增温对南亚热带森林土壤磷形态的影响及其对有效磷的贡献

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蒋芬¹^,²^,³, 黄娟¹^,², 褚国伟¹^,², 程严¹^,²^,³, 刘旭军¹^,²^,³, 刘菊秀¹^,², 列志旸¹^,²^,³^,^*(

)

Effects of warming on soil phosphorus fractions and their contributions to available phosphorus in south subtropical forests

JIANG Fen¹^,²^,³, HUANG Juan¹^,², CHU Guo-Wei¹^,², CHENG Yan¹^,²^,³, LIU Xu-Jun¹^,²^,³, LIU Ju-Xiu¹^,², LIE Zhi-Yang¹^,²^,³^,^*(

)

图1. 对照和增温处理下南亚热带森林不同土层的土壤温度和含水量(平均值+标准误, n = 3)。不同小写字母表示同一土层不同处理间差异显著(p < 0.05)。

Fig. 1. Soil temperature and water content of different soil layers under control and warming treatments in south subtropical forests (mean + SE, n = 3). Different lowercase letters indicate significant differences between different treatments (p < 0.05).