Ding Wei-xin, Meng Lei, Cai Zu-cong, Han Feng-xiang
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.
J Environ Sci (China). 2007;19(2):185-93. doi: 10.1016/s1001-0742(07)60030-8.
To understand the effects of long-term amendment of organic manure and N fertilizer on N2O emission in the North China Plain, a laboratory incubation at different temperatures and soil moistures were carried out using soils treated with organic manure (OM), half organic manure plus half fertilizer N (HOM), fertilizer NPK (NPK), fertilizer NP (NP), fertilizer NK (NK), fertilizer PK (NK) and control (CK) since 1989. Cumulative N2O emission in OM soil during the 17 d incubation period was slightly higher than in NPK soil under optimum nitrification conditions (25 degrees C and 60% water-filled pore space, WFPS), but more than twice under the optimum denitrification conditions (35 degrees C and 90% WFPS). N2O produced by denitrification was 2.1-2.3 times greater than that by nitrification in OM and HOM soils, but only 1.5 times greater in NPK and NP soils. These results implied that the long-term amendment of organic manure could significantly increase the N2O emission via denitrification in OM soil as compared to NPK soil. This is quite different from field measurement between OM soil and NPK soil. Substantial inhibition of the formation of anaerobic environment for denitrification in field might result in no marked difference in N2O emission between OM and NPK soils. This is due in part to more rapid oxygen diffusion in coarse textured soils than consumption by aerobic microbes until WFPS was 75% and to low easily decomposed organic C of organic manure. This finding suggested that addition of organic manure in the tested sandy loam might be a good management option since it seldom caused a burst of N2O emission but sequestered atmospheric C and maintained efficiently applied N in soil.
为了解长期施用有机肥和氮肥对华北平原氧化亚氮排放的影响,自1989年起,利用经有机肥(OM)、半量有机肥加半量化肥氮(HOM)、化肥氮磷钾(NPK)、化肥氮磷(NP)、化肥氮钾(NK)、化肥磷钾(PK)处理的土壤以及对照土壤(CK),在不同温度和土壤湿度条件下进行了实验室培养试验。在最佳硝化条件(25℃和60%的充水孔隙率,WFPS)下,OM土壤在17天培养期内的氧化亚氮累积排放量略高于NPK土壤,但在最佳反硝化条件(35℃和90%的WFPS)下,前者是后者的两倍多。OM和HOM土壤中反硝化产生的氧化亚氮比硝化产生的氧化亚氮多2.1 - 2.3倍,但在NPK和NP土壤中仅多1.5倍。这些结果表明,与NPK土壤相比,长期施用有机肥可显著增加OM土壤中通过反硝化作用产生的氧化亚氮排放。这与OM土壤和NPK土壤之间的田间测量结果有很大不同。田间反硝化厌氧环境形成的显著抑制可能导致OM和NPK土壤之间的氧化亚氮排放没有明显差异。部分原因是在质地较粗的土壤中,氧气扩散速度比需氧微生物的消耗速度快,直到WFPS达到75%,以及有机肥中易分解有机碳含量较低。这一发现表明,在所测试的砂壤土中添加有机肥可能是一个很好的管理选择,因为它很少导致氧化亚氮排放激增,同时能固存大气中的碳并有效地保持土壤中施用的氮。