土壤理化特性对稻田CH4排放的影响

为了研究土壤理化特性对稻田CH4 排放的影响 ,室外盆栽试验于 2 0 0 0年水稻生长季在南京农业大学实施 ,1 8个供试水稻土分别取自江苏宜兴、江宁、六合、仪征及宝应等地 .所有供试土壤的季节性CH4 平均排放通量为 6 42± 2 70mg·(m2 ·h) - 1,最低和最高值分别为 1 96mg·(m2 ·h) - 1和 1 1 0 6mg·(m2 ·h) - 1,两者相差约 5 6倍 .单相关分析结果表明 :影响CH4 排放的主要土壤参数为质地、氮素状况及铜含量 .CH4 排放与土壤砂粒含量呈正相关 (r =0 5 2 8,p =0 0 2 4) ,与粘粒含量呈负相关 (r =-0 484,p =0 0 42 ) .氮素含量高的土壤CH4 排放较低 ,CH4 排放与土壤全氮、速效氮和铵态氮含量的线性相关系数分别为 -0 449(p =0 0 62 )、-0 61 1 (p =0 0 0 7)和 -0 649(p =0 0 0 4) .土壤铜含量直接影响CH4 的排放 ,CH4 排放与有效态铜和全铜含量的线性相关系数分别为 -0 5 94(p =0 0 0 9)和 -0 5 47(p =0 0 1 9) .本研究并未观测到CH4 排放与土壤有机碳含量有相关关系 ,这与前人报道的实验室培养测定结果及稻田CH4 排放随土壤有机质含量提高而增加的假设完全不同 .逐步回归分析表明 ,不同土壤间CH4 排放的变异性有 75 5 %可由土壤有效态铜含量、镁 (全量 )含量及有效铁含量与全量铁之

Methane emission from rice paddy soils as influenced by soil physicochemical properties

To identify the key soil parameters influencing methane emission from rice paddies, and to quantitatively describe the relationship of methane emission with the soil properties, an outdoor pot experiment with a total of 18 paddy soils sampled from different regions in Jiangsu province was conducted in Nanjing Agricultural University during 2000 rice growing season. Seasonal average rate of CH4 emission for all the 18 soils was 6.42 +/- 2.70 mg.(m2.h)-1, ranging from 1.96 to 11.06 mg.(m2.h)-1, approximately a 5.6-fold difference between the maximum and the minimum. Correlation analysis indicated that the seasonal average of CH4 emission was positively dependent on soil sand content (r = 0.528, p = 0.024) and negatively on soil clay content (r = -0.484, p = 0.042). Negative correlation of CH4 emission against soil total nitrogen (r = -0.449, p = 0.062), available nitrogen (r = -0.611, p = 0.007) and NH4(+)-N(r = -0.649, p = 0.004) was also observed. Copper content of soils has a significant negative impact on CH4 emission. The correlation coefficient (r) of CH4 emission against soil available copper and with total copper was -0.594 (p = 0.009) and -0.547 (p = 0.019), respectively. No clear relationship existed between CH4 emission and soil carbon content. A further investigation suggests that the seasonal average rate of CH4 emission can be quantitatively determined by a linear combination of soil available copper, total manganese, and a ratio of available to total iron (R2 = 0.755, p = 0.0001).