首页|川西北高寒草甸土壤理化性质对土壤呼吸速率影响研究

川西北高寒草甸土壤理化性质对土壤呼吸速率影响研究

扫码查看
通过采样探讨了土壤理化性质对川西北高寒草甸土壤呼吸速率的影响.结果表明,在选取的研究区域内,有机碳、全氮、C/N、全磷、容重对浅丘山地灌丛的土壤呼吸速率影响最大,相关系数为0.5 ~0.8,均达到极显著相关;有机碳、全氮、C/N、全磷、容重、体积含水量及pH与浅丘山地草甸土壤呼吸速率间的相关系数非常小,均对浅丘山地草甸CO2的释放没有影响;有机碳、全氮、C/N、容重、体积含水量、pH对丘前阶地草甸的影响最大,相关系数也为0.5 ~0.8,P<0.01.整体上,浅丘山地灌丛剖面土壤理化性质对土壤呼吸速率的影响呈现出连续性和深层性;丘前阶地草甸则呈现出间断性和表层性;并且土壤理化性质对土壤呼吸速率的影响是浅丘山地灌丛大于丘前阶地草甸.
Influence of Soil Physical and Chemical Properties on Soil Respiration Rate of Alpine Meadow in the Northwestern Plateau of Sichuan Province
In this paper, we discussed the effects of soil physical and chemical properties on soil respiration rate of alpine meadow in the Northwestern Plateau of Sichuan Province by sampling. The results indicated that among all soil physical and chemical properties, the impacts of soil organic carbon, total nitrogen, C/N, total P and bulk density on upland shrub meadow' s(US) soil respirtian rate were important, and correlation coefficient is 0.5 ~0. %,P <0.01. The correlation coefficient of upland meadow's( UM) soil respirtian rate with soil organic carbon, total nitrogen, C/N, total P, bulk density, volume water content, and pH was very small, showing that these factors had no influence on UM' s CO2 emission. The efflux of CO2 in terrace meadow (TM) was correlated with the content of soil organic carbon, total nitrogen, C/N, bulk density, volume water, pH, and r = 0. 5 ~0. 8 ,P <0. 01. In a whole, the impact of vertical soil physical and chemical properties on soil respiration rate in US showed continuity and much more influence of deep properties. But the impact on TM showed discontinuity and much more influence of surface properties. Furthermore, the effect of soil physical and chemical properties on soil respiration rate was stronger in US than in TM.

alpine meadowsoil respirationsoil physical and chemical properties

徐洪灵、张宏、张伟

展开 >

四川城市职业学院公共服务系,四川成都610110

四川师范大学地理与资源科学学院,四川成都610101

高寒草甸 土壤呼吸 土壤理化性质

四川省教育厅自然科学重点基金

2006A071

2012

四川师范大学学报(自然科学版)
四川师范大学(中国 成都)

四川师范大学学报(自然科学版)

CSTPCDCSCD北大核心
影响因子:0.494
ISSN:1001-8395
年,卷(期):2012.35(6)
  • 18
  • 19