British Geological Survey, Maclean Building, Crowmarsh, Oxfordshire, United Kingdom.
British Geological Survey, Maclean Building, Crowmarsh, Oxfordshire, United Kingdom.
Sci Total Environ. 2021 Aug 10;781:146698. doi: 10.1016/j.scitotenv.2021.146698. Epub 2021 Mar 24.
Increased fluxes of reactive nitrogen (N), often associated with N fertilizer use in agriculture, have resulted in negative environmental consequences, including eutrophication, which cost billions of dollars per year globally. To address this, best management practices (BMPs) to reduce N loading to the environment have been introduced in many locations. However, improvements in water quality associated with BMP implementation have not always been realised over expected timescales. There is a now a significant body of scientific evidence showing that the dynamics of legacy N storage and associated time lags invalidate the assumptions of many models used by policymakers for decision making regarding N BMPs. Building on this evidence, we believe that the concepts of legacy N storage dynamics and time lags need to be included in these models. We believe the biogeochemical research community could play a more proactive role in advocating for this change through both awareness raising and direct collaboration with policymakers to develop improved datasets and models. We anticipate that this will result in more realistic expectations of timescales for water quality improvements associated with BMPs. Given the need for multi-nutrient policy responses to tackle challenges such as eutrophication, integration of N stores will have the further benefit of aligning both researchers and policymakers in the N community with the phosphorus and carbon communities, where estimation of stores is more widespread. Ultimately, we anticipate that integrating legacy N storage dynamics and time lags into policy frameworks will better meet the needs of human and environmental health.
活性氮(N)通量的增加,通常与农业中氮肥的使用有关,已经导致了负面的环境后果,包括富营养化,这在全球每年造成数十亿美元的损失。为了解决这个问题,已经在许多地方引入了最佳管理措施(BMPs)来减少 N 对环境的负荷。然而,与 BMP 实施相关的水质改善并不总是在预期的时间内实现。现在有大量的科学证据表明,遗留 N 储存的动态及其相关的时滞使许多决策者用于决策的 N BMPs 模型的假设失效。在此基础上,我们认为这些模型需要包含遗留 N 储存动态和时滞的概念。我们认为,生物地球化学研究界可以通过提高认识和直接与决策者合作来开发改进的数据和模型,在倡导这一改变方面发挥更积极的作用。我们预计,这将使人们对与 BMP 相关的水质改善的时间框架产生更现实的期望。鉴于需要采取多营养物政策应对富营养化等挑战,整合 N 储存将进一步使 N 界的研究人员和决策者与磷和碳界保持一致,在磷和碳界,储存的估计更为广泛。最终,我们预计将遗留 N 储存动态和时滞纳入政策框架将更好地满足人类和环境健康的需求。