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岷江上游干旱河谷边界波动的定量判定及其演化特征

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在山区人口迅速增加和社会经济高速发展的进程中,干旱河谷作为山区生态系统的重要组成部分之一,承载了严重的被干扰和过度利用.在RS与GIS技术的支持下,本研究选择岷江上游干旱河谷作为研究对象,应用马尔科夫预测法和土地利用动态变化空间分析测算模型,开展干旱河谷边界波动的定量判定及其演化特征研究.研究结果表明:岷江上游干旱河谷区面积与上边界在逐年增加,上边界平均每年沿垂直方向抬升约5 m,在未来较长时间内,干旱河谷面积的增长趋势将会越来越强;其中,1970至2010年干旱河谷转化速率(TRL70-2010)呈现不断上升趋势,分别为TRL70=1.44%,TRL80=0.95%,TRL90=2.32%,TRL2000=2.45%,TRL2010=3.59%;1990至2000年期间干旱河谷新增速率(IRL90-2000)最大,属于高速扩展期,在1970至1980年期间新增速率IRL70-80最小;1990至2000年期间干旱河谷"敏感性"最高,其年变化速率(CCL90-2000)为13.01%,其次为CCL2000-2010=6.51%,其余时期年均变化速率皆在4%左右.本研究结果可为我国西部灾害多发区聚落合理规划、灾害风险管理、人口合理分布与再调整提供重要的科学依据.
Quantitative Determination of Boundary Fluctuation in Arid Valley of the Upper Min River and Its Evolution Feature
Summary:With rapid population growth and socio-economic development in mountainous regions of western Chi-na,arid valleys are acting as an important part in support of mountain ecosystems and suffering serious engineered interference and over-exploitation.With the help of RS and GIS technology,this research took arid valleys in the upper reaches of Min River as a case study.It applied the Markov prediction method and the model of dynamic change of land use space analysis calculation to perform a quantitatively investigation on the boundary fluctuation of arid valleys in the upper reaches of Min River and its evolutionary features.Results confirmed that:The area of ar-id valleys in the upper reaches of Min River and its upper border had been growing for years,On an annual average, the upper boundary kept uplifting about 5 m per year in the vertical direction,and the growth trend in the arid valley areas would be getting stronger in the long run;During 1970 to 2010,the expansion rate of arid valley(TRL70-2010) presented a rising trend,with TRL70=1.44%, TRL80=0.95%, TRL90=2.32%, TRL2000=2.45%, TRL2010=3.59%.separately;And arid valleys had been highly developing from 1990 to 2000 with a unprecedented maxi-mum rate(IRL90-2000),which was regarded as high-speed expansion period,whereas for the period of 1970 to 1980,its rate IRL70-80dropped to the minimum;As for the period of 1990 to 2000,arid valley had the highest"sen-sitivity",with a annual rate of change(CCL90-2000)13.01%,followed by CCL2000-2010=6.51%,and in the remai-ning period,a average annual rate of change was about 4%.This research achievement can provide important scien-tific basis for rational site planning for settlements,disaster risk management,proper population distribution and re-adjustment in some areas of western China with a high susceptibility in geohazards.

arid valleyboundary fluctuationevolution patternrisk managementthe upper reaches of Min River

丁明涛、周鹏、张永旺、吕夏婷

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西南科技大学 环境与资源学院,四川 绵阳621010

重庆市彭水苗族土家族自治县水务局,重庆 彭水409600

干旱河谷 边界波动 演化特征 风险管理 岷江上游

四川省青年科技基金国家自然科学基金教育部人文社会科学研究专项任务项目

2017JQ00514137118515JDGC019

2017

山地学报
中科院水利部成都山地灾害与环境研究所 中国地理学会

山地学报

CSTPCDCSCD北大核心
影响因子:1.275
ISSN:1008-2786
年,卷(期):2017.35(2)
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