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Spatial-Temporal Dynamic Characteristics the Sanjiang Plain Marsh, China

机译:空间动态特征三江平原沼泽,中国

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By combining landscape ecology with GIS spatial analysis, this paper analyses the dynamics of the marsh landscape structure of the Sanjiang Plain in the past 30 years. Furthermore, taking Fujin County, located in the north of the plain, as an example, we analyze the conversion between marsh and other land use types. Ihe marsh in the Sanjiang Plain decreased greatly in the past 30 years, but the trend has begun to diminish. The marsh area decreased by 51.33% from 1980 to 1996, whereas it decreased by 4.19% from 1996 to 2009. The fragmentation of the marsh increased; the number of the patches increased by 326 from 1986 to 1996, whereas it only increased by 18 patches from 1996 to 2009. It is obvious that the speed of patch development diminished and the marsh fragmentation decreased, which shows that the reclamation of the marsh converted from the fragmentation of central area to the perimeter in large area of the marsh. The reclaimed marsh has been converted mainly to paddy field and dry land. Large-scale reclamation in the Sanjiang Plain influences its natural environment directly: the climate of the region turns from cold and wet to warm and dry, which makes the marsh both in the low-temperature north part and in the deeply stagnant east part suitable for further agriculture development. It is coincidental with the offset to southwest of the centroid of the marsh distribution in the Sanjiang Plain. The mechanism of marsh dynamics in the Sanjiang Plain is analyzed here. The marsh loss is mainly caused by human activities. It is impossible for the marsh in the Sanjiang Plain to naturally recover itself. Therefore, the restoration of the former marsh must rely on humans.
机译:通过用GIS空间分析结合景观生态学,本文分析了过去30年来三江平原沼泽景观结构的动态。此外,乘坐富士县位于平原北部,作为一个例子,我们分析了沼泽与其他土地使用类型之间的转换。在过去的30年里,在三江平原中,沼泽在三江平原下降,但趋势已经开始削弱。沼泽地区从1980年到1996年下降了51.33%,而它从1996年到2009年下降了4.19%。沼泽的碎片增加;从1986年到1996年增加了326的斑块的数量,而它只有18个修补程序从1996年到2009年增加了18个补丁。显然,贴片开发的速度减少,沼泽分散减少,表明沼泽转换的填海从中央区域的碎片到沼泽大面积的周边。回收的沼泽主要转换为稻田和干陆。三江平原的大规模垦区直接影响其自然环境:该地区的气候从寒冷和潮湿转动到温暖和干燥,这使得沼泽在低温北部和深度停滞的东部适合进一步的农业发展。它与西江平原沼泽分布的质心的偏移是掺合的。分析了三江平原中沼泽动力学的机制。沼泽损失主要由人类活动引起。三江平原中的沼泽是不可能自然恢复的。因此,前沼泽的恢复必须依赖人类。

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