Zhao Jin , Huifeng Wu , Hao Han , Yunchong Fu , Jing Zhang , Guofan Cao , Keyan Xu
{"title":"450年自然滑坡坝谷农田土壤水分动态:降水响应的洞察","authors":"Zhao Jin , Huifeng Wu , Hao Han , Yunchong Fu , Jing Zhang , Guofan Cao , Keyan Xu","doi":"10.1016/j.ecolind.2025.113661","DOIUrl":null,"url":null,"abstract":"<div><div>Tens of thousands of sediment check dams have historically played vital ecological functions in China’s Loess Plateau, and dammed valley farmland has been a significant agricultural resource for centuries. However, newly created valley farmlands under the “Gully Land Consolidation” project often face lower arable quality and frequent soil salinization compared to their natural counterparts. To draw insights from natural dammed valley farmland, we selected the 450-year-old Huangtuwa natural landslide-dammed valley farmland (NLDF) for high-frequency, long-term monitoring and analysis of soil water content and precipitation during 2019–2020 and used the HYDRUS-1D model to assess its water storage capabilities. The results indicate that the soils from 0–100 cm can be clearly categorized into three groups: the rapid response layer (0–40 cm), which reacts quickly to rainfall; the water transport and emergency reservoir layer (∼60 cm), characterized by lower water content that fluctuates rapidly during extreme rainfall, functioning as both a reservoir and drainage pathway; and the stable water supply layer (∼100 cm), with the most stable water content (16.6 %, SD: 1.2 %), crucial for fertility and cultivation. Based on HYDRUS-1D model calculations, the soil water storage of NLDF remained stable under low precipitation but showed a sharp rise and decline when precipitation exceeded 9.8 mm. We employed a random forest model to assess the factors influencing the soil layers’ response rates to rainfall and their soil moisture expansion potential during extreme rainfall events. The results emphasized that soil total nitrogen, organic carbon, and pH were more influential than physical properties, highlighting the significant interaction between soil moisture and nutrients and the potential important influence of vegetation on water movement in NLDF. Overall, NLDF’s sustained arability is attributed to its multi-dimensional, synergistic ecological layout. New dammed valley farmland should replicate NLDF’s structure by pre-establishing vertical soil layer distribution during landform reshaping and adopting a synergistic ecological layout that integrates vegetation, soil, and precipitation.</div></div>","PeriodicalId":11459,"journal":{"name":"Ecological Indicators","volume":"176 ","pages":"Article 113661"},"PeriodicalIF":7.0000,"publicationDate":"2025-05-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Soil water dynamics in a 450-year-old natural landslide-dammed valley farmland: Insights into precipitation responses\",\"authors\":\"Zhao Jin , Huifeng Wu , Hao Han , Yunchong Fu , Jing Zhang , Guofan Cao , Keyan Xu\",\"doi\":\"10.1016/j.ecolind.2025.113661\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Tens of thousands of sediment check dams have historically played vital ecological functions in China’s Loess Plateau, and dammed valley farmland has been a significant agricultural resource for centuries. However, newly created valley farmlands under the “Gully Land Consolidation” project often face lower arable quality and frequent soil salinization compared to their natural counterparts. To draw insights from natural dammed valley farmland, we selected the 450-year-old Huangtuwa natural landslide-dammed valley farmland (NLDF) for high-frequency, long-term monitoring and analysis of soil water content and precipitation during 2019–2020 and used the HYDRUS-1D model to assess its water storage capabilities. The results indicate that the soils from 0–100 cm can be clearly categorized into three groups: the rapid response layer (0–40 cm), which reacts quickly to rainfall; the water transport and emergency reservoir layer (∼60 cm), characterized by lower water content that fluctuates rapidly during extreme rainfall, functioning as both a reservoir and drainage pathway; and the stable water supply layer (∼100 cm), with the most stable water content (16.6 %, SD: 1.2 %), crucial for fertility and cultivation. Based on HYDRUS-1D model calculations, the soil water storage of NLDF remained stable under low precipitation but showed a sharp rise and decline when precipitation exceeded 9.8 mm. We employed a random forest model to assess the factors influencing the soil layers’ response rates to rainfall and their soil moisture expansion potential during extreme rainfall events. The results emphasized that soil total nitrogen, organic carbon, and pH were more influential than physical properties, highlighting the significant interaction between soil moisture and nutrients and the potential important influence of vegetation on water movement in NLDF. Overall, NLDF’s sustained arability is attributed to its multi-dimensional, synergistic ecological layout. New dammed valley farmland should replicate NLDF’s structure by pre-establishing vertical soil layer distribution during landform reshaping and adopting a synergistic ecological layout that integrates vegetation, soil, and precipitation.</div></div>\",\"PeriodicalId\":11459,\"journal\":{\"name\":\"Ecological Indicators\",\"volume\":\"176 \",\"pages\":\"Article 113661\"},\"PeriodicalIF\":7.0000,\"publicationDate\":\"2025-05-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Ecological Indicators\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1470160X25005916\",\"RegionNum\":2,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ecological Indicators","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1470160X25005916","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Soil water dynamics in a 450-year-old natural landslide-dammed valley farmland: Insights into precipitation responses
Tens of thousands of sediment check dams have historically played vital ecological functions in China’s Loess Plateau, and dammed valley farmland has been a significant agricultural resource for centuries. However, newly created valley farmlands under the “Gully Land Consolidation” project often face lower arable quality and frequent soil salinization compared to their natural counterparts. To draw insights from natural dammed valley farmland, we selected the 450-year-old Huangtuwa natural landslide-dammed valley farmland (NLDF) for high-frequency, long-term monitoring and analysis of soil water content and precipitation during 2019–2020 and used the HYDRUS-1D model to assess its water storage capabilities. The results indicate that the soils from 0–100 cm can be clearly categorized into three groups: the rapid response layer (0–40 cm), which reacts quickly to rainfall; the water transport and emergency reservoir layer (∼60 cm), characterized by lower water content that fluctuates rapidly during extreme rainfall, functioning as both a reservoir and drainage pathway; and the stable water supply layer (∼100 cm), with the most stable water content (16.6 %, SD: 1.2 %), crucial for fertility and cultivation. Based on HYDRUS-1D model calculations, the soil water storage of NLDF remained stable under low precipitation but showed a sharp rise and decline when precipitation exceeded 9.8 mm. We employed a random forest model to assess the factors influencing the soil layers’ response rates to rainfall and their soil moisture expansion potential during extreme rainfall events. The results emphasized that soil total nitrogen, organic carbon, and pH were more influential than physical properties, highlighting the significant interaction between soil moisture and nutrients and the potential important influence of vegetation on water movement in NLDF. Overall, NLDF’s sustained arability is attributed to its multi-dimensional, synergistic ecological layout. New dammed valley farmland should replicate NLDF’s structure by pre-establishing vertical soil layer distribution during landform reshaping and adopting a synergistic ecological layout that integrates vegetation, soil, and precipitation.
期刊介绍:
The ultimate aim of Ecological Indicators is to integrate the monitoring and assessment of ecological and environmental indicators with management practices. The journal provides a forum for the discussion of the applied scientific development and review of traditional indicator approaches as well as for theoretical, modelling and quantitative applications such as index development. Research into the following areas will be published.
• All aspects of ecological and environmental indicators and indices.
• New indicators, and new approaches and methods for indicator development, testing and use.
• Development and modelling of indices, e.g. application of indicator suites across multiple scales and resources.
• Analysis and research of resource, system- and scale-specific indicators.
• Methods for integration of social and other valuation metrics for the production of scientifically rigorous and politically-relevant assessments using indicator-based monitoring and assessment programs.
• How research indicators can be transformed into direct application for management purposes.
• Broader assessment objectives and methods, e.g. biodiversity, biological integrity, and sustainability, through the use of indicators.
• Resource-specific indicators such as landscape, agroecosystems, forests, wetlands, etc.