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Shrinkage and fragmentation of grasslands in the West Songnen Plain, China

机译:松嫩平原西部草原的萎缩和破碎化

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摘要

In the past century, especially the past five decades, the grasslands of the West Songnen Plain, Northeast China, were rapidly converted into croplands and salinized wasteland, and experienced a fragmentation process that is still ongoing. Almost no information is available on the spatial-temporal changes of grasslands in this area. In this study, grassland cover change, agricultural reclamation and salinized wasteland expansion were investigated during the past five decades. Grassland fragmentation was studied based on four landscape metrics. The grassland cover change was detected from a time series of topographic maps from 1954, satellite images of Landsat TM in 1986, 1995, and 2000 using remote sensing and geographic information systems (GIS). In addition, the land use changes were analyzed using a transition matrix of land use types, while the driving forces were explored according to climatic changes and socioeconomic developments. The results indicated a significant decrease in grassland area. Of the 1418 945 ha of native grassland in 1954, approximately 64% was removed by 2000, while the number of patches (NP) increased from 865 to 2035 and the mean patch size (MPS) decreased from 1640 ha to 252 ha. During the whole study period, the average annual decrease rate of grassland was 34 894 ha/year. Cropland and salinized wasteland were the two main land use types into which grassland converted. During the past decades, obvious climatic changes occurred, which supplied a favorable potential environment for agricultural development but damaged grassland productivity. On the other hand, population, GDP and livestock number increased significantly as grassland quality decreased. According to the results, the shrinkage and fragmentation of grasslands may well be explained by socioeconomic development and aided by changing climatic conditions. (C) 2008 Elsevier B.V. All rights reserved.
机译:在过去的一个世纪中,尤其是在过去的五十年中,中国东北的松嫩平原西部的草原迅速转变为农田和盐碱化的荒地,经历了持续的破碎过程。几乎没有关于该地区草地时空变化的信息。在这项研究中,对过去五年来的草地覆盖变化,农业开垦和盐碱化荒地扩展进行了调查。基于四个景观指标对草地破碎化进行了研究。利用遥感和地理信息系统(GIS),从1954年的地形图,1986年,1995年和2000年的Landsat TM的卫星图像的时间序列中检测出草地的变化。此外,利用土地利用类型的转换矩阵分析了土地利用的变化,同时根据气候变化和社会经济发展探索了驱动力。结果表明草原面积明显减少。在1954年的1418 945公顷原生草地中,到2000年,约有64%的土地被清除,而斑块数量(NP)从865增加到2035,平均斑块大小(MPS)从1640公顷减少到252公顷。在整个研究期间,草地的年均减少量为34894公顷/年。耕地和盐渍化荒地是草地转化成的两种主要土地利用类型。在过去的几十年中,发生了明显的气候变化,为农业发展提供了有利的潜在环境,但损害了草地的生产力。另一方面,随着草地质量的下降,人口,GDP和牲畜数量显着增加。根据结果​​,草原的萎缩和破碎可能可以用社会经济发展来解释,而气候条件的改变则可以帮助。 (C)2008 Elsevier B.V.保留所有权利。

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