Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610041, China; University of Chinese Academy of Sciences, Beijing, 100049, China.
Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610041, China; University of Chinese Academy of Sciences, Beijing, 100049, China; Institut Supérieur Agronomique et Vétérinaire de Faranah (ISAV/F), Faranah, 131, Guinea.
Environ Pollut. 2022 Mar 1;296:118751. doi: 10.1016/j.envpol.2021.118751. Epub 2021 Dec 29.
Straw and biochar amendments have been shown to increase soil organic carbon (SOC) stocks in arable land; however, their effects on hydrological fluxes of dissolved organic carbon (DOC), which may offset the benefits of C sequestration amounts remain uncertain. Therefore, we conducted a three-year field study that included four treatments (CK, control with no fertilizer; NPK, synthetic N fertilizer; RSDNPK, synthetic N fertilizer plus crop residues; BCNPK, synthetic N fertilizer plus biochar of crop straw) to investigate the effects of straw and biochar amendment on DOC losses through hydrological pathways of overland flow and interflow from a wheat-maize rotation system in the subtropical montane agricultural landscape. We detected substantial intra- and inter-annual variations in runoff discharge, DOC concentration, and DOC fluxes for both overland flow and interflow pathways, which were primarily attributed to variations in rainfall amount and intensity. On average, the DOC concentrations for interflow (2.98 mg C L) were comparable with those for overland flow (2.71 mg C L) throughout the three-year experiment. However, average annual DOC fluxes for interflow were approximately 2.60 times greater than those for overland flow, which probably related to higher runoff discharges of interflow than overland flow. Compared to the control, on average, the N fertilization treatments significantly decreased the annual DOC fluxes of overland flow and significantly increased annual DOC fluxes of interflow. Relative to the application of synthetic N fertilizer only, on average, crop straw amendment practice significantly increased annual DOC fluxes of interflow by 28.7%, while decreasing annual DOC fluxes of overland flow by 12.0%; in contrast, biochar amendment practice decreased annual DOC fluxes of interflow by 25.3% while increasing annual DOC fluxes of overland flow by 44.6%. Overall, considering both overland flow and interflow, crop straw amendment significantly increased hydrological DOC fluxes, whereas biochar had no significant effects on hydrological DOC fluxes throughout the three-year experiment. We conclude that crop straw incorporation strategies that aim to increase SOC stocks may enhance hydrological losses of DOC, thereby in turn offsetting its benefits in the subtropical montane agricultural landscapes.
秸秆和生物炭的添加已被证明可以增加耕地土壤有机碳(SOC)储量;然而,它们对溶解有机碳(DOC)水文通量的影响,这些影响可能会抵消碳固存量的好处,目前仍不确定。因此,我们进行了一项为期三年的田间研究,其中包括四个处理(CK,不施化肥对照;NPK,合成氮肥;RSDNPK,合成氮肥加作物残体;BCNPK,合成氮肥加作物秸秆生物炭),以调查秸秆和生物炭添加对亚热带山地农业景观中小麦-玉米轮作系统地表径流和侧向流中 DOC 损失的影响。我们发现,地表径流和侧向流的径流量、DOC 浓度和 DOC 通量都存在很大的年内和年际变化,这主要归因于降雨量和强度的变化。平均而言,整个三年实验期间,侧向流的 DOC 浓度(2.98mg C L)与地表径流的 DOC 浓度(2.71mg C L)相当。然而,侧向流的年平均 DOC 通量约为地表径流的 2.60 倍,这可能与侧向流的径流量高于地表径流有关。与对照相比,氮施肥处理平均显著降低了地表径流的年 DOC 通量,显著增加了侧向流的年 DOC 通量。与仅施用合成氮肥相比,平均而言,秸秆添加措施显著增加了侧向流的年 DOC 通量 28.7%,同时减少了地表径流的年 DOC 通量 12.0%;相比之下,生物炭添加措施减少了侧向流的年 DOC 通量 25.3%,同时增加了地表径流的年 DOC 通量 44.6%。总体而言,考虑到地表径流和侧向流,秸秆添加措施显著增加了水文 DOC 通量,而生物炭在整个三年实验中对水文 DOC 通量没有显著影响。我们的结论是,旨在增加 SOC 储量的秸秆添加策略可能会增加水文 DOC 的损失,从而抵消其在亚热带山地农业景观中的好处。