研究报告
贺冬冬,周维,陈霖,任晓静,莫永亮,朱波,胡荣桂.川中丘陵地区冬水田甲烷排放特征研究[J].环境科学学报,2017,37(6):2281-2287
川中丘陵地区冬水田甲烷排放特征研究
- Characteristics of methane emission from winter flooded paddy field in the hilly area of central Sichuan Province
- 基金项目:国家重点基础研究发展计划(No.2012CB417106);中央高校基本科研业务费专项基金(No.2662016PY098)
- 贺冬冬
- 华中农业大学资源与环境学院, 武汉 430070
- 周维
- 华中农业大学资源与环境学院, 武汉 430070
- 陈霖
- 华中农业大学资源与环境学院, 武汉 430070
- 任晓静
- 华中农业大学资源与环境学院, 武汉 430070
- 莫永亮
- 华中农业大学资源与环境学院, 武汉 430070
- 朱波
- 中国科学院成都山地灾害与环境研究所, 成都 610041
- 胡荣桂
- 华中农业大学资源与环境学院, 武汉 430070
- 摘要:以川中丘陵地区典型冬水田为对象,设置了有水稻常规施肥(RF)、无水稻常规施肥(NP)、有水稻无氮肥(NN)3种处理,以静态暗箱-气相色谱法对甲烷(CH4)排放进行了原位观测.结果表明,RF、NP和NN处理下CH4排放通量分别为-0.0042~18.29、0.03~16.78和0.10~26.76 mg·m-2·h-1,平均排放通量分别为10.22、4.25和14.15 mg·m-2·h-1(以每平方米每小时消耗/产生的C量(mg)计),水稻生长季是主要排放期,但休闲季CH4排放量仍占全年CH4总排放量的14%.没有水稻处理的CH4排放量显著低于有水稻处理(p<0.01);而不施氮肥处理的CH4排放量显著高于施肥处理(p<0.01).CH4排放通量与5 cm深土壤温度呈显著正相关(p<0.01),随着温度的升高,甲烷排放量呈指数增加.CH4排放通量与1~4 cm的稻田水深呈显著负相关(p<0.01),随着水深的增加,甲烷的排放呈指数迅速下降;而与4~8 cm的稻田水深无相关性,甲烷的排放也变化缓慢.由此表明,土壤温度和水深在很大程度上调控着CH4的排放.此外,研究结果也显示将冬水田休闲期改为旱作可减少CH4排放,对环境有利.
- Abstract:This study was conducted to investigate CH4 fluxes and associated environmental factors from a typical winter paddy field in the hilly region of central Sichuan Province. Three treatments were set, i.e. rice-flooded fallow rotation (RF), no plant (NP) and no nitrogen fertilizer (NN). CH4 fluxes were analyzed by the static opaque chamber and gas chromatography techniques. The results showed that CH4 fluxes from treatments of RF, NP and NN varied from -0.0042~18.29, 0.03~16.78 and 0.10~26.76 mg·m-2·h-1, with average fluxes of 10.22, 4.25 and 14.15 mg·m-2·h-1, respectively. The emissions of CH4 mainly occurred in a paddy soil during rice-growing season. However, emissions of CH4 in non-cropping season accounted for 14% of the total annual emissions, which could not be ignored. CH4 emission after treatment of RF was significantly higher than that of NP but lower than that of NN (p<0.01). CH4 emissions were positively correlated with soil temperature at the 5 cm depth (p<0.01) due to the exponential increase of the amount of methane emissions with temperature. CH4 fluxes were negatively related to water depth in 1~4 cm of paddy fields (p<0.01), which suggested that soil temperature and water depth significantly influenced the fluxes of CH4. The study also indicated that wheat cultivation in paddy soils during non-cropping season might be an effective way to reduce the release of CH4, which facilitated decreasing the emission of greenhouse gasses.
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