Long-term fertilization and liming increase soil fertility but reduce carbon stratification and stocks of paddy rice soils

IF 2.1 Q3 SOIL SCIENCE
E. Amoakwah, S. Kim, S. Jeon, J. Shim, Y. Lee, Soonik Kwon, Seon-Jin Park
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Abstract

There is lack of information on the impact of acidity correctives (lime and silicate) and nitrogen (N), phosphorus (P), and potassium (K) fertilizers on the fertility, carbon stocks, carbon stratification, and carbon sequestration potential of paddy soils. To fill this knowledge gap and contribute to knowledge on how the treatments impact the soil ecosystem functions and services, a long-term field experiment was established in 1954 with four treatments and five replicates arranged in a randomized complete block design.Four treatments with five replicates per treatment were laid out in a randomized complete block design. The treatments included control/untreated (CT), only NPK, silicate-fortified NPK (NPKSi), and lime-fortified NPK (NPKLi). The treatments were applied to paddy soils classified as Fluvaquentic Eutrudepts.Application of the treatments led to significant increases in soil pH by 0.9, 1.12, and 1.5 pH units in the NPK, NPKLi, and NPKSi-treated soils in 2021, respectively, compared to the initial soil pH. The increase in pH subsequently led to significant reductions in C stratification and C stocks, with reduced rates of C sequestration observed to be more pronounced in the soils treated with lime and silicate-fortified NPK fertilizers (NKPSi and NPKLi). Both NPKSi and NPKLi moderately increased soil fertility. The highest increase in soil fertility was observed in the NPKSi treatment, with an annual growth rate of 0.0160 and a relative change ratio of 128.2% relative to the initial soil fertility index recorded in 1970. A Pearson correlation analysis revealed that soil pH, exchangeable calcium, and available silicate were the soil properties that significantly contributed to the increase in the soil fertility of the treated soils in the rice paddy agroecosystem.Conclusively, the inclusion of silicate in long-term fertilization is an effective strategy to mitigate soil acidity and increase soil fertility.
长期施肥和石灰化提高了土壤肥力,但降低了水稻田土壤的碳分层和碳储量
关于酸性改良剂(石灰和硅酸盐)以及氮肥、磷肥和钾肥对水稻田土壤肥力、碳储量、碳分层和固碳潜力的影响,目前还缺乏相关信息。为了填补这一知识空白,并为了解这些处理如何影响土壤生态系统功能和服务做出贡献,1954 年建立了一个长期田间试验,采用随机完全区组设计,共设四个处理和五个重复。处理包括对照/未处理(CT)、单一氮磷钾、硅酸盐强化氮磷钾(NPKSi)和石灰强化氮磷钾(NPKLi)。与初始土壤 pH 值相比,施用 NPK、NPKLi 和 NPKSi 处理的土壤在 2021 年的土壤 pH 值分别显著提高了 0.9、1.12 和 1.5 个 pH 单位。pH 值的升高随后导致碳分层和碳储量的显著减少,在使用石灰和硅酸盐强化的 NPK 肥料(NKPSi 和 NPKLi)处理过的土壤中,碳固存率的降低更为明显。NPKSi 和 NPKLi 都适度提高了土壤肥力。NPKSi 处理的土壤肥力增幅最大,与 1970 年记录的初始土壤肥力指数相比,年增长率为 0.0160,相对变化率为 128.2%。皮尔逊相关分析表明,土壤 pH 值、可交换钙和可利用硅酸盐是显著提高稻田农业生态系统中经处理土壤肥力的土壤特性。
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CiteScore
1.90
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