Assessment of connectivity in a water‐stressed wetland (Kaabar Tal) of Kosi‐Gandak interfan, north Bihar Plains, India

机译：评估在印度北比哈德克斯（Kosi-Gandak Interfan）的水压湿地（Kaabar Tal）中的连通性评估

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Abstract >Landscape elements respond to the processes acting on them, and this response connects with neighboring landscape units. The propagation, superposition, and interference of these responses are functions of the connectivity among the landscape units. Such landscape units are referred to as ‘Connectivity Response Units’ or CRUs that are in turn influenced by topography and landuse/landcover (LULC). The CRUs are obtained by the application of diffusion‐kernel based smoothing technique over the connectivity potential maps. A framework has been designed using the CRUs to understand the impacts of changing LULC on the connectivity structure in a relatively flat terrain under pre‐ and post‐monsoon scenarios. The proposed framework has been applied to a water‐stressed wetland occurring in an interfan setting in north Bihar plains, eastern India. It has also been demonstrated that CRUs can be used as a viable option for understanding the seasonal and temporal dynamics of connectivity structure in and around such wetlands and for guiding a rehabilitation strategy for such fragile ecosystems. Copyright ? 2017 John Wiley & Sons, Ltd. </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 XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”> <title type =“main”>抽象</ title> >横向元素响应作用于它们的进程，此响应与相邻横向单元连接。这些响应的传播，叠加和干扰是横向单元之间的连接的函数。这种景观单元被称为“连接响应单元”或CRU，其又受到地形和土地使用/ Landcover（LULC）影响。通过在连接潜在地图上应用基于扩散 - 内核的平滑技术来获得CRU。使用CRU设计了一个框架，了解在预先和季风方案中，在季风方案和后季后地场景下的相对平坦的地形中改变LULC变化的影响。拟议的框架已应用于印度东部北比尔平原的互连湿地发生的湿地。还证明了CRU可以用作理解这种湿地和周围的连通结构的季节和时间动态，并为这种脆弱的生态系统引导康复策略的季节性和时间动态。版权？ 2017年John Wiley＆amp; SONS，LTD。</ 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-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2017年第13期</span><b style="margin: 0 2px;">|</b><span>共15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=Singh Manudeo&option=202" target="_blank" rel="nofollow">Singh Manudeo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tandon Sampat K.&option=202" target="_blank" rel="nofollow">Tandon Sampat K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sinha Rajiv&option=202" target="_blank" rel="nofollow">Sinha Rajiv;</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>Department of Earth SciencesIndian Institute of Technology KanpurKanpur India;</p> <p>Department of Earth SciencesIndian Institute of Technology KanpurKanpur India;</p> <p>Department of Earth SciencesIndian Institute of Technology KanpurKanpur India;</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/163.html" title="地球物理学">地球物理学;</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=hydrological connectivity&option=203" rel="nofollow">hydrological connectivity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=connectivity response unit&option=203" rel="nofollow">connectivity response unit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=diffusion‐kernel based smoothing&option=203" rel="nofollow">diffusion‐kernel based smoothing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=alluvial wetlands&option=203" rel="nofollow">alluvial wetlands;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ganga plains&option=203" rel="nofollow">Ganga plains;</a> </p> <div class="translation"> 机译：水文连接;连接响应单元;基于扩散基于平滑的平滑;发生湿地;Ganga Plains; 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