Results show that P availability in latosol derived from shallow-sea deposit is higher than that in latosol derived from basalt.
砖红壤磷有效性低的主要原因是土壤活性铝、铁、锰含量高，另外与土壤中
态无机磷
无机磷比
有
。
Results show that P availability in latosol derived from shallow-sea deposit is higher than that in latosol derived from basalt.
砖红壤磷有效性低的主要原因是土壤活性铝、铁、锰含量高，另外与土壤中态无机磷无机磷比有。
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