Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, 138 Haping Rd, Harbin, 150081, People's Republic of China.
Department of Agronomy, Iowa State University, Ames, IA, USA.
Sci Rep. 2020 Sep 9;10(1):14793. doi: 10.1038/s41598-020-71448-2.
Application of phosphorus (P), a major plant nutrient, as fertilizer is critical to maintain P level for crop production and yield in most cultivated soils. While, it may impact the dynamics, limited studies have examined the long-term effects of fertilization on P fractions in a soil profile in Mollisol. A long-term field experiment was conducted at the State Key Experimental Station of Agroecology of the Chinese Academy of Sciences in Hailun county, Heilongjiang Province, China. A sequential fractionation procedure was used to determine the effect of fertilizer (types) treatments including no fertilizer (CK), chemical fertilizer (NPK), chemical fertilizer plus straw (NPK + S) and pig manure (OM) on fractions of P and their distribution within 0-100 cm soil profiles. Unlike CK treatment, the long-term application of fertilizers increased the concentration and accumulation of total and available P in 0-20 and 0-40 cm soil depths than deeper soils, respectively. The phosphorus activity coefficient (PAC) ranged from 1.5 to 13.8% within 0-100 cm soil depth. The largest PAC value was observed under OM treatment at 0-40 cm soil depth and under NPK + S treatment at 40-100 cm soil depth. The Ca-P and Ca-P concentrations increased significantly by 0.5-7.5 times and 0.5-10.4 times, respectively in OM treatment with the largest value in 0-40 cm soil depth over CK treatment. The Al-P concentration under NPK + S and OM treatments increased throughout the soil profile. The OM treatment increased all Po concentrations in the 0-40 cm soil depth, while NPK and NPK + S treatments increased labile organic P, moderately labile organic P, and highly stable organic P in the 0-20 cm soil depth. Thus, the application of fertilizer and straw, or organic manure may enhance inorganic and organic P pool in a Mollisol in Northeast China. Thus, organic manure application in the subsoil as a potential P source and their impact should be considered in developing management practices and policies regarding nutrient management.
磷(P)是一种主要的植物养分,作为肥料应用对于维持大多数耕地土壤中的 P 水平和作物产量至关重要。然而,施肥可能会影响 P 的动态,尽管已有有限的研究考察了长期施肥对黑土土壤剖面中 P 形态的影响。在中国黑龙江省海伦县中国科学院农业生态系统国家重点实验站内进行了一项长期田间试验。采用连续提取法,研究了不同施肥(类型)处理(不施肥 CK、化肥 NPK、化肥加秸秆 NPK+S 和猪粪 OM)对 0-100 cm 土壤剖面中 P 形态及其分布的影响。与 CK 处理相比,长期施肥增加了 0-20 和 0-40 cm 土壤深度中总 P 和有效 P 的浓度和积累量,而对较深土壤的影响则较小。磷活性系数(PAC)在 0-100 cm 土壤深度范围内为 1.5-13.8%。在 0-40 cm 土壤深度下,OM 处理的 PAC 值最大,在 40-100 cm 土壤深度下,NPK+S 处理的 PAC 值最大。与 CK 相比,OM 处理下 Ca-P 和 Ca-P 浓度分别显著增加了 0.5-7.5 倍和 0.5-10.4 倍,在 0-40 cm 土壤深度下最大。NPK+S 和 OM 处理下 Al-P 浓度在整个土壤剖面中均增加。OM 处理增加了 0-40 cm 土壤深度内所有 Po 浓度,而 NPK 和 NPK+S 处理增加了 0-20 cm 土壤深度内的易解有机磷、中等解有机磷和高度稳定有机磷。因此,在中国东北地区黑土中,施用化肥和秸秆或有机肥可能会增加无机和有机 P 库。因此,在制定有关养分管理的管理实践和政策时,应考虑将底土中的有机肥作为潜在的 P 源及其影响。