排露沟流域不同海拔灌丛土壤碳氮磷化学计量特征
牟文博1, 徐当会1,*(
), 王谢军1, 敬文茂2, 张瑞英1, 顾玉玲1, 姚广前1, 祁世华1, 张龙1, 苟亚飞1
), 王谢军1, 敬文茂2, 张瑞英1, 顾玉玲1, 姚广前1, 祁世华1, 张龙1, 苟亚飞1
Soil carbon, nitrogen, and phosphorus stoichiometry along an altitude gradient in shrublands in Pailugou watershed, China
MOU Wen-Bo1, XU Dang-Hui1,*(), WANG Xie-Jun1, JING Wen-Mao2, ZHANG Rui-Ying1, GU Yu-Ling1, YAO Guang-Qian1, QI Shi-Hua1, ZHANG Long1, GOU Ya-Fei1
), WANG Xie-Jun1, JING Wen-Mao2, ZHANG Rui-Ying1, GU Yu-Ling1, YAO Guang-Qian1, QI Shi-Hua1, ZHANG Long1, GOU Ya-Fei1
图2. 排露沟流域土壤有机碳(SOC)、全氮(TN)、全磷(TP)含量及其化学计量比的相关性。虚线和实线分别代
Fig. 2. Correlations between soil organic carbon (SOC), total nitrogen (TN), total phosphorus (TP) contents and their stoichiometry in Pailugou watershed. Dashed line and solid line represents the nutrient indicator fitting line of 0-10 cm and 10-20 cm, respectively.
