淤泥
肥料
总有机碳
粒径
氮气
有机质
壤土
色散(光学)
分馏
土壤碳
土工试验
大块土
化学
炭黑
粒度分布
环境化学
堆积密度
土壤科学
土壤有机质
土壤水分
环境科学
农学
地质学
色谱法
物理化学
古生物学
物理
光学
天然橡胶
有机化学
生物
作者
Ying Yan,Hongfeng Xie,Hongbo He,Bai Zhang,Ying Chen,Xudong Zhang
摘要
The black soil fertilized with different amount of pig manure for 21 years was sampled from Gongzhuling long-term station. Fine clay( less than or equal 0.2μm), coarse clay (0.2-2μm), silt(2-53μm), fine sand(53-250μm) and coarse sand (250-2000μm) fractions were obtained by ultrasonic dispersion, centrifugation and wet sieving separation. Soil organic carbon(SOC) and total nitrogen(TN) were detected in bulk soil and particle-size fractions. The results show that soil organic matter mostly exist in the silt plus clay, and the ratios of carbon to nitrogen become narrow with particle size decreasing. Soil organic carbon in fine clay fraction is characterized by a more rapid turnover than in the coarse clay fraction. Except for the fine sand, the SOC, TN concentrations in bulk black soil and other size fractions increase significantly with the increase of pig manure application. The application of pig manure resulted in the increase of the enrichment coefficients of SOC and TN in coarse sand, while the decrease in clay fraction, especially in coarse clay. Moreover, C / N ratios in silt and sand fractions narrowed markedly. Change of pig manure application amount affected the concentrations of SOC, TN significantly, while C / N ratios slightly in both bulk soil and particle-size fractions.
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