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生物炭添加和灌溉对温室番茄地土壤反硝化损失的影响
摘要点击 2731  全文点击 1224  投稿时间:2016-03-23  修订日期:2016-05-17
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中文关键词  生物质炭  灌溉  反硝化  N2O排放  累积排放量
英文关键词  biochar  irrigation  denitrification  N2O emission  accumulative emissions
作者单位E-mail
张文娟 河海大学水利水电学院, 南方地区高效灌排与农业水土环境教育部重点实验室, 南京 210098 1623562107@qq.com 
佘冬立 河海大学水利水电学院, 南方地区高效灌排与农业水土环境教育部重点实验室, 南京 210098
中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室, 南京 210008 
shedongli@hhu.edu.cn 
Gamareldawla H. D. Agbna 河海大学水利水电学院, 南方地区高效灌排与农业水土环境教育部重点实验室, 南京 210098  
夏永秋 中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室, 南京 210008 yqxia@issas.ac.cn 
中文摘要
      生物炭添加和灌溉是番茄地常用的田间管理措施,然而其对反硝化的影响还不清楚. 本研究种植试验设置3个灌溉量水平分别为估算作物生育期需水量ET0的50%(W50%)、75%(W75%)、100%(W100%)和3个生物炭添加水平分别为B0(折合纯碳,0)、B25(折合纯碳,25t·hm-2)、B50(折合纯碳,50t·hm-2),在 2014 年和2015 年番茄收获后,每个试验小区采集具有代表性的土样进行室内培养试验,采用乙炔抑制法来研究土壤的反硝化损失和不加乙炔研究N2O的排放量. 结果表明生物炭和灌溉量显著改变了土壤的理化性质. 与 B0 相比,添加生物炭能够提高土壤全碳、全氮含量和pH 值,降低铵态氮、硝态氮含量,而灌水量降低了土壤中全氮和全碳的含量. 因此,与B0/W50%相比,B25/W75%和B50/W100%处理显著减少了反硝化损失量(P<0.05). 生物炭和灌溉量的交互作用对土壤无机氮含量和反硝化损失的影响均达到显著水平(P<0.05),且对硝态氮的影响表现为灌溉量 >生物炭添加量 >两者交互作用,对铵态氮的影响表现为生物炭添加量 >灌溉量 >两者交互作用,对反硝化损失的影响表现为灌溉量 >生物炭添加量 >两者交互作用. 反硝化损失量与土壤中无机氮含量、(CO2-C)矿化量与N2O排放量均呈正相关关系. 不同生物炭添加量和灌溉量处理后明显影响了N2O/DNP<0.05),培养结束时,各处理下的N2O累积排放量/DN累积排放量差异较大,介于0.31%~1.88%.
英文摘要
      Biochar addition and irrigation are normal farm practices for tomatoes management, while their impacts on denitrification are less known. In this study, three irrigation treatments(hereafter main plots)were set as 50% (W50%), 75% (W75%) and 100% (W100%) of reference evapotranspiration (ET0), and the subplots coupled three biochar treatments at the rates of 0 (B0), 25 t·hm-2 (B25) and 50 t·hm-2 (B50). Typical soil samples in each plot were collected when tomatoes were harvested in 2014 and 2015. We used acetylene inhibition method to study the denitrification loss, and also measured N2O emissions of tomato soil without acetylene amendment. The results showed that biochar and irrigation significantly changed the physical and chemical properties of the soil. Adding biochar improved total carbon, total nitrogen content and pH of the soil, while reduced the content of NH4+-N and NO3--N compared to B0. On the contrary, irrigation reduced the amount of total nitrogen and total carbon content. As a result, both biochar and irrigation significantly reduced denitrification losses (P<0.05). Moreover, the interaction of biochar and irrigation significantly reduced soil inorganic nitrogen and denitrification losses (P<0.05),and the orders of the influencing factors of NO3--N were irrigation, biochar, their interactions in turn, the orders of the influencing factors of NH4+-N were biochar, irrigation, their interactions in turn, the orders of the influencing factors of denitrification losses were irrigation, biochar, their interactions in turn. Denitrification losses were positively related to inorganic nitrogen content in the soil, CO2mineralization rates and N2O emission rates. The ratio of N2O/DN, ranging from 0.31% to 1.88%, was significantly affected by biochar and irrigation treatment in the fields (P<0.05).

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