生物炭对岩溶区黄龙病脐橙园土壤N2O排放的影响
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引用本文:岳鹏鹏,付灿,江晓雨,王蓉,黄雅丹.2022.生物炭对岩溶区黄龙病脐橙园土壤N2O排放的影响[J].地球学报,43(4):502-508.
DOI:10.3975/cagsb.2021.121601
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作者单位E-mail
岳鹏鹏 长江大学资源与环境学院 yue_pengpeng@163.com 
付灿 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
江晓雨 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室
北京大学地球与空间科学学院 
 
王蓉 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
黄雅丹 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室
冰岛大学地球科学学院 
2376393446@163.com 
基金项目:国家自然科学基金项目(编号: U20A2092; 42002106);中央级公益性科研院所基本科研业务费专项(编号: KK2005);中国地质调查局地质调查项目(编号: DD20190816; DD20190606)
中文摘要:岩溶区黄龙病柑橘园土壤氮转化存在特殊性。土壤改良剂生物炭对岩溶区黄龙病柑橘园土壤N2O排放的影响及其微生物调节途径目前尚不清楚。本文通过室内培育试验研究了生物炭添加对岩溶区黄龙病脐橙园土壤N2O排放、土壤氮素净硝化率/矿化率、硝化和反硝化功能基因的影响及其相互关系。结果表明, 添加生物炭改变了土壤氮素净硝化率/矿化率、反硝化相关功能基因nosZ和硝化相关功能基因AOA-amoA、AOB-amoA的丰度, 添加量为2%时是多数指标增长的峰值, 与对照差异显著。添加生物炭降低了岩溶区脐橙园土壤N2O的平均排放速率和累积排放量, 但各处理间差异不显著。DCA排序显示生物炭添加不同处理N2O的排放速率主要受NH+ 4-N含量、nirK丰度、nosZ丰度的负向影响, NO– 3-N含量和AOA-amoA丰度的正向影响。若要进一步提升生物炭对该土壤的减排效果, 应注意提升土壤NH+ 4-N水平和反硝化相关功能基因丰度, 抑制土壤NO– 3-N水平和硝化相关功能基因AOA-amoA的丰度。本研究结果可为岩溶区黄龙病柑橘园土壤N2O减排及调节机制研究提供借鉴。
中文关键词:生物炭  N2O排放  岩溶区土壤  柑橘黄龙病  脐橙园
 
Hydrochemical Characteristics and Genesis of Deep Brines in Wangchang Area, Qianjiang Depression, Jianghan Basin
Abstract:Soil nitrogen transformation of the Huanglongbing citrus orchard in the karst area has a particularity. The effects of soil amendment biochar on soil N2O emissions from the Huanglongbing citrus orchards in the karst areas and the microbial regulation pathways are currently unclear. In this study, the effects of biochar addition on soil N2O emissions, soil nitrogen net nitrification rates / mineralization rates, nitrification, and denitrification functional gene expression and their relationships were analyzed through cultivation experiments. The results showed that the addition of biochar altered the net nitrification rates / mineralization rates of soil nitrogen, abundance of denitrification-related functional genes nosZ, and nitrification-related functional genes AOA-amoA and AOB-amoA. When 2% biochar was added, it was the peak of most indicators, which was significantly different from the control. The addition of biochar reduced the average emission rates and cumulative emissions of N2O from the soil of the navel orange orchard in the karst area, but the differences among treatments were not significant. The DCA ordination test results showed that the N2O emission rates of different biochar addition treatments were mainly affected by the negative effects of NH+ 4-N content, nirK abundance, and nosZ abundance and the positive effects of NO– 3-N content and AOA-amoA abundance. To improve the effects of biochar on reducing soil N2O in the future, attention should be paid to increasing soil NH+ 4-N levels and the abundance of denitrification-related functional genes, while suppressing soil NO– 3-N levels and the abundance of nitrification-related functional genes, AOA-amoA. The results of this study provide a reference and support for the study of soil N2O emission reduction and mainatinence of the Huanglong citrus orchards in karst areas.
keywords:biochar  N2O emissions  soil in karst area  citrus Huanglongbing  navel orange orchard
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