砒砂岩区不同林分土壤水分动态变化及其对降雨的响应
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S157.1

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内蒙古自治区科技计划项目(内蒙古自治区风沙物理与防沙治沙工程重点实验室)“砒砂岩沟坡侵蚀过程与防治机制研究”(2025KYPT0043); 内蒙古自治区科技计划项目“砒砂岩沟坡崩塌机制与沟-坡-岸综合防治关键技术研究”(2025YFSH0001); 内蒙古黄河流域多沙粗沙区林草植被恢复技术体系研究采购项目(ZB2023021185)


Soil moisture dynamics in different forest species and their responses to rainfall in Pisha sandstone area
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    [目的] 研究砒砂岩区雨季降雨特征、不同林分土壤水分动态及其对降雨的响应,阐明不同降雨等级下土壤水分变化规律,为砒砂岩区造林树种选择提供科学依据。[方法] 基于2024年7—9月定点监测,分析砒砂岩区3种人工林 (柠条纯林、油松纯林、柠条×油松混交林)0—100 cm土层水分时空变化及其对降雨的响应。[结果] ①柠条×油松混交林的土壤含水率最高(26.15%),油松纯林次之(24.15%),柠条纯林最低(16.43%),3种林分土壤含水率随着土层深度的增加呈现出先增加后减少再增加的波动趋势。②随着降雨等级从小到大,土壤水分补充深度分别为10,60 cm,在降雨等级为大雨与暴雨时,0—100 cm深度的土壤水分均得到补充。在不同降雨等级下,柠条纯林土壤水分增量最高,油松次之,柠条×油松混交林的土壤水分增量最低。③在降雨等级为暴雨时,3种林分在0—50 cm土层中,均在雨后对降雨作出响应,且在第2天土壤含水率缓慢下降,50—100 cm土层出现水分运移的滞后性。[结论] 混交林整体保水能力优于纯林,但对降雨的水分增量响应较弱,柠条纯林虽含水率低,但对降雨的水分吸收能力较强,深层土壤对降雨的响应存在明显滞后性。在砒砂岩地区进行生态恢复过程中,可以优先选取柠条×油松混交林,来减少水分流失。

    Abstract:

    [Objective] The rainfall characteristics in the Pisha sandstone area during the rainy season, soil moisture dynamics in different forest stands, and their responses to rainfall were analyzed, and the soil moisture variation patterns under different rainfall levels clarified, in order to provide a scientific basis for the selection of afforestation tree species in the Pisha sandstone area. [Methods] Based on fixed-point monitoring from July to September 2024, temporal and spatial soil moisture variations in soil depth from 0 to 100 cm in three plantations (pure Caragana korshinskii, pure Pinus tabuliformis, and mixed C. korshinskii × P. tabuliformis forests) in the Pisha sandstone area during the rainy season were analyzed. [Results] ① The soil moisture content of the mixed C. korshinskii × P. tabuliformis forest was the highest (26.15%), followed by that of the pure P. tabuliformis forest (24.15%), and the lowest in the pure C. korshinskii forest (16.43%). The soil moisture content of the three forest stand types showed a fluctuating trend, first increasing, then decreasing, and then increasing again with increasing soil depth. ② With rainfall amounts from low to high, the soil moisture replenishment depths were 10 and 60 cm, respectively, and the soil moisture at a depth of 0—100 cm was replenished during heavy rainfall and rainstorm events. Under different rainfall amounts, the soil moisture increment of the pure C. korshinskii forest was the highest, followed by P. tabuliformis; the soil moisture increment of C. korshinskii × P. tabuliformis mixed forest was the lowest. ③ When rainstorm events occurred, all three stands showed responses in the 0—50 cm soil layer, the soil moisture content decreased slowly on the second day, and a water transportation lag appeared in the 50—100 cm soil layer. [Conclusion] The overall water holding capacity of mixed forests was better than those of the pure forests, however, the response to increased rainfall was weak. Although the water content of the pure C. korshinskii forest was low, the rainfall absorption capacity was stronger, and the deep soil rainfall response obviously lagged behind. For ecological restoration of the Pisha sandstone area, mixed C. korshinskii × P. tabuliformis forests should be preferentially selected to reduce water loss.

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王逸凡,李龙,弥宏卓,王志强,张尚轩,张宇,任亚楠,周星辰.砒砂岩区不同林分土壤水分动态变化及其对降雨的响应[J].水土保持通报,2025,45(5):187-198,217

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  • 收稿日期:2025-04-23
  • 最后修改日期:2025-06-12
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  • 在线发布日期: 2025-11-07
  • 出版日期: 2025-10-18