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国家自然科学基金(31070399)

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Effect of Long-Term Fertilization on Soil Enzyme Activities Under Different Hydrothermal Conditions in Northeast China被引量:13
2011年
Human activities have altered weather patterns by causing an increase in greenhouse gas. The effects of climate change have been studied, including effects on some ecosystems throughout the world. There are many studies on changes in the soil due to climate change, but much of them did not extend their research to soil enzyme that integrates information on soil microbial status and soil physical-chemical conditions. Meanwhile, there are lots of experimental fields established to study effects of long-term fertilization on soil enzyme activities, but many did not compare the difference of soil enzyme activities and did not analyze the effect of climatic factors on soil enzyme activities with long-term fertilization under different hydrothermal conditions. In this study, we compared soil enzyme activities of three long-fertilization stations which had different hydrothermal conditions in Northeast China, and analyzed the relationship of hydrothermal condition, soil chemical properties with soil enzyme activities. Hydrothermal conditions (annual temperature and total rainfall) decreased in order of Gongzhuling (Jilin Province, China ) Harbin (Heilongjiang Province, China) Heihe (Heilongjiang Province, China) over the course of the long-term fertilization experiment. Sunshine hours showed the longest in Gongzhuling, the second in Heihe, and the last in Harbin. However, the order of soil enzymes was not in agreement with hydrothermal conditions. Overall, the order of soil enzymes for the same treatment among three stations was consistent in 2008 with in 2009. Correlation analysis demonstrated that different soil enzymes achieved the different affected levels by climatic factors under different fertilization treatments. Urease activity showed a significant relationship with sunshine hours in no fertilizer (CK) treatment (R=-0.91, P0.01) and relative humidity in mineral fertilizers plus manure (MNPK) treatment (R=0.82, P0.05). Phosphatase activity exhibited a negative correlation with ann
JIAO Xiao-guangGAO Chong-shengLU Guo-hongSUI Yu-yu
黑土农田土壤有机碳演变研究进展被引量:32
2011年
在我国,由于国家粮食安全的需要,关注黑土、研究黑土的人越来越多,尤其是黑土可持续利用及其与环境的关系已成为当今研究的热点问题。黑土研究领域中最活跃的部分是黑土农田土壤有机质(碳)的研究。基于此,本文依据有关文献资料,简述了我国黑土的分布、黑土开垦历史、农田土壤有机碳的演变及其在农业上的贡献,系统分析了国内外农田土壤碳研究的方法及其进展,指出了开展我国黑土农田土壤碳演变及其预测研究的现实意义及其潜在价值,建议未来应侧重黑土农田土壤有机碳的变化与调控方面的研究,即在黑土农田土壤有机碳的定向培育技术、指标体系和量化表征评估方法、预测模型等方面有所突破,最终形成黑土农田土壤有机碳保护和利用的理论和方法。
高崇升王建国
关键词:黑土土壤有机碳土壤有机质
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