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<oembed><version>1.0</version><provider_name>Institute of Oceanography, NTU</provider_name><provider_url>https://www.oc.ntu.edu.tw/en/</provider_url><title>Temporal variations of submarine groundwater discharge into a tide-dominated coastal wetland (Gaomei Wetland, Western Taiwan) indicated by radon and radium Isotopes - Institute of Oceanography, NTU</title><type>rich</type><width>600</width><height>338</height><html>&lt;blockquote class="wp-embedded-content" data-secret="TnJjHHnh1G"&gt;&lt;a href="https://www.oc.ntu.edu.tw/en/research-highlights/15996/"&gt;Temporal variations of submarine groundwater discharge into a tide-dominated coastal wetland (Gaomei Wetland, Western Taiwan) indicated by radon and radium Isotopes&lt;/a&gt;&lt;/blockquote&gt;&lt;iframe sandbox="allow-scripts" security="restricted" src="https://www.oc.ntu.edu.tw/en/research-highlights/15996/embed/#?secret=TnJjHHnh1G" width="600" height="338" title="&#x201C;Temporal variations of submarine groundwater discharge into a tide-dominated coastal wetland (Gaomei Wetland, Western Taiwan) indicated by radon and radium Isotopes&#x201D; &#x2014; Institute of Oceanography, NTU" data-secret="TnJjHHnh1G" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"&gt;&lt;/iframe&gt;&lt;script&gt;
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</html><description>Although not as obvious as surface runoffs, groundwater flowing across the seabed into the ocean, so-called Submarine Groundwater Discharge (SGD), indeed occurs in many coastal areas. SGD, comprising of terrestrial fresh groundwater flowing from the aquifers and seawater infiltrating through the permeable sediments, is regarded as a significant process of hydrological cycle and play an [&hellip;]</description><thumbnail_url>https://www.oc.ntu.edu.tw/wp-content/uploads/2020/08/image0011.png</thumbnail_url></oembed>
