By analyzing the characteristic of urban agglomeration areas, proposing that considering the mobility of resource is essential in researching carrying capacity, the research used core cities of Central Henan urban agglomeration as cases to study, referencing press-state-response model to build the target system of carrying capacity, considering resource supply and consumption & environmental pollution and treatment, using AHP method to evaluate. Reliant exponential is used to evaluate the dependence severity. The result shows that according to the comparison of two results considering resource fluidity or not in Zhengzhou in 2004?2014, only considering resource fluidity can reflect the real condition of an area. Core cities of Central Henan urban agglomeration are short of water and energy resources but are enough to use with the supply of external resources. The orders of the carrying capacity index on resource and environment are Luohe, Xuchang, Xinxiang, Zhengzhou, Jiyuan, Jiaozuo, Luoyang, Pingdingshan and Kaifeng. According to the reliant exponential of external resources, grain resources in these nine cities are self-sufficiency. External energy resources are needed in Kaifeng, Xinxiang, etc. External water resources are needed in Zhengzhou, Kaifeng, etc. More external water resources are needed than external water resources.

The authors conducted experiments to simulate warming and alter precipitation since 2011, and investigated soil physical properties (soil particle size and pH) and carbon pools (soil total carbon (STC), soil organic carbon (SOC), soil extractable organic carbon (EOC) and microbial biomass carbon (MBC)) in July 2013. The results showed that warming significantly increased soil temperature and decreased soil moisture at the depths of 0-20 cm, and altered precipitation affected soil moisture at 0-20 cm depth, but had no influence on soil temperature. At the depth of 0-10 cm, warming significantly increased SMBC; increased precipitation significantly reduced EOC content and elevated MBC content; decreased precipitation significantly decreased soil sandy proportion, MBC content and increased soil clay proportion and EOC content. At the depth of 10-20 cm, increased precipitation led a reduction on EOC content. The interactions of warming and altered precipitation on soil indexes were not detected. The pattern of soil properties was changed mainly by altered precipitation, not warming, according to the results of PCA. The results suggest that given precipitation will be continuously increased in the future, increased precipitation may lead a reduction in soil clay proportion and EOC content in the topsoil, and subsequently affect plant primary production and micrbial communities in this region.