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首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >Spatial and temporal variations of grassland soil organic carbon and total nitrogen following grazing exclusion in semiarid Loess Plateau, Northwest China.
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Spatial and temporal variations of grassland soil organic carbon and total nitrogen following grazing exclusion in semiarid Loess Plateau, Northwest China.

机译:西北半干旱黄土高原放牧后草原土壤有机碳和总氮的时空变化

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摘要

Grazing exclusion is an efficient management practice for preventing grassland degradation in semiarid Loess Plateau. However, little information was known about the spatial and temporal variations of soil organic carbon (SOC) and total nitrogen (TN) following grazing exclusion. In this study, grasslands with grazing exclusion for 11 years at 29 different locations were investigated. The results showed that SOC and TN concentrations decreased with increasing of soil depth. SOC and TN concentrations in 0-20 cm layer were 1.4-2.0 times of that in the other layers. The coefficients of variation of SOC and TN concentrations were about 20%, indicating that there was a moderate variation among different locations. The mean SOC and TN densities were 63.36 and 6.62 t ha-1 respectively which were significantly affected by altitude and the mean annual precipitation (MAP) gradients (P<0.001). Grasslands with altitude of 500-2000 m or MAP of 450-570 mm were optimal for SOC and TN sequestrations. Otherwise, the effects of slope position and mean annual temperature on SOC and TN densities were insignificant (P>0.05). To explore temporal variations of SOC and TN, grasslands with different grazing exclusion ages (5, 10, 15, 20, 25, and 30 years) were investigated. SOC and TN concentrations increased by 89-385% and 86-330% respectively along the chronosequence within 30 years. Based on the values of SOC and TN concentrations, the grasslands were divided into two groups, grazing grassland and grazing exclusion grasslands. Within the group of grazing exclusion grasslands, grazing exclusion for 25 and 30 years facilitated the grasslands to accumulate higher SOC and TN than that for 5, 15, and 20 years. To conclude, SOC and TN accumulations of grazing exclusion grassland were depended on attitude, MAP, and grazing exclusion years.
机译:放牧是防止半干旱黄土高原草地退化的有效管理方法。然而,关于放牧后土壤有机碳(SOC)和总氮(TN)的时空变化知之甚少。在这项研究中,调查了在29个不同地点放牧11年的草地。结果表明,随着土壤深度的增加,SOC和TN的含量降低。 0-20 cm层的SOC和TN浓度是其他层的SOC和TN的1.4-2.0倍。 SOC和TN浓度的变化系数约为20%,表明不同位置之间存在中等变化。平均SOC和TN密度分别为63.36和6.62 t ha -1 ,这分别受到海拔高度和年平均降水(MAP)梯度的显着影响(P <0.001)。 SOC和TN隔离的最佳海拔高度为500-2000 m或MAP为450-570 mm的草原。否则,坡位和年平均温度对SOC和TN密度的影响不显着(P> 0.05)。为了探讨SOC和TN的时间变化,研究了不同放牧年龄(5、10、15、20、25和30年)的草地。在30年内,SOC和TN浓度沿时间顺序分别增加了89-385%和86-330%。根据土壤有机碳和总氮的含量,将草地分为放牧草地和放牧草地两大类。在放牧排斥草地组中,放牧排斥25年和30年促进了草地累积SOC和TN高于5年,15年和20年。总之,放牧草地的SOC和TN积累取决于态度,MAP和放牧年限。

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