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[水肥用量对夏玉米田土壤CO排放的综合影响]

[Comprehensive Effects of the Application of Water and Fertilizer Amount on CO Emission from Soils of Summer-maize Field].

作者信息

Yang Shuo-Huan, Zhang Bao-Cheng, Wang Li, Hu Tian-Tian

机构信息

College of Water Resources and Architectural Engineering, Northwest A & F University, Yangling 712100, China.

Key Laboratory for Agriculture Soil and Water Engineering in Arid Area, Ministry of Education, Northwest A & F University, Yangling 712100, China.

出版信息

Huan Jing Ke Xue. 2016 Dec 8;37(12):4780-4788. doi: 10.13227/j.hjkx.201605114.

Abstract

Field experiments were conducted to determine the effects of water and fertilizer amount on soil CO emissions by using the method of static chamber/gas chromatography in summer maize farmland ecosystem. Three factors (three irrigation levels including 90 mm, 76.5 mm and 63 mm, four nitrogen fertilizer levels including 300 kg·hm, 255 kg·hm, 210 kg·hm and 0 kg·hm, and four phosphate fertilizer levels including 90 kg·hm, 76.5 kg·hm, 63 kg·hm and 0 kg·hm) were designed in the experiment. The results showed that soil CO emission under different water and fertilizer conditions showed obvious seasonal fluctuation, the main and secondary peak appeared at jointing to tasseling stage and tasseling to grouting stage. The soil CO emissions were relevant to the supply levels of fertilizer and irrigation. In the high fertilizer F (N 300 kg·hm, PO 90 kg·hm) and low fertilizer F (N 210 kg·hm, PO 63 kg·hm) conditions, average soil CO emissions flux during the whole growth period of high water W (90 mm) was significantly higher than that of low water W (63 mm); the difference of soil CO emissions between medium water level W (76.5 mm) and low water level was not significant under medium and low nutrient condition F (N 255 kg·hm, PO 76.5 kg·hm). Soil CO emissions intensity of high fertilizer F was significantly larger (by 14.82%) than that of low fertilizer F under high water supply W (<0.05), and that of F was significantly bigger (by 8.03%) than that of F in the medium water supply(<0.05), while the difference between treatments at low water level was not significant(>0.05). Compared with nonfertilized treatment, soil CO cumulative emissions of the whole growth period with application of nitrogen fertilizer (210 kg·hm), phosphate fertilizer (63 kg·hm) and nitrogen mixed with phosphate fertilizer (210 kg·hm, 63 kg·hm) were significantly increased by 23.70%, 19.00% and 12.30%, respectively. And interaction effects between nitrogen and phosphorus fertilizer were extremely significant (<0.01). Variance analysis of the interaction of water and fertilizer showed that the average soil CO fluxes of the whole growth period were not statistically significant but cumulative emissions of soil CO were significant (<0.05) when the difference of supply level was 15%. In addition, soil CO flux and cumulative emission in the whole growth period were significant when supply differed by 30%. Obviously, soil CO emissions were promoted significantly by application of irrigation amount, nitrogen fertilizer, phosphorus rate and water and fertilizer interaction, while it was inhibited by nitrogen mixed with phosphorus. It was effective to regulate soil CO emission by water and fertilizer controlling measures.

摘要

通过静态箱/气相色谱法,在夏玉米农田生态系统中开展田间试验,以确定水和肥料用量对土壤CO排放的影响。试验设计了三个因素(三个灌溉水平,分别为90毫米、76.5毫米和63毫米;四个氮肥水平,分别为300千克·公顷、255千克·公顷、210千克·公顷和0千克·公顷;四个磷肥水平,分别为90千克·公顷、76.5千克·公顷、63千克·公顷和0千克·公顷)。结果表明,不同水、肥条件下土壤CO排放呈现明显的季节波动,主峰值和次峰值出现在拔节至抽雄期以及抽雄至灌浆期。土壤CO排放与肥料供应水平和灌溉有关。在高肥F(N 300千克·公顷,P₂O₅ 90千克·公顷)和低肥F(N 210千克·公顷,P₂O₅ 63千克·公顷)条件下,高水W(90毫米)处理在整个生育期的平均土壤CO排放通量显著高于低水W(63毫米)处理;在中低养分条件F(N 255千克·公顷,P₂O₅ 76.5千克·公顷)下,中水水平W(76.5毫米)和低水水平之间的土壤CO排放差异不显著。在高供水W条件下,高肥F处理的土壤CO排放强度显著大于低肥F处理(高14.82%)(P<0.05),在中供水条件下,高肥F处理的土壤CO排放强度显著大于低肥F处理(高8.03%)(P<0.05),而在低水水平处理间差异不显著(P>0.05)。与不施肥处理相比,施用氮肥(210千克·公顷)、磷肥(63千克·公顷)以及氮磷肥配施(210千克·公顷,63千克·公顷)处理在整个生育期的土壤CO累积排放量分别显著增加了23.70%、19.00%和12.30%。并且氮磷肥之间的交互作用极显著(P<0.01)。水、肥交互作用的方差分析表明,当供应水平差异为15%时,整个生育期的平均土壤CO通量无统计学显著差异,但土壤CO累积排放量显著(P<0.05)。此外,当供应差异为30%时,整个生育期的土壤CO通量和累积排放量显著。显然,灌溉量、氮肥、磷肥用量以及水、肥交互作用显著促进了土壤CO排放,而氮磷肥配施则抑制了土壤CO排放。通过水、肥调控措施来调节土壤CO排放是有效的。

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