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水蚀风蚀交错区流域景观格局变化及水沙响应关系

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为揭示土壤侵蚀最为剧烈的水蚀风蚀交错区下垫面景观格局变化对流域降雨产流、侵蚀产沙的影响程度,以水蚀风蚀交错区典型流域西柳沟为研究对象,根据Landsat TM影像数据和流域长系列水沙实测数据资料,借助GIS和Fragstats平台,分析流域景观格局和水沙变化特征,探讨景观指数与径流输沙的关系。结果表明:1)流域优势景观类型为草地,从斑块数量和面积变化率来分析,1985-2010年间耕地、林地和建设用地稳定性最高,其次为未利用土地。未利用土地、草地和耕地的转化最为剧烈,受人类活动影响最大。2)流域年径流量和年输沙量的年际差异显著;同年输沙量相比,径流量的减小趋势变化更为明显;径流泥沙相关关系显著,相关系数为0。67。3)景观指数与径流量、泥沙量呈显著线性相关,其中径流量与最大斑块指数、斑块结合度、聚集度指标和蔓延度指数均呈负相关,而与景观形态指数、景观分割度呈正相关;而泥沙仅与蔓延度指数、聚集度指标和斑块结合度成负相关,与其他景观指数呈正相关。研究结果表明,随着景观最大斑块指数、斑块结合度以及聚集度指数的提高,流域降雨入渗量明显增加,土壤侵蚀量明显减少;因此,提高流域景观最大斑块指数、斑块结合度以及聚集度指数可以增强水蚀风蚀交错区内流域的蓄水保土功能及生态优化作用,研究结果可为流域生态环境建设和水土资源综合利用提供理论支撑。
Relationships between landscape, runoff, and sedimentation in wind-water erosion crisscross region
[Background] Sedimentation and runoff variation caused by land use change has been emerged as one of the popular topics of discussion.And the phenomena is more obvious in wind-water erosion crisscross region than in other erosion region,thus it is necessary to study the effects of land use change on runoff and sediment in wind-water erosion crisscross region.Xiliu Gully watershed is the typical watershed in wind-water erosion crisscross region.[Methods] In order to meet the demand of ecological environment construction and comprehensive utilization of water and soil resources,and to put forward an actual production theory for our river basin management,relationships between landscape,runoff,and sedimentation were studied on the basis of long-term historical land use,runoff,and sediment data (1985-2010) by geographic information system and Fragstats software.[Results] 1) According to the Landsat TM data in 1985,1996,2000 and 2010,the spatial variation characteristics of the landscape pattern were analyzed.Grassland was the dominant landscape in the watersheds.Farmland,forest and construction land were in the highest stability,and the second main landscape type was unused land. Unused land,grassland and farmland experienced the greatest changes,which were suffered seriously from human activities.2) Precipitation,annual runoff and sediment changed significantly in last 50 years,but the variation amplitude of them was different.Average precipitation from 1960 to 2010 changed not so obviously,however runoff and sediment were decreased significantly.Moreover,the decreasing trend of runoff was more obvious than sediment in the same year.A Pearson correlation analysis showed that there was a significant correlation between annual runoff and sedimentation (P < 0.01).3) The variation of landscape status played an important role in the progress of precipitation to runoff,which not only inflected the output of the runoff and sediment,but also changed the mechanism of the rainfall to runoff.The main landscape ecological indexes,such as patch density,largest patch index,patch and spent landscape,et al.were analyzed,and the relationships between landscape pattern and runoff,sediment were studied.The Pearson correlation analysis showed that the landscape indexes (shorted for Lis) were in significant linear correlation with runoff and sedimentation.Largest Patch Index (LPI),Patch Cohesion Index (COHESION),Aggregation Index (AI) and Contagion Index (CONTAG) were negatively correlated with annual runoff,whereas Landscape Shape Index (LSI) and Landscape Division Index (DIVISION) were positively.CONTAG,AI and COHESION were negatively correlated with annual sedimentation,whereas other landscape indexes were positively.[Conclusions] From soil and water conservation in the watersheds,it was useful to increase soil infiltration and reduce soil erosion by improving LPI,COHESION,AI and CONTAG,which was also useful for the ecological construction and soil water resources utilization.

wind-water erosion crisscross regionlandscaperunoffsedimentationXiliu Gully watershed

王金花、李占斌、张荣刚、姚文艺

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西安理工大学西北旱区生态水利工程国家重点实验室培育基地,710048,西安

黄河水利科学研究院水利部黄土高原水土流失过程与控制重点实验室,450003,郑州

黄河水利委员会水文局,450004,郑州

水蚀风蚀交错区 景观格局 径流量 输沙量 西柳沟流域

国家重点基础研究计划(“973”计划)第三课题中央公益性科研院所专项经费项目河南省创新型科技人才队伍建设工程

2011CB403303HKY-2011-15162101510004

2016

中国水土保持科学
中国水土保持学会

中国水土保持科学

CSTPCDCSCD北大核心
影响因子:0.902
ISSN:1672-3007
年,卷(期):2016.14(3)
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