National-Regional Joint Engineering Research Center for Soil Pollution Control and Remediation in South China, Guangdong Key Laboratory of Integrated Agro-environmental Pollution Control and Management, Institute of Eco-environmental and Soil Sciences, Guangdong Academy of Sciences, Guangzhou 510650, China.
Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
Sci Total Environ. 2021 Mar 25;762:143059. doi: 10.1016/j.scitotenv.2020.143059. Epub 2020 Oct 15.
Carbon (C) and nitrogen (N) inputs to farmland via fertilizer application are potential sources of C and N that influence soil acidification and water eutrophication. A pilot study was conducted to compare the effects of compound fertilizer and rapeseed cake organic fertilizer on C and N preservation in the soils and runoff of a tea plantation as well as the C and N isotopic fractionation in soils over the three annual cycles of fertilization and tea-leaf harvest. Overall, rapeseed cake organic fertilization effectively increased the pH, total organic matter, NH-N and NO-N in soils by 2.19-4.29%, 8.04-21.14%, 53.65-100.32% and 5.74-54.08%, respectively, but decreased NH-N inputs in runoff by 10.36-25.12% and NO-N inputs in runoff by 8.94-24.10% relative to the same rate of pure N in compound fertilizer. Before fertilization in February, the average δC and δN were -25.15‰ and 1.88‰, while after a full year of fertilization and tea-leaf harvesting in October, the average soil δC and δN contents were -23.83‰ and -0.33‰ after compound fertilization and -26.22‰ and 1.64‰ after rapeseed cake organic fertilization, respectively, indicating the evident effects of fertilization on the isotopic fractionation in soil. In addition, the fractionation extent was positively associated with the fertilization rates under both fertilizers. However, the two fertilization types had different effects on the C and N isotope fractionations, with rapeseed cake organic fertilization contributing more to δC (21.07-81.80%) but less to δN (18.20-78.93%) and compound fertilization presenting the opposite results (1.88-46.18% and 53.82-98.12%, respectively). This study demonstrates that rapeseed cake organic fertilization can better preserve soil C and N pools while reducing their runoff in tea plantations, which may greatly hinder the regional soil acidification and water eutrophication trends.
农田通过施用化肥向土壤输入的碳(C)和氮(N)是影响土壤酸化和水体富营养化的 C 和 N 潜在来源。本研究进行了一项试点研究,以比较复合肥和菜籽饼有机肥对茶园土壤酸化和径流水体中 C 和 N 流失的影响,以及在三个施肥和茶叶收获年度周期中土壤 C 和 N 同位素分馏的影响。总体而言,菜籽饼有机肥可有效提高土壤 pH 值、总有机碳、NH-N 和 NO-N,分别提高 2.19-4.29%、8.04-21.14%、53.65-100.32%和 5.74-54.08%,但减少了径流中 NH-N 的输入(10.36-25.12%)和 NO-N 的输入(8.94-24.10%),与复合肥中相同的纯 N 投入相比。在 2 月施肥前,平均 δC 和 δN 分别为-25.15‰和 1.88‰,而在 10 月完成一年的施肥和茶叶收获后,复合肥处理后土壤 δC 和 δN 含量平均分别为-23.83‰和-0.33‰,菜籽饼有机肥处理后分别为-26.22‰和 1.64‰,表明施肥对土壤同位素分馏有明显影响。此外,两种肥料下,分馏程度与施肥率呈正相关。然而,两种施肥类型对 C 和 N 同位素分馏的影响不同,菜籽饼有机肥对 δC 的贡献更大(21.07-81.80%),对 δN 的贡献更小(18.20-78.93%),而复合肥的结果相反(1.88-46.18%和 53.82-98.12%)。本研究表明,菜籽饼有机肥可更好地保持茶园土壤 C 和 N 库,同时减少其径流水体中的流失,这可能会极大地阻碍区域土壤酸化和水体富营养化的趋势。