大兴安岭多年冻土泥炭地无机氮动态对秋季冻融的响应
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焦亚青 1,2( ), 宋立全 1,2( ), 臧淑英 1,2( ), 孙超峰 1,2, 鲁博权 1,2
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Response of inorganic nitrogen dynamics to autumn freeze-thaw in permafrost peatlands of the Greater Higgnan Mountains
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Yaqing JIAO 1,2( ), Liquan SONG 1,2( ), Shuying ZANG 1,2( ), Chaofeng SUN 1,2, Boquan LU 1,2
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图1. 秋季冻融期3种泥炭地浅层、深层土壤温度变化(XY:小叶章泥炭地;XA:兴安落叶松-泥炭藓泥炭地;BM:白毛羊胡子苔草泥炭地)
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Fig.1. Variations of soil temperature in shallow and deep layers of three permafrost peatlands during the autumn freeze-thaw period(XY: Calamagrostis angustifolia peatland; XA: Larix gmelina-Sphagnum peatland; BM: Eriophorum vaginatum peatland)
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