Dipartimento di Biologia, Università degli Studi di Napoli Federico II, Campus MS Angelo, via Cinthia, 80126 Napoli, Italy.
Dipartimento di Agraria, Università degli Studi di Napoli Federico II, via Università 100, 80055 Portici, Italy.
J Environ Manage. 2017 May 1;192:68-78. doi: 10.1016/j.jenvman.2017.01.037. Epub 2017 Jan 28.
Organic fertilization can preserve soil organic matter (SOM) and is foreseen as an effective strategy to reduce green house gases (GHGs) emissions in agriculture. However, its effectiveness needs to be clarified under specific climate, crop management and soil characteristics. A field experiment was carried out in a Mediterranean drip irrigated maize system to assess the pattern of soil CO and NO fluxes in response to the replacement of a typical bare fallow-maize cycle under urea fertilization (130 kg N ha y) (CONV) with: (i) bare fallow-maize cycles under two doses of compost (COM1 and COM2, 130 and 260 kg N ha y, respectively) and (ii) a vetch-maize cycle, with vetch incorporation as green manure (130 kg N ha y) (GMAN). Along the maize period (MP), reduced daily NO emissions were detected in organic treated soils compared to CONV, mainly in the first stages of the cultivation, thanks to the slow release of available nitrogen from the organic substrates. Cumulative NO fluxes (kg NO-N ha) in MP scored to 0.24, 0.14, 0.12 and 0.085 for CONV, COM1, COM2 and GMAN, respectively, with significantly lower emissions in GMAN respect to CONV. CO fluxes partially reflected the ranking observed for maize yields, with cumulated values (Mg CO-C ha) of 2.2, 1.5, 2.1, 2.1 for CONV, COM1, COM2 and GMAN, respectively, and significantly lower in COM1 respect to the other treatments. During the fallow period (FP), compared to CONV (0.77 Mg CO-C ha and 0.25 kg NO-N ha), enhanced GHG fluxes were detected in COM treatments (about 0.90 Mg CO-C ha and 0.37 kg NO-N ha, as averaged values from COM1 and COM2), likely driven by the slow prolonged mineralization of the added organic matter. GMAN showed comparable CO (0.82 Mg CO-C ha) and NO emissions (0.30 kg NO-N ha), in consequence of restrained post-harvest residual N coupled with the counteracting effect of vetch uptake. Respect to the total yearly GHG emissions in CONV (about 194 kg CO eq ha y), the overall results showed commensurate slightly higher GWP in COM treatments (+11% as averaged value from COM1 and COM2). The yield-scaled global warming potential (GWP) resulted 60% higher and nearly doubled for COM2 and COM1 respectively, according to the lower COM yields, markedly dampening at halved compost dose. GMAN appeared the best performing organic treatment, with lower GWP (-27%) and competitive yields respect to CONV. All treatments showed NO emission factors consistently lower compared with the default IPCC 1% value.
有机施肥可以保存土壤有机质(SOM),并被视为减少农业温室气体(GHG)排放的有效策略。然而,其有效性需要在特定的气候、作物管理和土壤特征下加以澄清。在一个地中海滴灌玉米系统中进行了一项田间试验,以评估土壤 CO 和 NO 通量对以下因素的响应模式:(i)在尿素施肥(130kgNha y)下用两种堆肥剂量(COM1 和 COM2,分别为 130 和 260kgNha y)代替典型的休耕-玉米轮作的休耕-玉米轮作,和(ii)作为绿肥的豌豆-玉米轮作,用豌豆作为绿肥(130kgNha y)(GMAN)。在玉米生长期间(MP),与 CONV 相比,有机处理土壤中的每日 NO 排放量减少,主要是在种植的早期,这要归功于有机基质中有效氮的缓慢释放。MP 期间的累积 NO 通量(kgNO-Nha)分别为 CONV、COM1、COM2 和 GMAN 的 0.24、0.14、0.12 和 0.085,GMAN 与 CONV 相比,NO 排放显著减少。CO 通量部分反映了玉米产量的排序,累积值(MgCO-Cha)分别为 CONV、COM1、COM2 和 GMAN 的 2.2、1.5、2.1 和 2.1,COM1 明显低于其他处理。在休耕期(FP),与 CONV(0.77MgCO-Cha 和 0.25kgNO-Nha)相比,COM 处理中检测到更高的温室气体通量(约为 0.90MgCO-Cha 和 0.37kgNO-Nha,分别为 COM1 和 COM2 的平均值),这可能是由于添加的有机物质的缓慢而持久的矿化作用所致。GMAN 表现出可比的 CO(0.82MgCO-Cha)和 NO 排放(0.30kgNO-Nha),这是由于收获后残留氮的限制以及豌豆吸收的抵消作用。与 CONV(约 194kgCOeqha y)的全年温室气体总排放量相比,COM 处理的总温室效应潜力(GWP)略高,平均值分别高出 11%(COM1 和 COM2)。COM2 和 COM1 的产量标准化全球变暖潜势(GWP)分别高出 60%和近 100%,这是由于 COM 产量较低,减半堆肥剂量明显减弱。GMAN 似乎是表现最好的有机处理方法,其 GWP 较低(-27%),与 CONV 相比,产量具有竞争力。与缺省的 IPCC1%值相比,所有处理的 NO 排放因子均明显较低。