Effects of fertilizer application strategies on soil organic carbon and total nitrogen storage under different agronomic practices: A meta‐analysis

Abstract

Fertilizer application strategies can impact soil health, mainly soil organic carbon (SOC) and total nitrogen (TN) sequestration, which are essential in mitigating climate change. Many studies have been conducted on the influence of fertilizer use on SOC and TN storage. Results can, however, be variable in different sites because of various management practices and environmental conditions; therefore, we conducted a global meta‐analysis of 953 observations from 143 papers on the impact of different fertilizers (mineral N (NF), manure (Mn) and mixed fertilizers (MNF: combination of mineral and organic fertilizer)) on SOC and TN storage under various cropping systems and environmental conditions in agricultural land. The results showed that MNF led to the greatest SOC and TN stocks. Noticeably, animal Mn sequestered higher amounts of SOC and TN compared to green Mn. In addition, MNF increases SOC in the medium term (10–20 years, 43.71%) and TN in the short term (0–10 years, 40.85%), which could be related to their nutrient's cycles and residence time in the soil. The higher effectiveness of SOC and TN sequestration (12.84% and 27.42%, respectively) under NF was observed at high rates >250 kg N/ha in comparison to low rates of 0–250 kg N/ha. A significant SOC increment was observed with MNF (37.76%) and Mn (19.45%) under continuous cropping (monoculture) than crop rotations. In contrast, TN was higher with MNF (58.31%) and Mn (18.23%) with crop rotations. The subhumid and semi‐arid zones had greater increase in SOC (28.24%) and TN (74.54%) stock in comparison to other climatic conditions. Overall, this study emphasized that MNF could optimize SOC and TN storage in agricultural soils depending upon edaphic and regional climatic conditions.

Phosphorus Distribution within Aggregates in Long-Term Fertilized Black Soil: Regulatory Mechanisms of Soil Organic Matter and pH as Key Impact Factors

“…Therefore, the change in soil pH controls the transformation of P forms, and a typical example is that the decrease in soil pH promotes the solubilization of calcium phosphate minerals and increases the Fe/Al-associated P [18,19]. Generally, both chemical fertilizer and chemical fertilizer combined with organic fertilizer increase SOM levels [20], which could be due to fertilization practices increasing production and promoting the input of more biomass, as well as the direct input of organic materials contributing to increasing SOM, while changes in soil pH vary by fertilization practices [21,22]. At present, there is a lack of assessment and mechanistic studies focusing on the impact of SOM and pH on soil P form transformation and distribution under different fertilization practices.…”