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黄河流域砒砂岩区地貌-植被-侵蚀耦合研究进展

申震洲 姚文艺 肖培青 饶良懿 李勉 杨吉山 焦鹏 荆诚然

申震洲,姚文艺,肖培青,等. 黄河流域砒砂岩区地貌-植被-侵蚀耦合研究进展[J]. 水利水运工程学报,2020(4):64-71 doi:  10.12170/20191229002
引用本文: 申震洲,姚文艺,肖培青,等. 黄河流域砒砂岩区地貌-植被-侵蚀耦合研究进展[J]. 水利水运工程学报,2020(4):64-71 doi:  10.12170/20191229002
(SHEN Zhenzhou, YAO Wenyi, XIAO Peiqing, et al. Research progress of spatial distribution about geomorphology-vegetation-water erosion in Pisha stone area of Yellow River[J]. Hydro-Science and Engineering, 2020(4): 64-71. (in Chinese)) doi:  10.12170/20191229002
Citation: (SHEN Zhenzhou, YAO Wenyi, XIAO Peiqing, et al. Research progress of spatial distribution about geomorphology-vegetation-water erosion in Pisha stone area of Yellow River[J]. Hydro-Science and Engineering, 2020(4): 64-71. (in Chinese)) doi:  10.12170/20191229002

黄河流域砒砂岩区地貌-植被-侵蚀耦合研究进展

doi: 10.12170/20191229002
基金项目: 国家重点研发计划资助项目(2017YFC0504503);国家自然科学基金资助项目(41201267)
详细信息
    作者简介:

    申震洲(1980—),男,河南安阳人,博士,正高级工程师,主要从事水土保持工作。E-mail:shenzz@139.com

    通讯作者:

    姚文艺(E-mail:wyyao@yrihr.com.cn

  • 中图分类号: S157.1

Research progress of spatial distribution about geomorphology-vegetation-water erosion in Pisha stone area of Yellow River

  • 摘要: 砒砂岩地区是黄河中游粗泥沙来源的核心区,是黄河流域生态保护的重点。揭示黄河中游砒砂岩地区地貌植被侵蚀耦合规律,对于砒砂岩区生态综合治理具有重要的理论指导价值。本文评述了砒砂岩区侵蚀地貌特征、植被生境空间分异规律、侵蚀空间分异规律,以及砒砂岩区地貌-植被-侵蚀空间耦合关系研究进展,并展望了其研究发展趋势。同时,提出了今后应加强研究的方向:应着重从机理层面对砒砂岩区的地形地貌空间结构分异特征、植被生境和群落分异特征及侵蚀时空分异特征进行深入研究,特别是将三者作为一个耦合系统的因素进行研究,解决制约砒砂岩区水土流失综合治理理论水平提升与实践的瓶颈问题;研究不同地貌单元的土壤侵蚀年内时空分异性特征及其成因,揭示坡沟系统水蚀年内时空分异性特征与自然植被时空分异性特征的耦合机理;揭示砒砂岩区地貌-植被-水蚀空间耦合机理。本综述可为黄河流域砒砂岩区生态保护、侵蚀规律研究及高质量发展提供一定参考。
  • 图  1  覆土砒砂岩的岩石互层结构

    Figure  1.  Interbedded structure in soil-covered Pisha stone

    图  2  砒砂岩分布范围

    Figure  2.  Distribution range of Pisha stone

    图  3  裸露和覆土砒砂岩区地形地貌

    Figure  3.  Bared and soil-covered Pisha stone area

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