{"title":"黄土高原土地利用变化引发的坡面产流机制变迁","authors":"Jiahui Zhou , Yongfu Wen , Peng Gao , Siyu Ren , Xiaoxue Guo , Xingmin Mu","doi":"10.1016/j.catena.2025.109517","DOIUrl":null,"url":null,"abstract":"<div><div>Large-scale land use change has been shown to have a significant impact on the underlying surface conditions, with consequences for soil erosion, river runoff, and sediment transport. The impact of land use change on soil infiltration capacity and whether the runoff generation mechanisms in typical watersheds of the Loess Plateau might change under strongly varying surface conditions remain unclear. This study selected three land use types in the Loess Plateau: forestlands, grasslands, and wastelands. Using a double-ring infiltrometer and artificial rainfall simulation, infiltration tests and rainfall-runoff experiments were conducted under different land use types to investigate the effects on soil properties, infiltration capacity, and slope runoff mechanisms. The results indicated that land use change significantly reduced the bulk density of shallow soils. Forestlands and grasslands exhibited significantly higher mean weight diameter and saturated hydraulic conductivity. Land use change effectively improved the infiltration characteristics. The infiltration characteristics of the soil vary across different soil layers. In the 0–30 cm soil layer, <em>K</em>s (saturated hydraulic conductivity) made a significant contribution to soil infiltration performance. In the simulated rainfall experiments, subsurface flow was observed in both forestlands and grasslands. Due to land use change, the soil infiltration capacity was significantly enhanced, which in turn affected the transformation of runoff generation mechanisms. This suggests that changes in soil infiltration due to land use change lead to a shift in slope runoff generation mechanisms, potentially transitioning from a single surface infiltration excess overland flow mechanism to a combination of infiltration excess overland flow and subsurface flow mechanisms. These findings enhance the understanding of hydrological processes such as infiltration and runoff after land use change.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"261 ","pages":"Article 109517"},"PeriodicalIF":5.7000,"publicationDate":"2025-10-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Transitions in slope runoff generation mechanisms induced by land use change in the Loess Plateau, China\",\"authors\":\"Jiahui Zhou , Yongfu Wen , Peng Gao , Siyu Ren , Xiaoxue Guo , Xingmin Mu\",\"doi\":\"10.1016/j.catena.2025.109517\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Large-scale land use change has been shown to have a significant impact on the underlying surface conditions, with consequences for soil erosion, river runoff, and sediment transport. The impact of land use change on soil infiltration capacity and whether the runoff generation mechanisms in typical watersheds of the Loess Plateau might change under strongly varying surface conditions remain unclear. This study selected three land use types in the Loess Plateau: forestlands, grasslands, and wastelands. Using a double-ring infiltrometer and artificial rainfall simulation, infiltration tests and rainfall-runoff experiments were conducted under different land use types to investigate the effects on soil properties, infiltration capacity, and slope runoff mechanisms. The results indicated that land use change significantly reduced the bulk density of shallow soils. Forestlands and grasslands exhibited significantly higher mean weight diameter and saturated hydraulic conductivity. Land use change effectively improved the infiltration characteristics. The infiltration characteristics of the soil vary across different soil layers. In the 0–30 cm soil layer, <em>K</em>s (saturated hydraulic conductivity) made a significant contribution to soil infiltration performance. In the simulated rainfall experiments, subsurface flow was observed in both forestlands and grasslands. Due to land use change, the soil infiltration capacity was significantly enhanced, which in turn affected the transformation of runoff generation mechanisms. This suggests that changes in soil infiltration due to land use change lead to a shift in slope runoff generation mechanisms, potentially transitioning from a single surface infiltration excess overland flow mechanism to a combination of infiltration excess overland flow and subsurface flow mechanisms. These findings enhance the understanding of hydrological processes such as infiltration and runoff after land use change.</div></div>\",\"PeriodicalId\":9801,\"journal\":{\"name\":\"Catena\",\"volume\":\"261 \",\"pages\":\"Article 109517\"},\"PeriodicalIF\":5.7000,\"publicationDate\":\"2025-10-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Catena\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0341816225008197\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225008197","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Transitions in slope runoff generation mechanisms induced by land use change in the Loess Plateau, China
Large-scale land use change has been shown to have a significant impact on the underlying surface conditions, with consequences for soil erosion, river runoff, and sediment transport. The impact of land use change on soil infiltration capacity and whether the runoff generation mechanisms in typical watersheds of the Loess Plateau might change under strongly varying surface conditions remain unclear. This study selected three land use types in the Loess Plateau: forestlands, grasslands, and wastelands. Using a double-ring infiltrometer and artificial rainfall simulation, infiltration tests and rainfall-runoff experiments were conducted under different land use types to investigate the effects on soil properties, infiltration capacity, and slope runoff mechanisms. The results indicated that land use change significantly reduced the bulk density of shallow soils. Forestlands and grasslands exhibited significantly higher mean weight diameter and saturated hydraulic conductivity. Land use change effectively improved the infiltration characteristics. The infiltration characteristics of the soil vary across different soil layers. In the 0–30 cm soil layer, Ks (saturated hydraulic conductivity) made a significant contribution to soil infiltration performance. In the simulated rainfall experiments, subsurface flow was observed in both forestlands and grasslands. Due to land use change, the soil infiltration capacity was significantly enhanced, which in turn affected the transformation of runoff generation mechanisms. This suggests that changes in soil infiltration due to land use change lead to a shift in slope runoff generation mechanisms, potentially transitioning from a single surface infiltration excess overland flow mechanism to a combination of infiltration excess overland flow and subsurface flow mechanisms. These findings enhance the understanding of hydrological processes such as infiltration and runoff after land use change.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.