Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtse River), Ministry of Agriculture, College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China.
Arch Environ Contam Toxicol. 2013 Aug;65(2):183-92. doi: 10.1007/s00244-013-9903-7. Epub 2013 Apr 23.
To investigate the influence of crop residues decomposition on nitrous oxide (N2O) emission, a field study was performed with application of crop residues with different C:N ratios in a bare yellow brown soil at the experimental station of Zhangjiachong at Zigui, China. We set up six experimental treatments: no crop residue (CK), rapeseed cake (RC), potato stalk (PS), rice straw (RS), wheat straw (WS), and corn straw (CS). The carbon (C) to nitrogen (N) ratios of these crop residues were 7.5, 32.9, 40.4, 65.7, and 90.9, respectively. Nitrous oxide fluxes were measured using a static closed chamber method. N2O emissions were significantly enhanced by incorporation of crop residues. Cumulative N2O emissions negatively correlated with C:N ratio (R (2) = 0.9821) of the crop residue, but they were positively correlated with average concentrations of dissolved organic carbon and microbial biomass carbon. Nitrogen emission fraction, calculated as N2O-N emissions originated from the crop residues N, positively correlated with C:N ratio of the residues (P < 0.05). Soil temperature did, whereas soil moisture did not, control the residue's induced N2O emissions because a significant correlation (P < 0.01) existed between soil temperature and N2O emissions in all treatments except the control. In contrast, a significant relationship between soil moisture and N2O emissions was found in the control only. Furthermore, N2O emission significantly correlated (P < 0.05) with NO3 (-)-N, and NH4 (+)-N contents from all residue treatments. These results indicate that (1) crop residues with distinct carbon and nitrogen contents can significantly alter soil N2O flux rates; and (2) soil biotic as well as abiotic variables are critical in determining soil-atmospheric N2O emissions after crop residue incorporation into soil.
为了研究作物残体分解对氧化亚氮(N2O)排放的影响,在中国秭归县张家冲实验站的黄棕壤上,采用不同 C:N 比的作物残体进行了田间研究。我们设置了 6 个实验处理:无作物残体(CK)、菜籽饼(RC)、马铃薯茎(PS)、稻草(RS)、麦草(WS)和玉米秸秆(CS)。这些作物残体的碳(C)氮(N)比分别为 7.5、32.9、40.4、65.7 和 90.9。采用静态封闭室法测量氧化亚氮通量。结果表明,添加作物残体显著增加了 N2O 的排放。N2O 排放的累积量与作物残体的 C:N 比呈显著负相关(R²=0.9821),但与溶解有机碳和微生物生物量碳的平均浓度呈显著正相关。从作物残体 N 中产生的 N2O-N 排放氮素排放分数与残体的 C:N 比呈显著正相关(P<0.05)。土壤温度(P<0.01)而不是土壤湿度(P>0.05)控制着残体诱导的 N2O 排放,因为除对照处理外,所有处理的土壤温度与 N2O 排放之间均存在显著相关性。相比之下,仅在对照处理中发现了土壤湿度与 N2O 排放之间的显著关系。此外,所有残体处理的 N2O 排放与 NO3(-)-N 和 NH4(+)-N 含量均呈显著相关(P<0.05)。这些结果表明:(1)具有明显碳氮含量的作物残体可显著改变土壤 N2O 通量速率;(2)土壤生物和非生物因素在残体施入土壤后决定土壤-大气 N2O 排放方面至关重要。