Chin J Plan Ecolo ›› 2018, Vol. 42 ›› Issue (3): 337-348.DOI: 10.17521/cjpe.2017.0241
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Yuan-Feng SUN1,2,Hong-Wei WAN1,Yu-Jin ZHAO1,Shi-Ping CHEN1,2,Yong-Fei BAI1,2,*()
Online:
2018-03-20
Published:
2018-03-08
Contact:
Yong-Fei BAI
Supported by:
Yuan-Feng SUN, Hong-Wei WAN, Yu-Jin ZHAO, Shi-Ping CHEN, Yong-Fei BAI. Spatial patterns and drivers of root turnover in grassland ecosystems in China[J]. Chin J Plan Ecolo, 2018, 42(3): 337-348.
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URL: https://www.plant-ecology.com/EN/10.17521/cjpe.2017.0241
Fig. 3 Changes in root turnover rate among grassland types in China. The boxes show the 25% and 75% percentiles, and the lines, hollow dots and solid dots represent the mean, median and outlier (95% confidence interval) values, respectively. Alp, alpine meadow; Ave, average value; Des, desert steppe; Mea, meadow steppe; Typ, typical steppe; Wtt, warm-temperate tussock;.
Fig. 4 Root turnover rate for different grassland types (mean + SE). Different lower-case letters indicate significant differences among grassland types (p < 0.05). Alp, alpine meadow; Des, desert steppe; Mea, meadow steppe; Typ, typical steppe; Wtt, warm-temperate tussock.
草地类型 Grassland type | 样本数 N | 平均值 Mean | 标准误差 SE |
---|---|---|---|
高寒草甸 Alpine meadow | 47 | 0.428 | 0.022 |
荒漠草原 Desert steppe | 14 | 0.360 | 0.063 |
草甸草原 Meadow steppe | 29 | 0.387 | 0.030 |
典型草原 Typical steppe | 57 | 0.246 | 0.019 |
热性草丛 Warm-temperate tussock | 7 | 0.782 | 0.077 |
Table 1 Statistics of root turnover rate in different grassland types
草地类型 Grassland type | 样本数 N | 平均值 Mean | 标准误差 SE |
---|---|---|---|
高寒草甸 Alpine meadow | 47 | 0.428 | 0.022 |
荒漠草原 Desert steppe | 14 | 0.360 | 0.063 |
草甸草原 Meadow steppe | 29 | 0.387 | 0.030 |
典型草原 Typical steppe | 57 | 0.246 | 0.019 |
热性草丛 Warm-temperate tussock | 7 | 0.782 | 0.077 |
气候因子 Climatic factor | 土壤理化性质 Soil properties | |||||
---|---|---|---|---|---|---|
MAT | MAP | Gravel | BD | pH | CEC | |
MAP | 0.50*** | |||||
Gravel | 0.09 | 0.46*** | ||||
BD | 0.01 | -0.13 | -0.16 | |||
pH | 0.04 | -0.12 | -0.31*** | -0.17* | ||
CEC | 0.14 | 0.35*** | 0.11 | -0.76*** | 0.11 | |
RTR | 0.45*** | 0.46*** | 0.39*** | -0.33*** | -0.18* | 0.30*** |
Table 2 Correlation coefficients of the root turnover rate with climatic factors and soil properties
气候因子 Climatic factor | 土壤理化性质 Soil properties | |||||
---|---|---|---|---|---|---|
MAT | MAP | Gravel | BD | pH | CEC | |
MAP | 0.50*** | |||||
Gravel | 0.09 | 0.46*** | ||||
BD | 0.01 | -0.13 | -0.16 | |||
pH | 0.04 | -0.12 | -0.31*** | -0.17* | ||
CEC | 0.14 | 0.35*** | 0.11 | -0.76*** | 0.11 | |
RTR | 0.45*** | 0.46*** | 0.39*** | -0.33*** | -0.18* | 0.30*** |
Fig. 9 The relative contributions of climatic variables and soil properties to root turnover rate. BD, bulk density (g.cm-3); MAT, mean annual temperature (℃); MAP, mean annual precipitation (mm); Gravel, gravel content (% vol.); pH, pH value.
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