The unreasonable use of fertilizers is a significant cause of cultivated soil cadmium (Cd) accumulation. Although there is research about the effect of fertilizers on soil cadmium (Cd) accumulation under different crops, soils, and cultivation durations locally and specifically, its relative and determinant factors are seldom comprehensively and comparatively researched and evaluated. We used meta-analysis to analyze the effects of fertilizers (mineral fertilizer N, P, K (NPK) with manure (NPKM), NPK with straw (NPKS), and the mineral fertilizer N (N), NK (NK)), crops, duration, climate, and soil texture on the Chinese soil total and available Cd change during 1987–2022. The results showed that the order of the increased soil total and available Cd change was NPKM (total: 62%–104%, available: 61%–143%) > NPKS (50%–86%, 48%–116%) > NPK (25%–50%, 35%–75%) > NK (5%–19%, 19%–33%) > N (2%–6%, 7%–31%). NPKM and NPKS significantly increased the total Cd under maize (104%, 86%) and available Cd under rice (136%, 116%). Cd changed the fastest with the NPKM cultivation duration for total Cd under maize (slope: 5.9) and available Cd under rice (6.6). The change of the soil total and available Cd had the higher value in the semiarid region, clay soils, lower pH, and long cultivations. The change of the soil total and available Cd were highest (398%, 375%) in the semiarid region for clay loam after 20–25 years of NPKM fertilization, when the pH decreased to the lowest (−1.9). According to the aggregated boosted tree analysis, the fertilizers and duration were the best explanatory variable (>53%) for the soil total and available Cd. In conclusion, the soil Cd could be mitigated through reducing the long–term manure, straw, and P fertilizer content with Cd, and field managements such as liming, wetting, and drying according to the crops, climate, and soil texture.

The effect of biochar addition on enzyme stoichiometry and regulatory mechanisms in saline-alkali soil is still vague. We studied how five years (2018–2023) of applying 10 t biochar ha⁻¹ yr⁻¹ influences soil’s chemical and microbial properties, microbial element utilization efficiency, and resource limitations in the Tarim River basin. Low, medium, and high nitrogen fertilization (kg N ha⁻¹) and irrigation (W) (mm) with or without biochar (B) were as follows: low nitrogen low irrigation (LNLW, 100/140), mid nitrogen mid irrigation (MNMW, 200/220), high nitrogen high irrigation (HNHW, 300/320), LNLWB, MNMWB, and HNHWB. Biochar application (LNLWB, MNMWB, HNHWB) increased soil organic carbon (+61%, +55%, +59%), total N (+9%, +16%, +8%), total phosphorus (+6%, +5%, +27%), microbial N (+75%, +86%, +28%) and P use efficiency (+60%, +45%, +27%), but decreased microbial biomass carbon (−6%, −29%, −45%), and microbial carbon use efficiency (−6%, −7%, −7%). Biochar application alleviated microbial C limitation but increased the P limitation of MNMW and the N limitation of HNHW. In conclusion, with a 1/3 reduction in N fertilization and irrigation compared with HNHW (MNMW), biochar can greatly alleviate microbial resource limitations and improve soil fertility in saline-alkaline soils.