新疆北部六种草地类型土壤碳氮磷生态化学计量特征
草地土壤碳氮磷含量及其生态化学计量的空间变异关系到草地生态系统的功能与稳定性。海拔、气候、土壤性质和植被如何影响新疆北部典型牧区额尔齐斯河(简称额河)流域土壤碳氮磷化学计量的空间格局尚不清楚。本文选取了额河流域六种主要草地类型的65个样点(0 ~ 10、10 ~ 20 cm土层)进行研究。结果表明:(1)高寒草甸、山地草甸、温性草甸草原有机碳(39.06 ~ 62.59 g·kg-1)、总氮含量(3.87 ~ 6.95 g·kg-1)以及六种草地类型的土壤总磷含量(0.53 ~ 1.59 g·kg-1)总体上高于中国土壤平均值(24.56 g·kg-1、1.88 g·kg-1、0.56 g·kg-1),而六种草地类型的土壤碳氮比(5.03 ~ 9.97)、碳磷比(7.50 ~ 52.38)以及温性草原、温性荒漠草原和温性荒漠土壤氮磷比(1.53 ~ 3.72)低于中国或全球土壤平均值(11.40、64.30、3.90)。(2)土壤碳氮磷含量以及碳磷比、氮磷比随着海拔升高(328 ~ 2655 m)、降水量增加以及温度降低而显著增加,并且与植被特征、土壤理化性质有显著的相关性。随着海拔的升高,土壤有机碳、总氮含量与土壤碳磷比在土层间的差异逐渐增加。(3)结构方程模型结果表明,海拔与气候因子对土壤碳氮磷含量及其生态化学计量的影响效应最高,海拔通过改变温度、降水、植被特征、土壤理化性质影响土壤碳氮磷含量,最终影响生态化学计量。未来应进一步开展气候变化对土壤碳氮磷及其生态化学计量影响的跨区域尺度研究。
Spatial variations in soil carbon, nitrogen, and phosphorus concentration, as well as their ecological stoichiometry, in grasslands are related to the function and stability of grassland ecosystems. The Irtysh River Basin features a significant disparity in altitude, notable climate variation, and diverse grassland types that display a vertical zonal distribution. However, the influence of altitude, climate, soil properties, and vegetation on the spatial patterns of soil carbon, nitrogen, and phosphorus stoichiometry in the Irtysh River Basin, which is a typical pastoral area in Xinjiang, has not been fully understood. This study investigated 65 sample points from six main grassland types (temperate desert, temperate desert steppe, temperate steppe, temperate meadow steppe, mountain meadow, alpine meadow) in the Irtysh River Basin, at depths of 0-10 cm and 10-20 cm. The results were as follows: (1) The soil organic carbon (39.06-62.59 gkg-1), total nitrogen (3.87-6.95 gkg-1), and total phosphorus concentration (0.53-1.59 gkg-1) of alpine meadow, mountain meadow, and temperate meadow steppe were higher than the average values of Chinese soil (24.56 gkg-11.88 gkg-10.56 gkg-1). However, the soil C : N (5.03-9.97) and C : P ratios (7.50-52.38) of six grassland types were lower than the average values of Chinese or global soil, as well as the soil N: P ratios (1.53-3.72) of temperate steppe, temperate desert steppe, and temperate desert (11.4064.303.90). (2) The concentrations of soil carbon, nitrogen, and phosphorus, as well as C : N and C : P ratios, increased significantly with increasing altitude (328-2655 m), precipitation and decreasing temperature. These parameters also showed significant correlations with soil physicochemical properties and vegetation characteristics. With increasing altitude and precipitation, and decreasing temperature, the differences in soil carbon and nitrogen concentration, and soil C : P ratios gradually increased among soil layers. (3) The results of the structural equation model (SEM) showed that altitude and climate factors had the highest impact on soil carbon, nitrogen, and phosphorus concentration, as well as their ecological stoichiometry. Altitude affected soil carbon, nitrogen, and phosphorus concentration by changing temperature, precipitation, vegetation characteristics, and soil physicochemical properties, ultimately affecting ecological stoichiometry. Future research should further investigate the impact of climate change on soil carbon, nitrogen, and phosphorus concentration, as well as on their ecological stoichiometry, at a regional scale. This paper provides basic data and a theoretical basis for estimating soil nutrient storage, as well as for the protection and utilization of grassland ecosystems in the Irtysh River Basin.
梁元也、范连连、马学喜、惠婷婷、毛洁菲、李耀明
农业科学研究环境科学基础理论自然地理学
Xinjiang Institute of Ecology and GeographyChinese Academy of SciencesXinjiang Urumqi 830011Research Center for Ecology and Environment of Central AsiaChinese Academy of SciencesXinjiang Urumqi 830011University of Chinese Academy of SciencesBeijing 100049
grassland typealtitudetemperaturesoil nutrientsoil ecological stoichiometryIrtysh River Basin
梁元也,范连连,马学喜,惠婷婷,毛洁菲,李耀明.新疆北部六种草地类型土壤碳氮磷生态化学计量特征[EB/OL].(2024-11-12)[2025-08-02].https://chinaxiv.org/abs/202411.00127.点此复制
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