Distribution characteristics of soil moisture and temperature under different land use types in the deep profile of loess area in northern Shaanxi, China.

Q3 Environmental Science
Ming-Hui Li, Yang-Yang Li, Jun Fan
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Abstract

Understanding the effects of different land use modes on the spatial and temporal variations of soil moisture and temperature in the deep profile and revealing the regulatory effects of various vegetation covers on regional water and heat resources can provide a theoretical basis for the optimization of land management and vegetation restoration. Taking the advantage of different land use patterns in the Liudaogou watershed in the northern part of Loess Plateau, we monitored soil moisture content as well as temperature in the 0-1000 cm soil layer in 2022 to analyze the temporal variation and vertical profile distribution characteristics of soil moisture and temperature under four land use modes (woodland, grassland, farmland, and wild grassland). The results showed that soil moisture and temperature distributions varied significantly across different land use types. In the growing season (April-October), total soil water storage in the 0-1000 cm soil layer of the four land use types, in a descending order, was as follows: soybean farmland (1393 mm), wild grassland (1374 mm), Caragana korshinkii forest (1218 mm), and alfalfa grassland (557 mm). Soil moisture of C. korshinkii forest and soybean farmland changed obviously in the 0-300 cm soil layer, and that of wild grassland and alfalfa grassland was in 0-500 and 0-200 cm soil layers, respectively, while soil moisture of deep soil layers fluctuated little. The impact of land use modes on soil temperature was primarily manifested in the 0-200 cm soil layer, and the depth was up to 300 cm. The depth of precipitation infiltration replenishment of the four land use modes was approximately 200 cm. The depth of soil moisture depletion was 200 cm in both C. korshinkii forest and alfalfa grassland, and was 100 cm in soybean farmland and wild grassland. Soil hydrothermal processes in the deep profile varied across vegetation types.

中国陕北黄土地区深剖面不同土地利用类型下土壤水分和温度的分布特征
了解不同土地利用模式对深剖面土壤水分和温度时空变化的影响,揭示不同植被对区域水热资源的调控作用,可为优化土地管理和植被恢复提供理论依据。利用黄土高原北部六道沟流域不同土地利用模式的优势,于2022年对0-1000 cm土层的土壤水分含量和温度进行了监测,分析了四种土地利用模式(林地、草地、农田和荒草地)下土壤水分和温度的时间变化和垂直剖面分布特征。结果表明,不同土地利用类型的土壤水分和温度分布差异显著。在生长季节(4 月至 10 月),四种土地利用类型 0-1000 厘米土层的土壤总蓄水量从高到低依次为:大豆农田(1393 毫米)、野生草地(1374 毫米)、Caragana korshinkii 森林(1218 毫米)和苜蓿草地(557 毫米)。大豆林和大豆农田的土壤水分在 0-300 cm 土层变化明显,荒草地和苜蓿草地的土壤水分分别在 0-500 cm 和 0-200 cm 土层变化明显,而深土层土壤水分波动较小。土地利用方式对土壤温度的影响主要表现在 0-200 cm 土层,深度可达 300 cm。四种土地利用模式的降水入渗补充深度约为 200 厘米。科尔辛基桉树林和紫花苜蓿草地的土壤水分消耗深度为 200 厘米,大豆农田和野生草地的土壤水分消耗深度为 100 厘米。不同植被类型深层剖面的土壤水热过程各不相同。
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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
自引率
0.00%
发文量
11393
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