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A Century of Legacy Phosphorus Dynamics in a Large Drainage Basin

机译：大型排水盆地中的一个世纪遗产磷动力学

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Abstract >There is growing evidence that the release of phosphorus (P) from “legacy” stores can frustrate efforts to reduce P loading to surface water from sources such as agriculture and human sewage. Less is known, however, about the magnitude and residence times of these legacy pools. Here we constructed a budget of net anthropogenic P inputs to the Baltic Sea drainage basin and developed a three‐parameter, two‐box model to describe the movement of anthropogenic P though temporary (mobile) and long‐term (stable) storage pools. Phosphorus entered the sea as direct coastal effluent discharge and via rapid transport and slow, legacy pathways. The model reproduced past waterborne P loads and suggested an ~30‐year residence time in the mobile pool. Between 1900 and 2013, 17 and 27?Mt P has accumulated in the mobile and stable pools, respectively. Phosphorus inputs to the sea have halved since the 1980s due to improvements in coastal sewage treatment and reductions associated with the rapid transport pathway. After decades of accumulation, the system appears to have shifted to a depletion phase; absent further reductions in net anthropogenic P input, future waterborne loads could decrease. Presently, losses from the mobile pool contribute nearly half of P loads, suggesting that it will be difficult to achieve substantial near‐term reductions. However, there is still potential to make progress toward eutrophication management goals by addressing rapid transport pathways, such as overland flow, as well as mobile stores, such as cropland with large soil‐P reserves. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >日益增长的证据表明，来自“遗产”商店的磷（p）释放可能会令人沮丧从农业和人类污水等来源减少P加载到地表水的努力。然而，较少是已知这些传统池的幅度和停留时间。在这里，我们构建了净人为P进入的预算，并开发了三个参数，双箱模型，以描述人为P虽然临时（移动）和长期（稳定）储存池。磷作为直接沿海污水排放和快速运输和缓慢，遗产途径进入海洋。该模型转载了过去的水性P负载，并建议在移动池中建议〜30年的停留时间。在1900和2013,17和27之间，分别在移动和稳定池中积累了MT P。由于沿海污水处理和与快速运输途径相关的减少，20世纪80年代以来，海上的磷投入已经减半。经过几十年的积累，系统似乎已转移到耗尽阶段;缺乏进一步减少净人为p输入，未来的水性载荷可能会降低。目前，来自移动池的损失有近一半的P负载，表明它将难以实现大量的近期减少。然而，仍有潜力通过解决快速运输途径，例如陆地流动，以及移动商店，例如具有大型土壤-P储备的耕地。</ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23728/'>《Global Biogeochemical Cycles》</a> <b style="margin: 0 2px;">|</b><span>2018年第7期</span><b style="margin: 0 2px;">|</b><span>共16页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McCrackin Michelle L.&option=202" target="_blank" rel="nofollow">McCrackin Michelle L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Muller‐Karulis B?rbel&option=202" target="_blank" rel="nofollow">Muller‐Karulis B?rbel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gustafsson Bo G.&option=202" target="_blank" rel="nofollow">Gustafsson Bo G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Howarth Robert W.&option=202" target="_blank" rel="nofollow">Howarth Robert W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Humborg Christoph&option=202" target="_blank" rel="nofollow">Humborg Christoph;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Svanb?ck Annika&option=202" target="_blank" rel="nofollow">Svanb?ck Annika;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Swaney Dennis P.&option=202" target="_blank" rel="nofollow">Swaney Dennis P.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Baltic Sea CentreStockholm UniversityStockholm Sweden;</p> <p>Baltic Sea CentreStockholm UniversityStockholm Sweden;</p> <p>Baltic Sea CentreStockholm UniversityStockholm Sweden;</p> <p>Department of Ecology and Evolutionary BiologyCornell UniversityIthaca NY USA;</p> <p>Baltic Sea CentreStockholm UniversityStockholm Sweden;</p> <p>Baltic Sea CentreStockholm UniversityStockholm Sweden;</p> <p>Department of Ecology and Evolutionary BiologyCornell UniversityIthaca NY USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/165.html" title="地质学">地质学;</a><a href="https://www.zhangqiaokeyan.com/clc/5109.html" title="生物地球化学、气体地球化学">生物地球化学、气体地球化学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=legacy phosphorus&option=203" rel="nofollow">legacy phosphorus;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eutrophication&option=203" rel="nofollow">eutrophication;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=model&option=203" rel="nofollow">model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Baltic Sea&option=203" rel="nofollow">Baltic Sea;</a> </p> <div class="translation"> 机译：遗传磷;富营养化;模型;波罗的海; 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