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宁夏天然草地土壤有机碳分布格局及驱动因素

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[目的]草地作为重要的土壤碳库,探究其有机碳的分布格局及影响因素对缓解温室效应、草地生态系统评价以及退化草地生态恢复具有重要意义。[方法]以宁夏3种类型天然草地(草甸草原、典型草原、荒漠草原)为研究对象,在195个样地测定0~20 cm和20~40 cm土层土壤有机碳(Soil Or-ganic Carbon,SOC)含量,利用分段结构方程模型(Segmented structural equation model)揭示土壤SOC含量与地理、气候、植被、和土壤因子的关系。[结果]在水平方向上0~20 cm和20~40 cm土层SOC平均含量分别为9。46和8。25 g/kg,草甸草原>典型草原>荒漠草原;在垂直剖面上SOC平均含量随土层深度增加而减少;由南到北呈递减的变化趋势。分段结构方程表明:在0~20和20~40 cm土层中SOC含量与TN、TP和丰富度指数呈极显著正相关(P<0。01),与pH值和年均温(MAT)呈极显著负相关(P<0。01),与年降水量(MAP)没有显著关系。0~20 cm土层中,总效应由大到小依次为:气候因子(0。38)>土壤因子(0。21)>丰富度指数(0。12)。20-40 cm土层中,总效应由大到小依次为土壤因子(0。39)>气候因子(0。23)>丰富度指数(0。13)。[结论]分段结构方程结果显示雨热条件是影响表层土壤SOC含量的主要因子,TN和TP是影响深层土壤SOC含量的主要因子。
Distribution pattern and driving factors of soil organic carbon of natural grassland in Ningxia
[Objective]Grassland is an important soil carbon pool. It is important to investigate the distribution pattern and influencing factors of organic carbon in grasslands in order to mitigate the greenhouse effect. The investi-gation is also of great significance in grassland ecosystem evaluation and ecological restoration of degraded grasslands.[Method]In this paper,three natural grassland types (meadow steppe,typical steppe and desert steppe) in Ningxia were taken as the research object.Soil organic carbon (SOC) in 0~20 cm and 20~40 cm soil layers was measured in 195 sample plots. The Composite structural equation model was used to reveal the relationship between soil organic carbon content and geography,climate,vegetation and soil factors.[Result]The results showed that in the horizontal direction,the average SOC content of natural grassland in 0~20 cm and 20~40 cm soil layers was 9.46 g/kg and 8.25 g/kg,respectively,with the order of meadow grassland>typical grassland>desert grassland. In the vertical section,SOC decreased with the increased of soil depth. There was a decreased trend from south to north. The seg-mental structural equation showed that in 0~20 cm and 20~40 cm soil layers,SOC content was positively correlated with TN,TP,and Margalef richness indices (P<0.01),and negatively correlated with pH and MAT (P<0.01),but had no significant relationship with MAP.In 0~20 cm soil layer,the total effect was in the order of climate factor (0.38)>soil factor (0.21)>Margale index (0.12). In the 20~40 cm soil layer,the total effect was in the order of soil factor (0.39)>climate factor (0.23)>Margale index (0.13).[Conclusion]The results of the fractional struc-tural equation showed that rain and heat conditions were the main factors affecting the SOC content of the surface soil.TN and TP were the main factors affecting the SOC content of the deep soil.

Ningxia natural grasslandsoil organic carbonenvironmental factorsstructural equation model

李旭梅、杨钧、李小伟、周亮、黄文广、杨君珑

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宁夏大学农学院,宁夏 银川 750021

宁夏草原工作站,宁夏 银川 750021

宁夏天然草地 有机碳 环境因子 结构方程模型

2024

草原与草坪
中国草学会 甘肃农业大学

草原与草坪

CSTPCD
影响因子:0.686
ISSN:1009-5500
年,卷(期):2024.44(4)