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晚稻根际土壤特性对CH4和N2O排放的影响
引用本文:傅志强,朱华武,陈灿,黄璜. 晚稻根际土壤特性对CH4和N2O排放的影响[J]. 热带作物学报, 2012, 33(1): 5-10
作者姓名:傅志强  朱华武  陈灿  黄璜
作者单位:1. 湖南农业大学农学院,湖南长沙410128;农业部多熟制作物栽培与耕作学重点开放实验室,湖南长沙410128
2. 湖南农业大学农学院,湖南长沙,410128
基金项目:粮食丰产科技工程项目(No. 2011BAD16B01);国家科技攻关计划项目(No. 2008BAD95B02)和湖南省自然科学基金项目(No. 09JJ5011)。
摘    要:为进一步揭示水稻根际土壤特性对CH4和N2O排放的影响机理,采用静态暗箱/气相色谱法对晚稻不同品种的CH4和N2O排放通量进行了原位观测,并对CH4和N2O排放通量与水稻根际土壤特性的相关性进行了分析。结果表明:不同品种CH4、N2O季平均排放通量间存在差异,变化范围分别为9.27~14.57 mg/(m2·h)、7.16~15.28 μg/(m2·h);CH4排放通量与5 cm处土壤Eh值呈极显著负相关(p<0.01),与pH值呈显著正相关(p<0.05);N2O排放通量与5 cm处土壤Eh呈负相关,但不显著,与pH值呈显著负相关(p<0.05)。CH4排放通量与0~7、7~13、13~20处土壤溶液中CH4浓度均呈显著正相关(p<0.05),N2O排放通量与7~13 cm处N2O浓度呈显著正相关(p<0.05);CH4、N2O排放通量与0~7、7~13、13~20 cm处土壤溶液pH值均呈显著负相关(p<0.05),CH4排放通量与电导率呈极显著正相关(p<0.01),N2O与电导率呈负相关,但不显著。因此,水稻根际土壤Eh、pH、电导率以及CH4浓度是影响CH4排放的重要因素,根际土壤pH与N2O排放密切相关。

关 键 词:水稻;品种;CH4;N2O;排放通量;根际土壤特性

Effects of Late Rice Rhizospheric Soil Characteristics on CH4 and N2O Emission from Paddy Field
FU Zhiqiang,ZHU Huawu,CHEN Can and HUANG Huang. Effects of Late Rice Rhizospheric Soil Characteristics on CH4 and N2O Emission from Paddy Field[J]. Chinese Journal of Tropical Crops, 2012, 33(1): 5-10
Authors:FU Zhiqiang  ZHU Huawu  CHEN Can  HUANG Huang
Affiliation:1,2 1 Agronomy College of Hunan Agricultural University,Changsha,Hunan 410128,China 2 Key Laboratory of Ministry of Agriculture for Multi-cropping Cultivation and Farming System,Changsha,Hunan 410128,China
Abstract:An,one-year field experiment was conducted to measure in situ the greenhouse gases emission fluxes of the late rice cultivars in Hunan double-cropping rice areas and the correlation between the greenhouse gases emission and the characteristics of rice rhizospheric soil was studied to probe the effect of rice rhizospheric soil characteristics on methane and nitrous oxide emission by the method of static opaque chamber / modified gas chromatography.The results showed that the seasonal average emission fluxes of CH4 and N2O were different among rice cultivars,and their variation ranges were from 9.27 to 14.57 mg/(m2/h)and from 7.16 to 15.28 μg/(m2/h),respectively.CH4 emission fluxes were significantly negatively correlated with the Eh of 5cm depth soil(p<0.01),and were significantly positively correlated with the 5cm depth soil pH values(p<0.05).The negative correlation was not significant between N2O emission flux and 5cm soil Eh,however,the significantly negative correlation existed between the N2O emission flux and the pH values of 5cm depth soil(p<0.05).At the late rice growth stages,CH4 emission fluxes were significantly positive correlation with the CH4 contents of 0~7 cm,7~13 cm and 13~20 cm depth soil solution(p<0.05),and the N2O emission fluxes were significantly positive correlation with the N2O content of 7~13 cm depth soil(p<0.05).In addition,there were significantly negative correlation among CH4,N2O emission fluxes and the pH of 0~7 cm,7~13 cm,13~20 cm depth soil(p<0.05),and CH4 emission fluxes were significantly positive correlation with the conductivity of 0~7 cm,7~13 cm,13~20 cm depth soil solution(p<0.01),but the negative correlations were not significant between N2O emission fluxes and the conductivity of soil solution.Therefore,Eh,pH,conductivity and CH4,content of rice rhizosphere soil solution were the key factors that influenced CH4 emission from the paddy soil,and the rhizospheric soil pH was closely related with N2O emission.
Keywords:Rice  Cultivar  CH4  N2O  Emission flux  Rhizospheric soil characteristic
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