Wang Zi-Jun, Wang Hong-Hao, Li Jin-Qiu, Wu Yan-Zheng, Fu Pei-Jiao, Meng Lei, Tang Shui-Rong
College of Tropical Crops, Hainan University, Haikou 570228, China.
Huan Jing Ke Xue. 2021 Aug 8;42(8):3931-3942. doi: 10.13227/j.hjkx.202011247.
Based on the rice-vegetable crop rotation model, in-situ measurements of nitrous oxide (NO) and methane (CH) emissions were conducted in double-cropping rice fields in Hainan to determine the impact of coconut chaff biochar on greenhouse gas emissions. The experiment involved four treatments:conventional farming fertilization (CON), nitrogen fertilizer combined with 20 t ·hm biochar (B1), nitrogen fertilizer combined with 40 t ·hm biochar (B2), and no nitrogen fertilizer, as the control (CK). The NO and CH emissions were measured using static chamber-gas chromatography during the two paddy seasons, and the global warming potential (GWP) and greenhouse gas intensity (GHGI) were also estimated. The results show that NO emission dynamics during the early rice season are closely related to the mineral nitrogen content of the soil. The NO is emitted at the rice seedling and tillering stages after fertilization. The cumulative NO emission during the early rice season was 0.18-0.76 kg ·hm. Compared with the CON treatment, the biochar treatments reduced NO by 18%-43%, and the B2 treatment resulted in a significant reduction. The addition of biochar may promote the reduction of NO at the early rice seedling stage and increase NO emissions by improving the soil NO-N content at the early rice tillering stage. During the late rice season, NO is emitted during the heading and maturity stages, and the cumulative NO emission was 0.17-0.34 kg ·hm. The B1 treatment reduced emissions by 37%, and B2 increased emission by only 3%, which is not a significant difference. The peak of CH emissions from rice fields appeared in the late phase of the early rice season and prophase of the late rice season. The cumulative emission of CH in the early rice season was 3.11-14.87 kg ·hm. Compared with CON, the CK treatment increased emission by 39%. The biochar treatment may increase soil aeration and limit the ability of CH production in the early rice season, as B1 and B2 treatments reduced CH emissions by 28% and 71%. The cumulative CH emission in late rice season was 53.1-146.3 kg ·hm, and the emission dynamics were significantly positively correlated with NH-N content. CK and B1 treatments increased CH emissions by 52% and 99%, respectively compared with CON, and the B2 treatment significantly increased CH emissions by 176%. Compared with CON, the B1 and B2 treatments increased the yield by 12.0% and 14.3% when applied in the early rice season and by 7.6% and 0.4% when applied in the late rice season, respectively. Due to the increased methane emissions in the late rice season, biochar amendment increased the GWP of the double-cropping rice field, in which the high amount of biochar reached a significant level; different amounts of biochar had no significant effect on the GHGI of the double-cropping rice field. Thus, the application of coconut chaff biochar for the reduction of greenhouse gas emission, from rice fields in hot areas, requires further research.
基于稻菜轮作模式,在海南双季稻田进行了氧化亚氮(NO)和甲烷(CH)排放的原位测量,以确定椰壳生物炭对温室气体排放的影响。该试验包括四种处理:常规耕作施肥(CON)、氮肥+20 t·hm生物炭(B1)、氮肥+40 t·hm生物炭(B2)以及不施氮肥作为对照(CK)。在两个水稻季利用静态箱-气相色谱法测量了NO和CH排放,并估算了全球变暖潜势(GWP)和温室气体强度(GHGI)。结果表明,早稻季NO排放动态与土壤矿质氮含量密切相关。施肥后在水稻苗期和分蘖期排放NO。早稻季NO累积排放量为0.18-0.76 kg·hm。与CON处理相比,生物炭处理使NO减少了18%-43%,B2处理导致显著减少。添加生物炭可能促进早稻苗期NO的还原,并通过提高早稻分蘖期土壤NO-N含量增加NO排放。晚稻季,在抽穗期和成熟期排放NO,NO累积排放量为0.17-0.34 kg·hm。B1处理使排放量减少了37%,B2处理仅使排放量增加了3%,差异不显著。稻田CH排放峰值出现在早稻季后期和晚稻季前期。早稻季CH累积排放量为3.11-14.87 kg·hm。与CON相比,CK处理使排放量增加了39%。生物炭处理可能增加土壤通气性并限制早稻季CH产生能力,因为B1和B2处理使CH排放量分别减少了28%和71%。晚稻季CH累积排放量为53.1-146.3 kg·hm,排放动态与NH-N含量显著正相关。与CON相比,CK和B1处理分别使CH排放量增加了52%和99%,B2处理使CH排放量显著增加了176%。与CON相比,B1和B2处理在早稻季施用时产量分别提高了12.0%和14.3%,在晚稻季施用时产量分别提高了7.6%和0.4%。由于晚稻季甲烷排放量增加,生物炭改良增加了双季稻田的GWP,其中高量生物炭达到显著水平;不同量生物炭对双季稻田的GHGI没有显著影响。因此,在炎热地区稻田应用椰壳生物炭减少温室气体排放还需要进一步研究。