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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
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2. 对照和增温处理下南亚热带森林每个土层的土壤不同形态磷(P)含量(平均值+标准误, n = 3)。Al-Pi, 无机铝磷; Al-Po, 有机铝磷; Ca-Pi, 无机钙磷; Fe-Pi, 无机铁磷; Fe-Po, 有机铁磷; NH4Cl-Pi, NH4Cl提取态磷; O-Pi, 无机闭蓄态磷; O-Po, 有机闭蓄态磷; Pi, 总无机磷; Po, 总有机磷; Pt, 总磷。不同小写字母表示不同处理间差异显著(p < 0.05)。

Fig. 2. Concentrations of different soil phosphorus (P) fractions of three soil layers under control and warming treatments in south subtropical forests (mean + SE, n = 3). Al-Pi, inorganic P associated with aluminum; Al-Po, organic P associated with aluminum; Ca-Pi, inorganic P associated with calcium; Fe-Pi, inorganic P associated with iron; Fe-Po, organic P associated with iron; NH4Cl-Pi, NH4Cl extracted P; O-Pi, inorganic occluded P; O-Po, organic occluded P; Pi, total inorganic P; Po, total organic P; Pt, total P. Different lowercase letters indicate significant differences between different treatments (p < 0.05)