首页|黄淮海平原不同土地利用方式对土壤有机碳及微生物呼吸的影响

黄淮海平原不同土地利用方式对土壤有机碳及微生物呼吸的影响

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土壤是陆地生态系统最大的碳库,有机碳通过微生物分解作用向大气释放CO2,土壤碳库的微小变化将会对大气CO2浓度和全球碳循环产生巨大的影响.在当前人类活动频繁和土地利用与土地覆被变化的背景下,研究不同土地利用方式对土壤有机碳等理化性质和土壤微生物呼吸等功能的影响,可以阐明影响土壤碳汇功能的关键因子,为未来土地利用管理提供科学依据.以开封市为例,研究了黄淮海平原不同土地利用方式(包括弃耕地、草地、果园、农田和森林)下土壤湿度、pH值、铵态氮、硝态氮、总碳、总氮、有机碳、可溶性有机碳、微生物生物量碳氮、微生物呼吸及其温度敏感性的变化规律.研究结果表明,(1)森林土壤湿度、总碳、总氮、有机碳(1.48%)、微生物生物量碳氮含量显著高于其他土地利用方式,但其微生物呼吸(101.06 mg·kg-1·d-1)和温度敏感性(1.18)最小.(2)农田土壤的总碳、总氮、有机碳、微生物生物量碳氮含量均次于森林且高于其他土地利用方式,微生物呼吸速率较大(128.55 mg·kg-1·d-1).(3)弃耕地、草地和果园土壤碳氮和微生物碳氮较小.(4)结构方程模型表明土地利用方式可以直接解释土壤有机碳积累的68%,且可通过土壤湿度间接地影响土壤有机碳和微生物呼吸.土壤有机碳和微生物呼吸分别被土壤湿度和硝态氮含量等因子解释了93%和54%.该研究表明森林生态系统利于土壤有机碳固持,其较小的微生物呼吸温度敏感性对应对未来全球气候变化具有重大意义;农田占地面积广大,农业经营中在保障粮食生产的同时要采取免耕或秸秆还田等措施充分发挥其碳汇作用.
Effects of Different Land Use Types on Soil Organic Carbon and Microbial Respiration in Huang-Huai-Hai Plain
Soils are the largest carbon pools in terrestrial ecosystems.Soil organic carbon can be decomposed by microorganisms and release CO2 to atmosphere.Minor changes in soil carbon pool will significantly affect atmospheric CO2 concentration and global carbon cycling.Under the current background of frequent human activities and land use/cover changes (LUCC),it is necessary to study the effects of different land use types on soil physico-chemical properties and microbial functions (such as soil organic carbon and microbial respiration) to illuminate the key factors of influence soil carbon sequestration function and provide scientific evidence for future land use management.This study chose Kaifeng as pilot city and measured soil moisture,soil pH,NH4+,NO3-,total carbon,total nitrogen,organic carbon,dissolved organic carbon,microbial biomass carbon,microbial biomass nitrogen,microbial respiration and its temperature sensitivity in different land use types,including old-field,grassland,orchard,farmland,and forest in Huang-Huai-Hai Plain.The results showed that:(1) All soil moisture,total carbon,total nitrogen,organic carbon (1.48%),microbial biomass carbon and nitrogen in forest were significantly higher than that in other land use types.However,microbial respiration (101.06 mg·kg-1·d-1) and its temperature sensitivity (1.18) were minimum.(2) Soil total carbon,total nitrogen,organic carbon,microbial biomass carbon and nitrogen in farmland were lower than that in forest,but higher than that in other land use types.Microbial respiration rate (128.55 mg·kg-1·d-1) was high in farmland.(3) Soil carbon,nitrogen,and microbial carbon and nitrogen contents in old-field,grassland,and orchard were less than forest and farmland.And (4) structural equation model showed that land use type directly explained 68% of soil organic carbon and indirectly influenced soil organic carbon and microbial respiration through soil moisture.Soil organic carbon and microbial respiration were explained 93% and 54%,respectively,by soil moisture and NO3-.The results indicate that forest ecosystem will facilitate soil organic carbon sequestration,and their minor temperature sensitivity of microbial respiration will be of great importance in countermeasure of global climatic change in future.Farmland cover larger area.Carbon sink function should be developed by no-tillage and straw return in agricultural management in the meantime of crop production are protected.

soil physico-chemical propertiesorganic carbon mineralizationcarbon sequestrationland managementstructural equation model

李英、韩红艳、王文娟、杨光菲、赵灿灿

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河南大学生命科学学院,河南开封475004

土壤理化性质 有机碳矿化 碳汇 土地管理 结构方程模型

国家自然科学基金

31640011

2017

生态环境学报
广东省生态环境与土壤研究所 广东省土壤学会

生态环境学报

CSTPCDCSCD北大核心
影响因子:1.608
ISSN:1674-5906
年,卷(期):2017.26(1)
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