Department of Soil Science, Faculty of Agriculture, University of Zanjan, Zanjan, Iran.
Department of Soil Science, Faculty of Agriculture, University of Tabriz, Tabriz, Iran.
Sci Rep. 2023 Mar 29;13(1):5113. doi: 10.1038/s41598-023-32127-0.
In most agricultural fields, when soil pH is high, elemental sulfur or sulfuric acid are used to reduce soil pH and increase the availability of macro and micronutrients for optimum crop yield. However, how these inputs impact soil greenhouse gas emissions is unknown. This study aimed to measure the amount of greenhouse gas emissions and pH after the application of various doses of elemental sulfur (ES) and sulfuric acid (SA). Using static chambers, this study quantifies soil greenhouse gas emissions (CO, NO, and CH) for 12 months after the application of ES (200, 400, 600, 800, and 1000 kg ha) and SA (20, 40, 60, 80 and 100 kg ha) to a calcareous soil (pH 8.1) in Zanjan, Iran. Also, in order to simulate rainfed and dryland farming which are common practices in this area, this study was conducted with and without sprinkler irrigation. Application of ES slowly decreased soil pH (more than half a unit) over the year whereas application of SA temporarily reduced the pH (less than a half unit) for a few weeks. CO and NO emissions and CH uptake were maximum during summer and lowest in winter. Cumulative CO fluxes ranged from 1859.2 kg CO-C ha year in the control treatment to 2269.6 kg CO-C ha year in the 1000 kg ha ES treatment. Cumulative fluxes for NO-N were 2.5 and 3.7 kg NO-N ha year and cumulative CH uptakes were 0.2 and 2.3 kg CH-C ha year in the same treatments. Irrigation significantly increased CO and NO emissions and, depending on the amount of ES applied, decreased or increased CH uptake. SA application had a negligible effect on GHGs emissions in this experiment and only the highest amount of SA altered GHGs emissions.
在大多数农业领域,当土壤 pH 值较高时,会使用元素硫或硫酸来降低土壤 pH 值,增加大量和微量元素的可用性,以实现作物产量的最佳化。然而,这些投入如何影响土壤温室气体排放尚不清楚。本研究旨在测量不同剂量的元素硫(ES)和硫酸(SA)施用后温室气体排放和 pH 值的变化。本研究使用静态室,在伊朗赞詹的钙质土壤(pH 值为 8.1)上,在 12 个月内量化了 ES(200、400、600、800 和 1000 kg ha)和 SA(20、40、60、80 和 100 kg ha)施用后土壤温室气体排放(CO、NO 和 CH)的数量。此外,为了模拟该地区常见的雨养和旱地农业,本研究在有和没有 sprinkler 灌溉的情况下进行。ES 的施用使土壤 pH 值在一年内缓慢下降(超过半单位),而 SA 的施用使 pH 值在几周内暂时下降(不到半单位)。CO 和 NO 排放和 CH 吸收在夏季达到最大值,在冬季达到最小值。累积 CO 通量范围从对照处理的 1859.2 kg CO-C ha year 到 1000 kg ha ES 处理的 2269.6 kg CO-C ha year。NO-N 的累积通量分别为 2.5 和 3.7 kg NO-N ha year,相同处理下 CH 的累积吸收量分别为 0.2 和 2.3 kg CH-C ha year。灌溉显著增加了 CO 和 NO 的排放,并且取决于施用的 ES 量,减少或增加了 CH 的吸收。在本实验中,SA 的施用对 GHGs 排放的影响可以忽略不计,只有最高量的 SA 会改变 GHGs 排放。