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Soil Organic Matter Dynamics in a Sloped Sandy Cropland of Northeast Thailand with Special Reference to the Spatial Distribution of Soil Properties

机译:泰国东北坡地沙质农田土壤有机质动力学特征及其空间分布特征

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摘要

Sandy soils are widely distributed in Northeast Thailand. We analyzed the spatial distribution of soil properties and the dynamics of organic matter on a sloped cropland near Khon Kaen city in Northeast Thailand. Our research site included a sugarcanefield on the main slope, a mango plantation on the lower slope, a wetland rice field in the lowland, and a teak plantation on the opposite slope. 116 soil samples were collected from this 510 X 270 m field at 30-m intervals, and the spatial distributions of various soil properties were evaluated using geostatistical analysis. A clear spatial variation was observed for organic C and N soil content, particle size distribution, and other related properties. In the teak and mango plantations, the soil texture was finer and the C and N levels were higher than in the sugarcane field. Soil organic matter (SOM) dynamics and soil erosion were postulated to be driving forces behind the observed heterogeneity in soil properties. The dynamics of the SOM were analyzed in five plots, which were representative of the site's topography and land use. Both the SOM stock and annual soil respiration were higher under tree vegetation than in the sugarcane plots, as measured in the upper 15 cm of the soil layer. Annual soil respiration was high, often exceeding 40% of the total SOM stock. The SOM was observed to rapidly increase under tree vegetation through litter input. The redistribution of soil properties through SOM dynamics could be easily implemented in this sandy, sloped land.
机译:沙土在泰国东北部广泛分布。我们分析了泰国东北部孔敬市附近坡耕地土壤特性的空间分布和有机质的动态。我们的研究地点包括主坡地上的甘蔗田,低坡地上的芒果种植园,低地上的湿地稻田和对面的柚木种植园。从510 X 270 m的田地以30 m的间隔收集了116个土壤样品,并使用地统计学方法评估了各种土壤性质的空间分布。观察到有机碳和氮的土壤含量,粒径分布和其他相关特性的明显空间变化。在柚木和芒果种植园中,土壤质地比甘蔗田更细,碳和氮含量更高。假定土壤有机质(SOM)动力学和土壤侵蚀是造成土壤特性异质性的驱动力。在五个样地中分析了SOM的动态,这些样地代表了站点的地形和土地利用。在土壤植被的上层15厘米处测得,树木植被下的SOM储量和年度土壤呼吸均高于甘蔗地。每年的土壤呼吸很高,经常超过SOM总量的40%。观察到,通过垫料输入,SOM在树木植被下迅速增加。通过SOM动力学对土壤性质的重新分配可以在这片沙质的坡地上轻松实现。

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