长江流域资源与环境 >> 2016, Vol. 25 >> Issue (02): 307-315.doi: 10.11870/cjlyzyyhj201602017
王娅娅1, 杨艳芳2, 李云飞1, 刘文静1, 张平究1
WANG Ya-ya1, YANG Yan-fang2, LI Yun-fei1, LIU Wen-jing1, ZHANG Ping-jiu1
摘要: 选取菜子湖区不同退耕年限(3、5、7、9、11和21 a)湿地、以仍耕油菜地和原始湿地土壤为研究对照,分析了土壤全铝和活性铝形态组分特征,探讨退耕还湖后湿地土壤铝元素组分特征变化及其生态效应。结果表明,研究区土壤全铝含量和活性铝含量分别在16.78~57.05 g/kg和1 699.94~3 823.49 mg/kg之间,其中活性铝总量占全铝含量的6.70%~11.84%。退耕还湖3~11a期间,土壤全铝、活性铝总量及5种形态活性铝总体均随退耕年限延长而增加;退耕11~21 a期间均下降。不同形态活性铝中,可溶性铝AlS含量最低,而酸溶无机铝Al(OH)30和腐殖酸铝Al-HA含量较高,分别占活性铝总量的42%~53% 和39%~50%,左右着活性铝总量的变化。分析讨论表明退耕后湿地植被和水文条件的改变导致土壤粘粒,有效磷和有机质的变化,进而影响退耕后土壤活性铝组分特征。其中0~5 cm土壤毒性较强的交换性铝Al3+和羟基铝Al(OH)2+、Al(OH)2+含量均在退耕3~9 a期间逐渐增加,占活性铝总量的比例也有所增加,该退耕期湿地土壤存在一定的铝毒生态风险。
中图分类号:
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