Liu Xin-Yu, Lu Jiang, Meng Xuan, Liu Zheng, Song Peng, Li Ji, Tian Guang-Ming
Organic Recycling Research Institute (Suzhou) of China Agricultural University, Suzhou 215100, China.
Institute of Rural Economy, Liaoning Academy of Agricultural Sciences, Shenyang 110161, China.
Huan Jing Ke Xue. 2023 Aug 8;44(8):4647-4654. doi: 10.13227/j.hjkx.202204315.
The literature from a long-term fertilization experiment in the Yangtze River Economic Belt from January 1992 to May 2022 was collected, and the data of farmland soil organic carbon were extracted and integrated. Using the normalization treatment and the analysis method of relative annual variation, the overall change in soil organic carbon content in farmland in the Yangtze River Economic Belt under different long-term fertilization measures was studied, and the change differences of soil organic carbon content under three tillage modes were compared so as to judge and analyze the influence of the duration of the experiment on soil organic carbon dynamics. The results showed that under different long-term fertilization measures, the organic carbon content of farmland soil in the Yangtze River Economic Belt in China showed an overall upward trend. The NP, NPK, O, and NPKO treatments all increased the organic carbon content of agricultural soils, with that of the NPKO treatment being the largest. The sole application of inorganic nitrogen fertilizer reduced the organic carbon content of the soil. The rates of change in soil organic carbon content were 0.22 g·(kg·a), 0.24 g·(kg·a), and 0.16 g·(kg·a)for dryland, paddy, and water-dry rotation farmland, respectively. Additionally, the relatively rapid increase effect of organic carbon brought by the O and NPKO treatments could last for no more than 28 years in dryland soil but could still last for more than 28 years in paddy field and paddy-upland rotation soil. There was some variation in the rate of change of soil organic carbon content between soil types. The average rate of change of organic carbon was 0.25 g·(kg·a)for red soils, 0.14 g·(kg·a) for brown soils, 0.19 g·(kg·a) for tidal soils, and 0.15 g·(kg·a) for rice soils. The trend of NPKO>O>NPK>NPK>NP>N was basically maintained for the rate of change in soil organic carbon content. The NPKO treatments were all significantly higher than the chemical fertilizer (N, NP, and NPK) treatments alone. The N treatment showed a reduction in organic carbon content in both red soil and rice soils. Considering the carbon fixation of farmland soil, the combined application of organic and inorganic fertilizers is a more suitable fertilization method in this area.
收集了1992年1月至2022年5月长江经济带长期施肥试验的文献资料,提取并整合了农田土壤有机碳数据。采用归一化处理和相对年变化分析方法,研究了长江经济带不同长期施肥措施下农田土壤有机碳含量的总体变化情况,并比较了三种耕作方式下土壤有机碳含量的变化差异,以判断和分析试验时长对土壤有机碳动态的影响。结果表明,在不同长期施肥措施下,我国长江经济带农田土壤有机碳含量总体呈上升趋势。NP、NPK、O和NPKO处理均提高了农田土壤有机碳含量,其中NPKO处理增幅最大。单施无机氮肥降低了土壤有机碳含量。旱地、水田和水旱轮作农田土壤有机碳含量的变化速率分别为0.22 g·(kg·a)、0.24 g·(kg·a)和0.16 g·(kg·a)。此外,O和NPKO处理带来的有机碳较快增加效应在旱地土壤中持续不超过28年,但在水田和水旱轮作土壤中仍可持续超过28年。不同土壤类型间土壤有机碳含量变化速率存在一定差异。红壤有机碳平均变化速率为0.25 g·(kg·a),棕壤为0.14 g·(kg·a),潮土为0.19 g·(kg·a),水稻土为0.15 g·(kg·a)。土壤有机碳含量变化速率基本维持NPKO>O>NPK>NP>N的趋势。NPKO处理均显著高于单施化肥(N、NP和NPK)处理。N处理在红壤和水稻土中均表现为有机碳含量降低。从农田土壤固碳角度考虑,有机无机肥配施是该区域较为适宜的施肥方式。