低位泥炭沼泽 low moor

互联网2013-11-14

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　　在湖沼或河边等地下水位非常高的水湿地方形成的平坦沼泽。其组成种是以芦苇、菅茅类为优势种，所以又称为芦苇 -菅茅沼泽。地下水上升所供给的无机盐类（特别是碱性盐类），其所解离出的离子为腐殖质吸附饱和以致形成中性泥炭，但不生长水藓。以这点和养料丰富而与高位泥炭沼泽相区别。在日本关东、中部地方以南的平原有小面积的零散分布。在高地或高纬度寒冷气候条件下，随着泥炭的堆积脱离地下水的影响，可很快地向高位泥炭沼泽过渡。

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