School of Water Conservancy, North China University of Water Resources and Electric Power, Zhengzhou, Henan, 450045, China.
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, Shaanxi, 712100, China.
J Environ Manage. 2024 Sep;368:122140. doi: 10.1016/j.jenvman.2024.122140. Epub 2024 Aug 12.
Applying biochar to nitrogen (N)-fertilized soils is recognized as an effective technique for enhancing soil carbon (C) accumulation and improving agroecosystem sustainability. However, the impact of co-application of biochar and N fertilizer on soil C and N stocks, as well as their fractions, within the 0-60 cm soil profile remains unclear. This study examined the soil C and N fractions as well as stocks in soil profiles, and the primary influencing factors in wheat field with different rates of biochar (0, 20 and 40 t ha; B0, B1 and B2) and N application (0, 180 and 360 kg N ha; N0, N1 and N2). The results revealed that compared to B0N0 treatment, biochar plus N application increased soil organic carbon (SOC) and dissolved organic carbon (DOC), while N application alone decreased microbial biomass carbon (MBC). SOC in topsoil (0-10 cm) and DOC in subsoil (40-60 cm) were more susceptible to biochar and N application. The combined application of biochar and N enhanced soil N fractions, with NO-N having the highest sensitivity than the other N fractions, whereas biochar application alone decreased topsoil inorganic N content. Biochar and N application significantly altered soil C stocks (4.33%-42.20%) and N stocks (-1.24%-20.91%) within the 0-60 cm soil layers, and belowground biomass and SOC were the main influencing factors, respectively. The combination of moderate biochar (42.35 t ha) and N (277.78 kg ha) application was the most beneficial for soil C accumulation in the 0-60 cm depth. These findings indicate the positive impacts of co-applying of biochar and N in agroecosystems on soil C and N accumulations, and highlight the importance of C and N stabilization in both topsoil and subsoil under management practice.
将生物炭应用于施氮土壤被认为是一种有效提高土壤碳(C)积累和改善农业生态系统可持续性的技术。然而,生物炭和氮肥共施对 0-60cm 土壤剖面中土壤 C 和 N 储量及其组分的影响尚不清楚。本研究调查了不同生物炭(0、20 和 40t/ha;B0、B1 和 B2)和氮肥(0、180 和 360kg/ha;N0、N1 和 N2)用量下小麦田土壤剖面中的 C 和 N 组分以及储量,以及主要影响因素。结果表明,与 B0N0 处理相比,生物炭与氮肥共施增加了土壤有机碳(SOC)和溶解性有机碳(DOC),而氮肥单施降低了微生物生物量碳(MBC)。表层土壤(0-10cm)的 SOC 和亚表层土壤(40-60cm)的 DOC 更容易受到生物炭和氮肥的影响。生物炭和氮肥的共同应用增强了土壤 N 组分,其中硝态氮(NO-N)比其他 N 组分更敏感,而生物炭单独施用会降低表层土壤无机 N 含量。生物炭和氮肥的施用显著改变了 0-60cm 土层土壤 C 储量(4.33%-42.20%)和 N 储量(-1.24%-20.91%),地下生物量和 SOC 分别是主要影响因素。在农业生态系统中,适度生物炭(42.35t/ha)和氮肥(277.78kg/ha)的共施最有利于 0-60cm 土层土壤 C 的积累。这些结果表明,生物炭和氮肥共施对土壤 C 和 N 积累具有积极影响,并强调了在管理实践中,C 和 N 在表层和亚表层的稳定的重要性。