详细信息
若尔盖地区主要覆被类型浅层土壤持水量和有机碳关系研究 被引量:4
Study on the Relationship Between Water Holding Capacity and Organic Carbon in Shallow Soil of Main Plant Cover Types in the Zoige Region
文献类型:期刊文献
中文题名:若尔盖地区主要覆被类型浅层土壤持水量和有机碳关系研究
英文题名:Study on the Relationship Between Water Holding Capacity and Organic Carbon in Shallow Soil of Main Plant Cover Types in the Zoige Region
作者:付琳玉[1,2] 孙永玉[1,3] 胥汝宇[1] 刘文斗[1] 廖声熙[1] 唐国勇[1,3,4]
第一作者:付琳玉
机构:[1]中国林业科学研究院高原林业研究所,云南昆明650233;[2]南京林业大学,江苏南京210037;[3]国家林业局云南元谋荒漠生态系统定位观测站,云南昆明650233;[4]国家林业局云南建水荒漠生态系统定位观测站,北京100083
年份:2022
卷号:30
期号:4
起止页码:818-824
中文期刊名:草地学报
外文期刊名:Acta Agrestia Sinica
收录:CSTPCD;;北大核心:【北大核心2020】;CSCD:【CSCD2021_2022】;
基金:中央级公益性科研院所基本科研业务费专项资金(CAFYBB2020ZA004);国家自然科学基金(31670613)资助。
语种:中文
中文关键词:若尔盖地区;土壤持水量;土壤有机碳;拟合曲线斜率
外文关键词:Zoige Region;Soil water holding capacity;Soil organic carbon;Slope of curve fitting
分类号:S182.2
摘要:为探究若尔盖地区浅层土壤持水量和有机碳关系,以若尔盖地区主要覆被类型(沼泽化草甸、非沼泽化草甸和天然林地)浅层(0~20 cm)土壤为研究对象,分析其有机碳和水分特征,探究土壤有机碳含量和最大持水量关系。结果表明:3种覆被类型浅层土壤总孔隙度、最大持水量和有机碳含量均存在明显差异,其中,沼泽化草甸土壤最大持水量最高(2592.46 g·kg^(-1)),是非沼泽化草甸和天然林地的4.0和1.9倍;沼泽化草甸土壤有机碳含量(416.11 g·kg^(-1))约为非沼泽化草甸和天然林地的4.2和2.7倍;若尔盖地区浅层土壤最大持水量与有机碳含量呈极显著正相关关系(R^(2)=0.92,P<0.01),每一种覆被类型土壤水碳也均呈极显著正相关关系;3种覆被类型浅层土壤水碳拟合曲线斜率范围为4.11~7.43,天然林地最大,依次为非沼泽化草甸和沼泽化草甸。研究揭示该地区天然林地土壤最大持水量对有机碳含量变化最敏感,沼泽化草甸土壤水碳关系相对稳定。研究结果对科学判断全球变化背景下区域碳水功能评估提供数据基础。
In order to explore that relationship between water holding capacity and organic carbon of shallow soil in the Zoige region,in this study,the shallow soils(0~20 cm)of main plant cover types(swamp meadow,non-swamped meadow and natural forest)in the Zoige Region were collected and analyzed the characteristics of organic carbon and water moisture to explore the relationships between soil organic carbon content and maximum water holding capacity.The results showed that:there were obvious differences in total porosity,maximum water holding capacity and organic carbon content of shallow soil among the three cover types.Among them,the maximum water holding capacity of swamped meadow soil was the highest(2592.46 g·kg^(-1)),which was 4.0 and 1.9 times that of non-swamped meadow and natural forest.The content of soil organic carbon in swamped meadow(416.11 g·kg^(-1))was about 4.2 and 2.7 times that of in non-swamped meadow and natural forest.There was a very significant positive correlation between the maximum water holding capacity of shallow soil and organic carbon content in the Zoige region(R^(2)=0.92,P<0.01),while there was also a very significant positive correlation between soil water and carbon of each plant cover type.The slope of fitting curve of water and carbon in shallow soil of three types of cover ranges from 4.11 to 7.43,and the natural forest land is the largest,followed by non-swamped meadow and swamped meadow.The study revealed that the maximum water holding capacity of natural forest soil in this area is the most sensitive to change of organic carbon content,and the relationship between water and carbon in swamped meadow soil is relatively stable.The results provide data basis for scientific judgment of regional carbohydrate functional evaluation under the background of global change.
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