首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Spatial distribution pattern changes of oasis soil types in Manasi River Basin, arid northwestern China.
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Spatial distribution pattern changes of oasis soil types in Manasi River Basin, arid northwestern China.

机译:西北干旱地区玛纳斯河流域绿洲土壤类型的空间分布格局变化

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Soil distribution pattern play a significant role in the stability conservation and economic development of oasis in arid regions. Hence, ecologists and agrology scientists have a central interest in understanding the spatial distribution changes of soil types. The aim of this study was to analyze the main processes of soil distribution pattern changes from 1987 to 2006 through the landscape indexes. Soil types and soil distribution pattern changes were assessed and compared by using two soil maps made in 1987 and 2006. 14 soil types were classified and analyzed in the study area. Results indicated many differences among the changes of different soil types. During the period from 1987 to 2006, there were widespread changes in spatial distribution of soil types in Manasi River Basin at class-level. The area of Petrocambids decreased, whereas Aquicambids increased. The small patches began to coalesce into large ones and the patch numbers decreased during the past 20 years, which brought about the fragmentation decrease in Manasi River Basin. In contrast to the decrease of the patch density, the average patch area of 12 soil types increased. With the increasing man-made disturbance, more soil type patches, especially the agricultural soil patches were close to square in shape. During the recent 20 years, the decreased patch shape indexes occupied about 57% of all while the increased patch shape indexes were over 40%. The split index of most soil types has also declined during the same period. The landscape-level indexes also reflected the spatial distribution changes of oasis soil types. The landscape diversity index and landscape evenness index have increased while the landscape dominance index has decreased in the recent 20 years, which showed that more equirotal soil patches were formed and various soil types dominated the soil landscape in Manasi River Basin. Changes of different soil types are one of major indictors to show environment changes and impacts of human activities. Therefore, it is necessary to emphasize the study of soil type changes in the arid and semiarid region.Digital Object Identifier http://dx.doi.org/10.1016/j.catena.2011.06.001
机译:土壤分布格局在干旱地区绿洲的稳定性保护和经济发展中起着重要作用。因此,生态学家和农业学家对了解土壤类型的空间分布变化具有主要兴趣。这项研究的目的是通过景观指数分析1987年至2006年土壤分布格局变化的主要过程。利用1987年和2006年制作的两张土壤图对土壤类型和分布格局的变化进行了评估和比较。研究区域对14种土壤类型进行了分类和分析。结果表明,不同土壤类型的变化之间存在许多差异。在1987年至2006年期间,玛纳斯河流域的土壤类型空间分布发生了广泛的变化。 Petrocambids的面积减少,而Aquicambids的面积增加。在过去的20年中,小斑块开始聚集成大斑块,而斑块数量减少了,这导致了玛纳斯河流域的破碎化减少。与斑块密度的下降相反,12种土壤类型的平均斑块面积增加了。随着人为干扰的增加,更多的土壤类型斑块,特别是农业土壤斑块形状接近正方形。在最近的20年中,下降的斑块形状指数约占总数的57%,而上升的斑块形状指数超过40%。同期大多数土壤类型的分裂指数也下降了。景观水平指标也反映了绿洲土壤类型的空间分布变化。近20年来,景观多样性指数和景观均匀度指数上升,景观优势指数下降,说明玛纳斯河流域形成的等旋土壤斑块较多,各种土壤类型主导着土壤景观。不同土壤类型的变化是显示环境变化和人类活动影响的主要指标之一。因此,有必要着重研究干旱和半干旱地区土壤类型的变化。数字对象标识符http://dx.doi.org/10.1016/j.catena.2011.06.001

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