蓄水对三峡库区消落带土壤和植被的影响研究进展OA
Effects of Impoundment on Soil and Vegetation in the Water-Level Fluctuation Zone of Three Gorges Reservoir
三峡水库"蓄清排浑"的运行模式致使三峡库区消落带与自然消落带截然不同.综述了近十几年来三峡水库蓄水前后消落带土壤理化性质和植物群落的变化情况.相关研究表明,蓄水后消落带土壤pH、土壤有机碳和总氮等变化显著,土壤pH逐渐趋于中性,土壤有机碳和总氮含量随水位涨落周期的增加呈下降趋势.土壤质地、容重等物理性质和土壤pH、有机碳和总氮等化学性质随着水位高程的变化也会发生相应改变.干流和支流消落带植物群落组成和物种多样性均已发生显著变化,许多原有陆生植物难以适应新的生境而消亡.不同水位高程区植物组成和物种多样性也不同,优势物种以狗牙根(Cynodon dactylon)和苍耳(Xanthium strumarium)为主,新的稳定植物群落已逐渐形成.今后应加强消落带先锋物种对环境胁迫的生理生态响应研究,进一步完善消落带生态系统植物-土壤-水耦合关系研究,开展土壤碳氮的主要损失形态和途径分析,并对消落带生态系统进行长时序、大尺度的调查,为三峡库区消落带生态恢复和重建提供参考.
The water-level fluctuation zone(WLFZ)in Three Gorges Reservoir is a land-water ecotone formed by periodic water level fluctuation in the mainstream and tributaries of the Yangtze River im-pounded by Three Gorges Dam.The operating mode of'storing clear water and discharging muddy water'from Three Gorges Reservoir makes the WLFZ of Three Gorges Reservoir entirely different from natural water-level fluctuation zones.In this study,we reviewed the changes of soil physical and chemical proper-ties and vegetation communities in the WLFZ before and after impoundment of Three Gorges Reservoir over the past ten years.Relevant studies showed that soil pH,soil organic carbon and total nitrogen changed significantly after impoundment.The soil pH gradually tended toward neutral,and the contents of soil organic carbon and total nitrogen decreased with the number of water level fluctuation cycles.Physical properties such as soil texture and bulk density and chemical properties such as soil pH,soil or-ganic carbon and total nitrogen varied with water level elevation.Plant community composition and spe-cies diversity in the WLFZ of the mainstem and tributaries have changed significantly,and many of the original terrestrial plants have not adapted to the altered habitat and died out.Plant composition and diver-sity also varied with location within the WLFZ.Prior to inundation,the dominant species were primarily Cynodon dactylon and Xanthium strumarium and new plant communities have gradually formed.In the future,it is imperative to intensify research on the physiological and ecological responses of pioneer spe-cies within the WLFZ to environmental stressors.Additionally,there is a need to further refine our under-standing of the plant-soil-water coupling dynamics in the WLFZ ecotone.It is also crucial to undertake analysis focusing on the primary loss mechanisms and pathways of soil carbon and nitrogen and conduct-ing long-term,large-scale surveys of the WLFZ ecotone are essential.These efforts,collectively,provide valuable insights and references for ecological restoration and reconstruction endeavors in the WLFZ of Three Gorges Reservoir.
李秋宏;王小国;刘祥龙
中国科学院、水利部成都山地灾害与环境研究所,四川 成都 610299中国科学院大学,北京 100049中国科学院、水利部成都山地灾害与环境研究所,四川 成都 610299
资源环境
蓄水消落带土壤理化性质植物群落三峡库区
impoundmentwater-level fluctuation zonephysicochemical soil propertiesvegetation communityThree Gorges Reservoir
《水生态学杂志》 2026 (1)
252-264,13
国家自然科学基金(E1K1290290).
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