长江流域资源与环境 >> 2015, Vol. 24 >> Issue (09): 1552-1559.doi: 10.11870/cjlyzyyhj201509016
赵新新1, 金晓斌1, 杜心栋1, 周寅康1, 刘海玲2
ZHAO Xin-xin1, JIN Xiao-bin1, DU Xin-dong1, ZHOU Yin-kang1, LIU Hai-ling2
摘要: 滩涂湿地在吸收、转化和滞留氮、磷等营养元素方面具有重要功能。选取江苏东部沿海典型滩涂区,分别对垦殖时间为0、3、6、17、30、60 a的沿海滩涂进行采样,对相应的土壤氮总转化速率指标进行实验测定。结果表明,滩涂垦殖后,表征氮素活化过程的指标,如总矿化率、总硝化率、净矿化率和净硝化率等有所增加,而有利于氮固持的铵态氮同化率指标无显著变化,硝态氮同化率指标变慢;围垦期限超过30 a后,各氮总转化速率指标渐趋稳定。相关性分析表明,净矿化率、总矿化率、铵态氮同化率、净硝化率、总硝化率与围垦年限呈显著正相关(p<0.01),相关性系数分别为0.966、0.929、0.819、0.800、0.798;硝态氮同化率与围垦年限呈显著负相关(p<0.01),相关性系数为-0.685;除铵态氮外,全氮、硝态氮、pH值、有机碳均与各氮总转化速率指标呈显著相关关系(p<0.01)。滩涂垦殖后土壤理化性质指标的改变带来土壤氮总转化速率的变化,一定程度上破坏了土壤氮生态系统平衡。
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