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首页> 外文期刊>Comptes rendus. Biologies >Spatial distribution of pH and organic matter in urban soils and its implications on site-specific land uses in Xuzhou, China.
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Spatial distribution of pH and organic matter in urban soils and its implications on site-specific land uses in Xuzhou, China.

机译:中国徐州城市土壤pH值和有机质的空间分布及其对特定土地利用的影响。

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摘要

The spatial variation of soil pH and soil organic matter (SOM) in the urban area of Xuzhou, China, was investigated in this study. Conventional statistics, geostatistics, and a geographical information system (GIS) were used to produce spatial distribution maps and to provide information about land use types. A total of 172 soil samples were collected based on grid method in the study area. Soil pH ranged from 6.47 to 8.48, with an average of 7.62. SOM content was very variable, ranging from 3.51 g/kg to 17.12 g/kg, with an average of 8.26 g/kg. Soil pH followed a normal distribution, while SOM followed a log-normal distribution. The results of semi-variograms indicated that soil pH and SOM had strong (21%) and moderate (44%) spatial dependence, respectively. The variogram model was spherical for soil pH and exponential for SOM. The spatial distribution maps were achieved using kriging interpolation. The high pH and high SOM tended to occur in the mixed forest land cover areas such as those in the southwestern part of the urban area, while the low values were found in the eastern and the northern parts, probably due to the effect of industrial and human activities. In the central urban area, the soil pH was low, but the SOM content was high, which is mainly attributed to the disturbance of regional resident activities and urban transportation. Furthermore, anthropogenic organic particles are possible sources of organic matter after entering the soil ecosystem in urban areas. These maps provide useful information for urban planning and environmental management.
机译:研究了徐州市区土壤pH和土壤有机质(SOM)的空间变化。常规统计,地统计学和地理信息系统(GIS)用于生成空间分布图并提供有关土地使用类型的信息。基于网格方法的研究区域共收集了172个土壤样品。土壤的pH范围为6.47至8.48,平均为7.62。 SOM含量变化很大,范围从3.51 g / kg到17.12 g / kg,平均为8.26 g / kg。土壤pH值呈正态分布,而SOM呈对数正态分布。半变异函数结果表明,土壤pH和SOM分别具有较强的空间依赖性(21%)和中等(44%)。变异函数模型对于土壤pH值是球形的,对于SOM是指数型的。使用克里金插值法获得空间分布图。高pH值和高SOM倾向于发生在混合林地覆盖区,例如市区的西南部,而在东部和北部则发现较低的值,这可能是由于工业和工业的影响。人类活动。在中心城区,土壤pH值低,但SOM含量高,这主要是由于区域居民活动和城市交通的干扰。此外,在进入市区土壤生态系统后,人为有机颗粒可能是有机物的来源。这些地图为城市规划和环境管理提供了有用的信息。

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