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Spatial pattern of soil organic carbon and total nitrogen, and analysis of related factors in an agro-pastoral zone in Northern China

机译:土壤有机碳的空间模式及全氮气,以及中国北方农业田园区的相关因素分析

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摘要

The spatial pattern of soil organic carbon (SOC) and total nitrogen (TN) densities plays a profound important role in estimating carbon and nitrogen budgets. Naiman Banner located in northern China was chosen as research site, a total of 332 soil samples were taken in a depth of 100 cm from the low hilly land in the southern part, sandy land in the middle part and an alluvial plain in the northern part of the county. The results showed that SOC and TN density initially decreased and then increased from the north to the south, The highest densities, were generally in the south, with the lowest generally in the middle part. The SOC and TN densities in cropland were significantly greater than those in woodland and grassland in the alluvial plains and for Naiman as a whole. The woodland SOC and TN density were higher than those of grassland in the low hilly land, and higher densities of SOC and TN in grassland than woodland in the sandy land and low hilly land. There were significant differences in SOC and TN densities among the five soil types of Cambisols, Arenosols, Gleysols, Argosols, and Kastanozems. In addition, SOC and TN contents generally decreased with increasing soil depth, but increased below a depth of 40 cm in the Cambisols and became roughly constant at this depth in the Kastanozems. There is considerable potential to sequester carbon and nitrogen in the soil via the conversion of degraded sandy land into woodland and grassland in alluvial plain, and more grassland should be established in sandy land and low hilly land.
机译:土壤有机碳(SOC)和总氮(TN)的密度的空间模式起着估算碳和氮的预算产生深远的重要的作用。奈曼旗位于中国北部被选为研究点,一共有332个土壤样品在100厘米的深度采取从低丘岗地在南部的部分,中间部分沙地及北部的冲积平原县。结果表明,SOC和TN密度最初在南方的中间环节减少,然后从北面提高到南部,密度最高,普遍,最低一般。农田SOC和TN密度显着高于在冲积平原林地和草地和奈曼作为一个整体显著更大。林地SOC和TN密度均高于低草地丘陵地的更高,和SOC和TN的草地比在沙地和低丘陵地带林地更高的密度。有五种类型土壤雏形土,红砂土,潜育土,Argosols和Kastanozems之间的SOC和TN密度显著差异。另外,SOC和TN内容一般与土壤深度的增加而降低,但在雏形土的40cm的深度以下增加,并在该深度在Kastanozems成为大致恒定。有相当大的潜力螯合碳和氮中的经由退化沙地在冲积平原转化为林地和草地土壤,更草原应在沙地和低丘陵土地来建立。

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