Guo Hui-Nan, Ma Li-Juan, Huang Zhi-Jie, Li Mei-Qi, Hou Zhen-An, Min Wei
Key Laboratory of Oasis Ecological Agriculture of Xinjiang Corps, College of Agriculture, Shihezi University, Shihezi 832003, China.
Huan Jing Ke Xue. 2020 May 8;41(5):2455-2467. doi: 10.13227/j.hjkx.201910137.
A shortage of freshwater resources has become a fundamental and chronic problem for sustainable agriculture development in arid regions. Use of saline water irrigation has become an important means for alleviating freshwater scarcity. However, long-term irrigation with saline water may cause salt accumulation in the soil, and further affect nitrogen transformation and NO emission. To investigate this, we conducted a ten-year field experiment to evaluate the effect of irrigation water salinity and N amount on NO emission and denitrifying bacterial communities. The experimental design was a 2×2 factorial with two irrigation water salinity levels (salinity levels are expressed as electrical conductivity), 0.35 dS·m and 8.04 dS·m, and two N amounts, 0 kg·hm and 360 kg·hm, representing SFN0, SHN0, SFN360, and SHN360, respectively. The results indicated that long-term saline water irrigation significantly increased soil salinity, moisture, and NH-N content, whereas it decreased soil pH, NO-N, organic matter, and total nitrogen content. Irrigation with saline water significantly inhibited NO emission, being associated with a decreased in level of 45.19% (unfertilized plots) and 43.50% (fertilized plots) compared with irrigation with fresh water. NO emission increased as the N amount increased; the NO emission was 161% higher in the fertilized plots than in the unfertilized plots. In the unfertilized plots, saline water irrigation significantly reduced the activity of denitrifying enzymes, the abundance of , , and , and the diversity of denitrifying bacterial communities. In the fertilized plots, saline water irrigation did not significantly affect the abundance of , whereas it significantly reduced the abundance of and . Saline water irrigation and nitrogen application altered the community structures of denitrifying bacteria with , , and ; the irrigation water salinity seemed to have a greater impact on the denitrifying bacterial community in comparison with fertilization. Linear discriminant analysis (LDA) effect size (LEfSe) analysis demonstrated that denitrifying bacterial potential biomarkers increased as the water salinity increased, meaning that saline water irrigation could alter the community structures of denitrifying bacteria, and promote the growth of dominant species. Our findings indicate that increased abundance of , , and promoted NO emission, and although long-term saline water reduced soil NO emission, it resulted in a continuous increase of soil salinity. The emission of NO had extremely positive correlation with soil NO-N, organic matter, total nitrogen, denitrifying bacteria abundance, and denitrifying enzyme activities, and was negatively correlated with soil moisture. The soil physiochemical properties and the community structure of denitrifying bacteria had a significant influence on soil NO emission in cotton fields, and bacteria showed the highest association with NO emission, thus it might be a dominant microflora in the process of denitrification. This information will aid in reducing atmospheric NO emissions in agriculturally productive alluvial grey desert soils.
淡水资源短缺已成为干旱地区可持续农业发展的一个基本且长期存在的问题。使用咸水灌溉已成为缓解淡水短缺的重要手段。然而,长期用咸水灌溉可能导致土壤中盐分积累,并进一步影响氮转化和一氧化氮排放。为对此进行研究,我们开展了一项为期十年的田间试验,以评估灌溉水盐度和氮用量对一氧化氮排放及反硝化细菌群落的影响。试验设计为2×2析因试验,有两个灌溉水盐度水平(盐度水平以电导率表示),分别为0.35 dS·m和8.04 dS·m,以及两个氮用量,分别为0 kg·hm和360 kg·hm,分别代表SFN0、SHN0、SFN360和SHN360。结果表明,长期咸水灌溉显著增加了土壤盐分、湿度和铵态氮含量,而降低了土壤pH值、硝态氮、有机质和总氮含量。咸水灌溉显著抑制了一氧化氮排放,与淡水灌溉相比,未施肥地块一氧化氮排放水平降低了45.19%,施肥地块降低了43.50%。一氧化氮排放随氮用量增加而增加;施肥地块的一氧化氮排放量比未施肥地块高161%。在未施肥地块,咸水灌溉显著降低了反硝化酶活性、nirS、nirK和nosZ的丰度以及反硝化细菌群落的多样性。在施肥地块,咸水灌溉对nirS的丰度没有显著影响,而显著降低了nirK和nosZ的丰度。咸水灌溉和施氮改变了nirS、nirK和nosZ反硝化细菌的群落结构;与施肥相比,灌溉水盐度似乎对反硝化细菌群落有更大影响。线性判别分析(LDA)效应大小(LEfSe)分析表明,随着水盐度增加,反硝化细菌潜在生物标志物增加,这意味着咸水灌溉可改变反硝化细菌群落结构,并促进优势物种生长。我们的研究结果表明,nirS、nirK和nosZ丰度增加促进了一氧化氮排放,虽然长期咸水灌溉降低了土壤一氧化氮排放,但导致土壤盐分持续增加。一氧化氮排放与土壤硝态氮、有机质、总氮、反硝化细菌丰度和反硝化酶活性呈极显著正相关,与土壤湿度呈负相关。土壤理化性质和反硝化细菌群落结构对棉田土壤一氧化氮排放有显著影响,nirK细菌与一氧化氮排放的关联度最高,因此它可能是反硝化过程中的优势微生物群落。这些信息将有助于减少农业生产性冲积灰漠土中的大气一氧化氮排放。