北部湾典型入海河流水沙变化及其对土地利用景观格局的响应
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1.南宁师范大学;2.南宁师范大学 地理科学与规划学院;3.广西北部湾海洋环境变化与灾害研究重点实验室;4.北部湾大学 海洋学院

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北部湾大学海洋科学广西一流学科(平陆运河建设背景下钦州湾动力地貌对水沙变化的响应,DRB006;《广西北部湾河口海岸研究与实践》教材建设,DTC003);国家自然科学基金(北部湾南流江三角洲潮滩响应热带气旋的动力地貌过程,42366008)


Changes of water and sediment in typical rivers entering the sea in Beibu Gulf and their response to land use landscape pattern
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Guangxi Key Laboratory of Marine Environment Change and Disaster in Beibu Gulf,Beibu Gulf University

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    摘要:

    [目的]土地利用变化是人类活动干预地形地貌变化的直观表现,景观指数可从景观生态学的角度描述土地利用的结构组成与空间配置。半个世纪以来,在气候变化和人类活动的影响下河流水沙呈现锐减的趋势,研究人类活动影响下中小河流水沙变化特征可为流域水土保持和航道水沙管理提供科学支撑。[方法]利用景观指数、水沙突变检验等方法,文章基于南流江、钦江流域近60年的水沙数据和相关土地利用数据,分析景观格局对水沙变化的影响。[结果]结果表明:(1)南流江和钦江流域的径流量和输沙量呈逐渐下降趋势。输沙量下降趋势比径流量的明显,径流量和输沙量的突变点都发生在21世纪00年代 。(2)钦江流域的林地由1990年占比38%增加至2020年的41.6%,南流江的耕地向林地转移面积逐渐增大。退耕还林政策取得成效,水沙变化也呈现逐渐减少的趋势。(3)两个流域的水沙变化与景观破碎化程度呈负相关关系、与斑块聚集度呈正相关关系。[结论]总体上南流江和钦江流域内土地利用变化格局保持较稳定,水沙变化受土地利用变化较明显,因此相关部门应该继续加强对生态用地的保护和管理 。为了防止水土流失,应该避免人类活动对景观格局的过度干扰,合理规划景观空间配置。

    Abstract:

    [Objective] Land use change is a visual manifestation of human activities intervening in topographic and geomorphic changes. The structural composition and spatial configuration of land use can be described through analyzing landscape index from the perspective of landscape ecology. In the past half century, under the influence of climate change and human activities, the water and sediment has been sharply reduced. The study of water and sediment changes in small and medium-sized rivers under the influence of human activities can provide scientific support for soil and water conservation and waterway water and sediment management in the watersheds. [Methods] Using the landscape index, water-sediment mutation test and other methods, the paper analyzes the influence of landscape patterns on water and sediment changes based on the data of water & sediment data and land use of Nanliu River and Qinjiang River Basins in the past 60 years. [Results] The results show that: (1) the runoff and sediment transport in the Nanliu River and Qinjiang River Basin show a gradual downward trend. The decreasing trend of sediment transport was more obvious than that of runoff, and the sudden change points of both runoff and sediment transport occurred in the 00s of the 21th century. (2) The proportion of forest land in Qinjiang River basin increased from 38% in 1990 to 41.6% in 2020, and the transfer area of cultivated land to forest land in Nanliujiang River gradually increased. The policy of returning farmland to forests has been effective, and the water-sediment change also shows a trend of gradual reduction. (3) The water-sediment changes in the two watersheds were negatively correlated with the degree of landscape fragmentation and positively correlated with the degree of patch aggregation. [Conclusion] In general, the land use change within the Nanliu River and Qinjiang River Basins remains stable, and the water-sediment change is more obviously affected by the land use change, so the relevant departments should strengthen the protection and management of eco-lands. In order to prevent soil erosion, excessive interference of landscape pattern by human activities should be avoided and landscape spatial configuration should be rationally planned.

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  • 收稿日期:2023-12-13
  • 最后修改日期:2024-03-06
  • 录用日期:2024-03-07
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