在典型红壤丘陵区平均坡度为10°的坡耕地径流小区(2 m×5 m)上进行降雨强度为1.69mm min-1(大雨强)、1.31 mm min-1(中雨强)和0.64 mm min-1(小雨强)的模拟降雨试验,并对模拟降雨过程中泥沙的迁移规律和土壤有机碳的流失富集规律进行了研究。结果表明:侵蚀作用下土壤流失量随着降雨强度的增大而增加,并与径流量呈显著的立方关系,径流量是坡耕地土壤流失的重要影响因素;土壤有机碳流失以泥沙结合态为主,泥沙态有机碳流失量占总有机碳流失量的84%以上,最高达97.6%;泥沙中有机碳富集比随着降雨强度的增大而减小,有机碳的选择性迁移在低强度降雨条件下表现更为明显;中雨强和小雨强下有机碳的富集比与黏粒的富集比分别呈极显著和显著正相关,而大雨强泥沙有机碳富集比与黏粒富集比没有显著的线性关系。雨强是影响泥沙流失和泥沙有机碳迁移的重要因素。
Batch and soil column experiments were conducted to evaluate the influence of KH2PO4, （NH4）H2PO4and Ca（H2PO4）2on the adsorption and leaching characteristics of Cu and Zn in red soil. The results show that all the three phosphates can greatly improve the adsorption capacity of red soil for Cu and Zn, and the effect of different phosphates on Cu and Zn adsorption follows the order of Ca（H2PO4）2〉KH2PO4〉（NH4）H2PO4. The addition of phosphate has little effect on the mobility of Cu. Ca（H2PO4）2and （NH4）H2PO4 show a strong ability in immobilizing Zn while the immobilization ability of KH2PO4 is much weaker. All the three phosphates are helpful for modifying the partitioning of Cu and Zn from the non-residual phase to the residual phase; however, they could also enhance the contents of Cu and Zn associated with exchangeable and carbonates fractions.
