 36 ›› Issue (12): 3749-3760.doi: 10.13287/j.1001-9332.202512.006

• 研究论文 • 上一篇    下一篇

荒漠草原黑沙蒿灌丛穿透雨空间分布特征及其对浅层土壤水分的影响

陈晓莹1,2, 陈林2,3*, 李敏岚4, 曲文杰5, 宋乃平2,3, 杨新国2,3, 陈应龙6   

  1. 1临沂职业学院乡村振兴学院, 山东临沂 276000;
    2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, 银川 750021;
    3宁夏大学生态环境学院, 银川 750021;
    4甘肃林业职业技术大学测绘工程学院, 甘肃天水 741020;
    5宁夏大学农林与生态学部, 银川 750021;
    6西澳大学农业与环境学院, 澳大利亚珀斯 6009
  • 收稿日期:2025-08-11 修回日期:2025-10-23 出版日期:2025-12-18 发布日期:2026-07-18
  • 通讯作者: *E-mail: chenlin198388@163.com
  • 作者简介:陈晓莹, 女, 1995年生, 博士。主要从事生态水文过程研究。E-mail: chenxiaoyingls@163.com
  • 基金资助:
    国家自然科学基金项目(32360423)、宁夏自然科学基金一般项目(2025AAC030143)、宁夏回族自治区重点研发计划项目(2025BEG01007)和宁夏自然科学基金创新群体项目(2024AAC01004)

Spatial distribution characteristics of throughfall in Artemisia ordosica shrublands and its impact on shallow soil moisture in desert steppe

CHEN Xiaoying1,2, CHEN Lin2,3*, LI Minlan4, QU Wenjie5, SONG Naiping2,3, YANG Xinguo2,3, CHEN Yinglong6   

  1. 1College of Resource and Environment College of Rural Revitalization, Linyi Vocational College, Linyi 276000, Shandong, China;
    2Key Laboratory for Restoration and Reconstruction of Degraded Ecosystem in Northwestern China of Ministry of Education, Ningxia University, Yinchuan 750021, China;
    3School of Ecology and Environment, Ningxia University, Yinchuan 750021, China;
    4College of Geomatics Engineering, Gansu Forestry Voctech University, Tianshui 741020, Gansu, China;
    5Faculty of Agriculture, Forestry and Ecology, Ningxia University, Yinchuan 750021, China;
    6College of Agriculture and Environment, University of Western Australia, Perth 6009, Australia
  • Received:2025-08-11 Revised:2025-10-23 Online:2025-12-18 Published:2026-07-18

摘要: 本研究以荒漠草原典型人工固沙灌木黑沙蒿为研究对象,基于2021和2022年生长季穿透雨、植被特征、气象因子以及冠层内外0~60 cm浅层土壤水分的野外定位观测,探究黑沙蒿灌丛穿透雨的空间分布特征,并使用增强回归树(BRT)模型量化了各主要影响因素的相对贡献率,分析了黑沙蒿灌丛冠层投影区内外浅层土壤水分的补给特征。结果表明: 研究期间共观测到有效降雨事件31次,总降雨量为333.15 mm。在次降雨事件中,黑沙蒿灌丛的平均穿透雨量为8.03 mm,平均穿透雨率为69.9%,穿透雨产生的次降雨阈值为0.69 mm。穿透雨空间格局表现为“雨极”分布在灌丛外缘、“旱极”分布在灌丛中部的特点。BRT模型显示,黑沙蒿灌丛的穿透雨形成过程中非生物因素占主导地位,其中降雨量(相对贡献为89.8%)是最重要的变量,其次是相对湿度和风速,而生物因素的影响占比相对较小(相对贡献<3%)。黑沙蒿灌丛冠层下0~60 cm平均土壤水分补给量(2.88 mm)和平均土壤水分补给速率(3.6%·h-1)均高于冠层外(2.69 mm和3.3%·h-1),增幅分别为6.6%和9.1%,但差异不显著,表明降雨对黑沙蒿冠层下的浅层土壤水分的补给效果更好。降雨量和穿透雨量是影响黑沙蒿冠层下浅层土壤水分补给量的两个关键因素。

关键词: 荒漠草原, 黑沙蒿灌丛, 穿透雨, 土壤水分补给

Abstract: We investigated the spatial distribution of throughfall in Artemisia ordosica, a typical sand-binding shrub species commonly planted in desert steppe. Based on field observations during the growing seasons of 2021 and 2022, we examined throughfall, vegetation characteristics, meteorological variables, and shallow soil moisture (0-60 cm soil layer) within and outside the shrub canopy, aiming to elucidate the spatial heterogeneity of throughfall in shrublands and assess its influence on soil moisture replenishment. We further quantified the relative contributions of key biotic and abiotic factors influencing throughfall by using boosted regression tree (BRT) model. The results showed that 31 effective rainfall events occurred over the study period, with a cumulative precipitation of 333.15 mm. The mean throughfall amount per event was 8.03 mm, corresponding to an average throughfall rate of 69.9%. The minimum rainfall threshold required to generate measurable throughfall was 0.69 mm. Spatially, throughfall exhibited a heterogeneous pattern characterized by a “rain peak” at the shrub periphery and a “drought center” near the shrub core. The BRT analysis revealed that abiotic factors played a dominant role in regulating throughfall, with rainfall amount contributing the most (89.8%), followed by relative humidity and wind speed. In contrast, the contribution of biotic factors was minor (<3%). The average shallow soil moisture recharge under the shrub canopy (2.88 mm, with a recharge rate of 3.6%·h-1) was slightly higher than that in the area outside the canopy (2.69 mm and 3.3%·h-1), with respective increases of 6.6% and 9.1%. However, these differences were not statistically significant. The findings suggested that rainfall under the canopy of A. ordosica provided relatively more effective moisture replenishment to shallow soil layers. Rainfall amount and throughfall amount were the two most critical factors influencing shallow soil moisture recharge.

Key words: desert steppe, Artemisia ordosica shrubland, throughfall, soil moisture replenishment