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Spatial-Temporal Dynamic Characteristics the Sanjiang Plain Marsh, China

机译:三江平原湿地的时空动态特征

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摘要

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:通过将景观生态学与GIS空间分析相结合,分析了三江平原近30年来沼泽地景观结构的动态变化。此外,以平原北部的富锦县为例,我们分析了沼泽和其他土地利用类型之间的转换。在过去的30年中,三江平原的沼泽大大减少了,但是这种趋势已经开始减弱。从1980年到1996年,沼泽面积减少了51.33%,而从1996年到2009年减少了4.19%。从1986年到1996年,斑块的数量增加了326个,而从1996年到2009年,斑块的数量仅增加了18个斑块。很明显,斑块的发展速度降低了,沼泽的碎片化程度降低了,这表明沼泽的开垦已转化为沼泽。从中心区域的碎片到大面积沼泽的周边。开垦的沼泽地已主要转变为稻田和旱地。三江平原的大规模开垦直接影响着其自然环境:该地区的气候从寒冷潮湿转变为温暖干燥,这使得低温北部地区和深陷停滞的东部地区的沼泽都非常适合。农业的进一步发展。它与三江平原沼泽分布的质心向西南偏移是巧合的。本文分析了三江平原沼泽动力机制。沼泽地的损失主要是由于人类活动造成的。三江平原的沼泽不可能自然恢复。因此,恢复前沼泽必须依靠人类。

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