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	<title>Science at Sea &#187; coring</title>
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	<link>http://scienceatsea.oceanography.dal.ca</link>
	<description>Reports from research missions at sea</description>
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		<title>Filling the MUC with muck!</title>
		<link>http://scienceatsea.oceanography.dal.ca/2013/05/251/</link>
		<comments>http://scienceatsea.oceanography.dal.ca/2013/05/251/#comments</comments>
		<pubDate>Sat, 18 May 2013 11:34:52 +0000</pubDate>
		<dc:creator>Liz Kerrigan</dc:creator>
				<category><![CDATA[Instruments]]></category>
		<category><![CDATA[Pacific]]></category>
		<category><![CDATA[RV Sonne]]></category>
		<category><![CDATA[coring]]></category>
		<category><![CDATA[geoscience]]></category>
		<category><![CDATA[instruments]]></category>
		<category><![CDATA[MUC]]></category>
		<category><![CDATA[mud]]></category>
		<category><![CDATA[Multi-Corer]]></category>

		<guid isPermaLink="false">http://scienceatsea.oceanography.dal.ca/?p=251</guid>
		<description><![CDATA[Often times ocean scientists are interested in what’s happening below the water, on the ocean floor. One instrument used to sample deep-water ocean sediments is a Multi-Corer or MUC. What’s cool about a MUC is that it keeps the sediment-water interface intact. The ability of the MUC to preserve the most recent (top) sediment layer [...]]]></description>
				<content:encoded><![CDATA[<p>Often times ocean scientists are interested in what’s happening below the water, on the ocean floor. One instrument used to sample deep-water ocean sediments is a Multi-Corer or MUC. What’s cool about a MUC is that it keeps the sediment-water interface intact. The ability of the MUC to preserve the most recent (top) sediment layer makes it unique from gravity or piston corers, which essentially sacrifice the top sediment layers for increased penetration depths and longer cores. We send the MUC instrument, which can be seen in the pictures below, to the bottom of the ocean using a winch. Once the instrument has hit the bottom, the tubes are slowly driven into the sediment and sealed before it is hauled back up to the surface. Using a MUC we can see exactly what’s happening at the seafloor surface even though its been pulled up 4000 m from the bottom of the ocean! In the end, we get about 30-40 cm of sediment from the ocean floor in each MUC tube.</p>
<p>Just by looking at the cores and feeling the mud we can identify boundary and redox layers as well as differences in grain size. But to find out more, we take samples of these cores for future analysis.</p>
<p>If you like getting muddy, then you’ll love sediment work! To sub-sample these cores we remove a tube filled with sediment from the MUC and place it on a stand. Once the core is on the stand we can move it down centimeter-by-centimeter revealing 1 cm of sediment at a time and scraping it off. For the first few really wet centimeters we put the sub-samples in a glass jar. After that we fill syringes with sediment every few centimeters until we get to the end of the core. Since we’re dealing with mud, and not water, we have to cut the tip off the syringe and then push it into the sediment core to get our sub-sample. Once we’ve taken these sub-samples we can look at things like nitrogen isotopes, sediment grain size, and multiple other parameters. Ultimately, this information from the sediment helps us reveal a little bit more about what’s happening in the ocean above, both today and in the past.</p>
<p>&nbsp;</p>
<div id="attachment_252" class="wp-caption alignnone" style="width: 235px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0138.jpg"><img class="size-medium wp-image-252" alt="An empty MUC on the ship before deployment" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0138-225x300.jpg" width="225" height="300" /></a><p class="wp-caption-text">An empty MUC on the ship before deployment</p></div>
<div id="attachment_253" class="wp-caption alignnone" style="width: 310px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0184.jpg"><img class="size-medium wp-image-253" alt="The MUC coming up!" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0184-300x225.jpg" width="300" height="225" /></a><p class="wp-caption-text">The MUC coming up!</p></div>
<div id="attachment_254" class="wp-caption alignnone" style="width: 310px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0196.jpg"><img class="size-medium wp-image-254" alt="Cores filled with sediment" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0196-300x225.jpg" width="300" height="225" /></a><p class="wp-caption-text">Cores filled with sediment</p></div>
<div id="attachment_255" class="wp-caption alignnone" style="width: 310px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0406.jpg"><img class="size-medium wp-image-255" alt="Tip-less syringe to be filled with sediment" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_0406-300x225.jpg" width="300" height="225" /></a><p class="wp-caption-text">Tip-less syringe to be filled with sediment</p></div>
<div id="attachment_256" class="wp-caption alignnone" style="width: 235px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_1834.jpg"><img class="size-medium wp-image-256" alt="Putting the core on to the core stand" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_1834-225x300.jpg" width="225" height="300" /></a><p class="wp-caption-text">Putting the core on to the core stand</p></div>
<div id="attachment_257" class="wp-caption alignnone" style="width: 310px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_1838.jpg"><img class="size-medium wp-image-257" alt="Sampling the first few muddy centimeters" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_1838-300x225.jpg" width="300" height="225" /></a><p class="wp-caption-text">Sampling the first few muddy centimeters</p></div>
<p>&nbsp;</p>
<div id="attachment_258" class="wp-caption alignnone" style="width: 310px"><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_1840.jpg"><img class="size-medium wp-image-258" alt="Sampling with the tip-less syringe" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/IMG_1840-300x225.jpg" width="300" height="225" /></a><p class="wp-caption-text">Sampling with the tip-less syringe</p></div>
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		</item>
		<item>
		<title>Tropical Pacific geoscience</title>
		<link>http://scienceatsea.oceanography.dal.ca/2013/05/tropical-pacific-geoscience/</link>
		<comments>http://scienceatsea.oceanography.dal.ca/2013/05/tropical-pacific-geoscience/#comments</comments>
		<pubDate>Tue, 14 May 2013 18:52:54 +0000</pubDate>
		<dc:creator>Laura deGelleke</dc:creator>
				<category><![CDATA[Pacific]]></category>
		<category><![CDATA[RV Sonne]]></category>
		<category><![CDATA[coring]]></category>
		<category><![CDATA[geoscience]]></category>
		<category><![CDATA[mud]]></category>

		<guid isPermaLink="false">http://scienceatsea.oceanography.dal.ca/?p=210</guid>
		<description><![CDATA[It&#8217;s always nice to &#8220;have&#8221; to go to sea in the tropics, especially when it&#8217;s 10 C and rainy back in Halifax. Dal MSc student Liz Kerrigan and her supervisor, Prof. Markus Kienast, are currently sailing aboard the 98 m German research vessel RV Sonne between Kaohsiung in Taiwan and Jayapura in the easternmost corner [...]]]></description>
				<content:encoded><![CDATA[<p>It&#8217;s always nice to &#8220;have&#8221; to go to sea in the tropics, especially when it&#8217;s 10 C and rainy back in Halifax. Dal MSc student Liz Kerrigan and her supervisor, Prof. Markus Kienast, are currently sailing aboard the 98 m German research vessel RV Sonne between Kaohsiung in Taiwan and Jayapura in the easternmost corner of Indonesia.</p>
<p>The research work being conducted is, in general, geoscience. What does this mean to student scientists onboard? More often than not it means getting muddy. Inevitably on a geoscience cruise, some amount of mud will be brought up from the seafloor and processed. The fate of the mud varies and depends on who wants it and for what, which often determines how it was retrieved from seafloor. Processing onboard can involve splitting, cutting, sub-sampling mud/porewater, logging, and <em>always</em> labeling. You can see Liz sub-sampling a <a href="http://scienceatsea.oceanography.dal.ca/2013/05/multi-corer/">multi-corer</a> tube in 1 cm slices and using a modified syringe in the pictures below.</p>
<p>Every now and then, crafty professors manage to escape the daily grind at the office and actually make it out on one of their cruises. Markus gets points for craftiness here: not only has he managed to make it out on a cruise, he&#8217;s selected a tropical location and is keeping his hands clean&#8230; or at least mud-free! You can see Markus sampling seawater from niskin bottles in a CTD <a href="http://scienceatsea.oceanography.dal.ca/2013/04/the-oceanographic-rosette/">rosette</a> in the pictures below. He is hoping water column profiles of nutrient concentrations and the isotopic composition of nitrate will help explain water mass distributions in the study area, and aid in ground-truthing the interpretation of paleoceanographic proxy records.</p>
<p>This cruise (SO-228) combines three cruise proposals for research in the Western Pacific. <a href="http://www.marum.de/Page13223.html">Read more about the proposed research and cruise plans on the MARUM Bremen University website</a>.</p>
<p><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/sonne_starboard.png"><img class="alignnone size-full wp-image-218" alt="sonne_starboard" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/sonne_starboard.png" width="300" height="225" /></a></p>
<p><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/liz2.png"><img class="alignnone size-full wp-image-214" alt="liz2" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/liz2.png" width="400" height="300" /></a></p>
<p><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/liz1.png"><img class="alignnone size-full wp-image-213" alt="liz1" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/liz1.png" width="400" height="300" /></a></p>
<p><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/markus2.png"><img class="alignnone size-full wp-image-216" alt="markus2" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/markus2.png" width="300" height="400" /></a></p>
<p><a href="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/markus1.png"><img class="alignnone size-full wp-image-215" alt="markus1" src="http://scienceatsea.oceanography.dal.ca/wp-content/uploads/2013/05/markus1.png" width="400" height="300" /></a></p>
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		</item>
		<item>
		<title>Sampling mud flats despite large tides!</title>
		<link>http://scienceatsea.oceanography.dal.ca/2012/07/sampling-mud-flats-despite-large-tides/</link>
		<comments>http://scienceatsea.oceanography.dal.ca/2012/07/sampling-mud-flats-despite-large-tides/#comments</comments>
		<pubDate>Mon, 09 Jul 2012 21:00:27 +0000</pubDate>
		<dc:creator>Jessica Carriere-Garwood</dc:creator>
				<category><![CDATA[Bay of Fundy]]></category>
		<category><![CDATA[Field work]]></category>
		<category><![CDATA[coring]]></category>
		<category><![CDATA[field work]]></category>
		<category><![CDATA[mud]]></category>

		<guid isPermaLink="false">http://www.phys.ocean.dal.ca/scienceatsea/?p=127</guid>
		<description><![CDATA[You might have heard that the Bay of Fundy is home of the largest tides in the world, reaching heights above 16 m. As part of my Master&#8217;s project, I needed to obtain sediment cores from mud flats that experience such huge tides. Our usual hand coring technique consists of using a simple device to [...]]]></description>
				<content:encoded><![CDATA[<p>You might have heard that the Bay of Fundy is home of the largest tides in the world, reaching heights above 16 m. As part of my Master&#8217;s project, I needed to obtain sediment cores from mud flats that experience such huge tides. Our usual hand coring technique consists of using a simple device to push plastic barrels into water-covered sediment, seal them, and bring them out. It is usually carried out from a small ship or even by simply walking into the water (see left picture below). This technique, however, was completely useless in the Bay of Fundy! Instead, we set up two semi-permanent pier that allowed us to walk over the mud without disturbing it and manually dig out our cores at low tide (see right picture below).</p>
<p>As you can see, my supervisor Paul Hill is not one to shy away from heavy work!</p>
<p>&nbsp;</p>
<div id="attachment_136" class="wp-caption alignleft" style="width: 280px"><a href="http://www.phys.ocean.dal.ca/scienceatsea/wp-content/uploads/2013/03/P1000735.jpg"><img class=" wp-image-136 " alt="Usual hand coring technique." src="http://www.phys.ocean.dal.ca/scienceatsea/wp-content/uploads/2013/03/P1000735-300x225.jpg" width="270" height="203" /></a><p class="wp-caption-text">Usual hand coring technique.</p></div>
<div id="attachment_128" class="wp-caption alignright" style="width: 225px"><a href="http://www.phys.ocean.dal.ca/scienceatsea/wp-content/uploads/2013/03/DSC00549-e1363823314449.jpg"><img class=" wp-image-128 " alt="Hand coring in the Bay of Fundy" src="http://www.phys.ocean.dal.ca/scienceatsea/wp-content/uploads/2013/03/DSC00549-e1363823314449-239x300.jpg" width="215" height="270" /></a><p class="wp-caption-text">Hand coring in the Bay of Fundy</p></div>
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		</item>
		<item>
		<title>Grand Banks/Flemish Cap geoscience</title>
		<link>http://scienceatsea.oceanography.dal.ca/2011/09/seismics-and-sediment-coring-on-the-grand-banks-and-in-flemish-pass/</link>
		<comments>http://scienceatsea.oceanography.dal.ca/2011/09/seismics-and-sediment-coring-on-the-grand-banks-and-in-flemish-pass/#comments</comments>
		<pubDate>Thu, 15 Sep 2011 17:42:17 +0000</pubDate>
		<dc:creator>Laura deGelleke</dc:creator>
				<category><![CDATA[Atlantic]]></category>
		<category><![CDATA[CCGS Hudson]]></category>
		<category><![CDATA[coring]]></category>
		<category><![CDATA[geoscience]]></category>

		<guid isPermaLink="false">http://www.phys.ocean.dal.ca/scienceatsea/?p=21</guid>
		<description><![CDATA[In August 2011, I had the opportunity to sail on the CCGS Hudson for a seismic and sediment coring expedition to the Grand Banks and Flemish Cap. We collected over 60 piston cores in 15 days and made seismic transects all night! &#8230; and I made some great friends and got screeched in while we [...]]]></description>
				<content:encoded><![CDATA[<p>In August 2011, I had the opportunity to sail on the CCGS Hudson for a seismic and sediment coring expedition to the Grand Banks and Flemish Cap. We collected over 60 piston cores in 15 days and made seismic transects all night! &#8230; and I made some great friends and got screeched in while we stopped in St. John&#8217;s, Newfoundland for a crew change <img src='http://scienceatsea.oceanography.dal.ca/wp-includes/images/smilies/icon_wink.gif' alt=';)' class='wp-smiley' /> </p>
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		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Sediment coring off the Galápagos Islands</title>
		<link>http://scienceatsea.oceanography.dal.ca/2009/04/galapagos-islands/</link>
		<comments>http://scienceatsea.oceanography.dal.ca/2009/04/galapagos-islands/#comments</comments>
		<pubDate>Mon, 20 Apr 2009 17:10:32 +0000</pubDate>
		<dc:creator>Laura deGelleke</dc:creator>
				<category><![CDATA[Pacific]]></category>
		<category><![CDATA[RV Knorr]]></category>
		<category><![CDATA[coring]]></category>

		<guid isPermaLink="false">http://www.phys.ocean.dal.ca/scienceatsea/?p=12</guid>
		<description><![CDATA[While doing my master&#8217;s in oceanography at Dal, I had the opportunity to sail on the R/V Knorr for a coring expedition targeting the Galápagos platform and the Peruvian Margin. We departed from and returned to port at Puerto Ayora on Santa Cruz Island in the Galápagos, Ecuador. In addition to being on one of [...]]]></description>
				<content:encoded><![CDATA[<p>While doing my master&#8217;s in oceanography at Dal, I had the opportunity to sail on the <a title="WHOI R/V Knorr" href="http://www.whoi.edu/page.do?pid=8157">R/V Knorr</a> for a coring expedition targeting the Galápagos platform and the Peruvian Margin. We departed from and returned to port at Puerto Ayora on Santa Cruz Island in the Galápagos, Ecuador.</p>
<p>In addition to being on one of the best sediment coring vessels in the world, I got to stay at the <a title="Charles Darwin Research Foundation" href="http://www.darwinfoundation.org/english/pages/index.php">Charles Darwin Research Foundation</a> in Puerto Ayora where I swam with endemic marine iguanas and tried to fall asleep to the surprisingly loud sound of mating Galápagos giant tortoises.</p>
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