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The impact of different grazing intensity on topsoil physical and chemical properties in Xilamuren grassland

机译:不同放牧强度对XILAMUREN草原上的表土物理性质的影响

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Grassland is an important ecosystem in land surface. Soil is the basis of grassland ecosystem, and the changes of its properties directly affect grassland ecosystem. The study region is located in Xilamuren grassland using the methods of field sampling and experimental analysis. It was divided into four test areas according to grazing intensity. Soil physical and chemical properties were analyzed in each test area. The results showed that: the trend of soil water content decreased and then increased with increasing grazing intensity, soil water content in repaired grassland was the lowest. For the soil mechanical composition, particle size content increased first and then decreased with increasing grazing intensity when the particle size was 1-0.05mm. The difference between the highest and lowest values was obvious. When the particle size was 0.05-0.002mm, the trend of particle size fluctuated, first decreased and then increased, finally reduce again and the difference between the highest and lowest values was obvious. When the particle size was less than 0.002mm, the trend of particle size content increased with increasing grazing intensity. In soil chemical properties, soil organic matter appears downward trend overall as grazing intensity increase. Soil organic matter content was the lowest in repaired grass. Available N and P first decreased and then increased with increasing grazing intensity, the minimum values appeared in the repaired grassland and degraded grassland respectively. Available K content increased with increasing grazing intensity.
机译:草原是陆地表面的重要生态系统。土壤是草原生态系统的基础,其物业的变化直接影响草原生态系统。该研究区位于Xilamuren草原,使用现场采样和实验分析。根据放牧强度,它分为四个测试区域。在每个测试区分析土壤物理和化学性质。结果表明:土壤含水量的趋势下降,随后随着放牧强度的增加而增加,修复草原的土壤水含量最低。对于土壤机械组合物,粒度含量升高,然后在粒径为1-0.05mm时随着放牧强度的增加而降低。最高和最低值之间的差异是显而易见的。当粒径为0.05-0.002mm时,粒径波动的趋势,首先降低,然后增加,最终再次减少,最高和最低值之间的差异是显而易见的。当粒径小于0.002mm时,粒度含量的趋势随着放牧强度的增加而增加。在土壤化学性质中,由于放牧强度增加,土壤有机质总体上显示下降趋势。土壤有机质含量是修复的草丛中最低的。可用N和P首先降低,然后随着放牧强度的增加而增加,在修复的草地和降解草原中出现了最小值。随着饲养强度的增加,可用的K含量增加。

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