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      <image:caption>Ian takes notes while Kate pauses from tailings sampling to pose for a snapshot!</image:caption>
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      <image:caption>ATLIN CARBONATE PLAYAS These playas are natural analogues for sequestration of carbon dioxide within Mg-carbonate minerals. Field sampling was conducted in 2004, 2005, 2007, 2011 and 2012. Check out publications by Power et al. (2007, 2009 and 2014).</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1483166599431-0WF15D7AHWKFNX1Q4DSE/Clinton+Ck+from+air.jpg</image:loc>
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      <image:caption>CLINTON CREEK ABANDONED MINE This abandoned mine host approximately 11 million tonnes of chrysotile mine wastes that have sequestered over 100,000 tonnes of carbon dioxide. Field campaigns were undertaken in 2004, 2005, 2007 and 2011. For more information, see publications by Power et al. (2010, 2011b) and Wilson et al. (2009).</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1483166657081-BFIZMX5C8RXDIT9TIHCA/IMG_6490.JPG</image:loc>
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      <image:caption>SWIFT CREEK SERPENTINITE LANDSLIDE This landslide is a natural analogue for the weathering of ultramafic mine tailings. The landslide advances several metres per year. The serpentine minerals have weathered to form magnesium carbonate and pyroaurite.</image:caption>
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      <image:caption>MOUNT KEITH NICKEL MINE This mine is located in Western Australia and produces approximately 11 million tonnes of mine tailings per year. Field sampling and laboratory analyses have revealed that approximately 40,000 tonnes of CO2 are sequestered each year. See publications by Power et al. (2011a), Bea et al. (2012) and Wilson et al. (2014).</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1483166355597-N8W06RYB2A80ASJ5Z1SJ/IMG_0085.JPG</image:loc>
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      <image:caption>DIAVIK DIAMOND MINE The Diavik mine is located in the Northwest Territories, Canada. These ultramafic mine tailings sequester carbon dioxide as they weather. See publications by Wilson et al. (2011) and Power et al. (2011a).</image:caption>
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      <image:caption>Atlin hydromagnesite-magnesite playas, viewed from a helicopter</image:caption>
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      <image:caption>Hydromagnesite plates with magnesite crystals wedged inbetween</image:caption>
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      <image:caption>Testing for magnesium carbonate using dilute HCl acid</image:caption>
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      <image:caption>The Trent Experimental Farm being prepared for planting and enhanced weathering trials.</image:caption>
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      <image:caption>Carbonate crust cementing Mount Keith mine tailings</image:caption>
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      <image:caption>Zivi measuring CO2 fluxes for her enhanced weathering plots.</image:caption>
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      <image:caption>Reactor vessels incubated in a carbonate wetland</image:caption>
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      <image:caption>Bacterium growing on mine wastes from Peru</image:caption>
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      <image:caption>The coarse residues and processing plant at the Venetia Diamond Mine, South Africa.</image:caption>
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      <image:caption>Kwon Rausis measuring CO2 fluxes for soils amended with wollastonite at the Trent Experimental Farm.</image:caption>
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      <image:caption>Calcium carbonate formed from the reaction of atmospheric CO2 with CaO powder.</image:caption>
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      <image:title>Home - Outdoor experiments</image:title>
      <image:caption>We’re interested in the weathering of rocks and minerals under real-world climatic conditions and at relatively large, metre-scales.</image:caption>
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      <image:title>Home - CO2 flux experiments</image:title>
      <image:caption>We’re using a range of equipment to measure CO2 fluxes under laboratory conditions where we can control important variables like moisture content.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1585095459471-CG4CPWIODLF48TADNGBC/DSC02584.JPG</image:loc>
      <image:title>Home - Column experiments</image:title>
      <image:caption>In the PowerGeolab, we use a variety of column experiments to study mineral weathering including the influence of organic amendments. These columns are held in an environmental chamber that controls temperature and relative humidity.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1585860012396-VR71GZLD9T4DKGCRL172/IMG_8392.JPG</image:loc>
      <image:title>Home - Batch reactors</image:title>
      <image:caption>We carry out a range of batch reactor experiments to understand cation release and CO2 mineralization. These reactors are being injected with 100% CO2 gas.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1584029921678-O0OE3NQ2VNVGCM9QRCGW/IMG_9997.JPG</image:loc>
      <image:title>Home - Cementation chambers</image:title>
      <image:caption>We use a variety of chambers, some are inexpensive Tupperware, others are more sophisticated including a CO2 incubator. Here, we’re examining the cementation and stabilization of tailings through carbonation.</image:caption>
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      <image:title>Home - Automated wet/dry cycling</image:title>
      <image:caption>In nature, wetting drives mineral dissolution, releasing cations such as Mg and Ca, while evaporation drives mineral precipitation. This experimental setup is able to do 4 wet/dry cycles per day.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1599524121238-L2I62MQSMRJVTTOH1X5L/0E1FB226-E204-417D-8342-EBB08E31CCC7.JPG</image:loc>
      <image:title>Home - D2 Phaser XRD</image:title>
      <image:caption>Mineral ID and quantification.</image:caption>
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      <image:title>Home - Parr stirred reactor</image:title>
      <image:caption>This reactor enables us to perform carbonation experiments at elevated temperatures and pressures.</image:caption>
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      <image:title>Home - Zeiss SteREO Discovery.V20 stereomicroscope</image:title>
      <image:caption>We use this microscope to examine tiny precipitates, image polished sections, and even do basic petrography.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1584028900246-V4J3R1YAWF0HEMB0MSND/DSC02200.JPG</image:loc>
      <image:title>Home - CO2 incubator and environmental chamber</image:title>
      <image:caption>We’re doing some really fun and interesting experiments using our CO2 incubator (left) and environmental chamber (right).</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1585094198539-DD961286TO0N73JVCKKW/DSC02591.JPG</image:loc>
      <image:title>Home - UIC Coulometer</image:title>
      <image:caption>This instrument measures the inorganic carbon content of solids and waters.</image:caption>
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      <image:title>Home - BET surface area analyzer</image:title>
      <image:caption>Surface area directly relates to mineral reactivity. We use a BET system to obtain accurate surface areas of tailings samples.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1584028884226-0JXRDCZEP2UU75JS44N7/195AE3B8-96E5-449F-AB72-ACB046BD49B2.JPG</image:loc>
      <image:title>Home - Spinning, weighing, and sonicating</image:title>
      <image:caption>We have plenty of equipment for sample preparation including balances, sonication and shaker baths, centrifuge, and fumehood.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1584028884528-Q4AR2D24LPM6ZOM335X9/IMG_0697.JPG</image:loc>
      <image:title>Home - Shake and sieve</image:title>
      <image:caption>We can determine particle sizes of tailings and sediments using our vibratory sieve shaker and a laser-based system.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1585094193129-FAMLZ41P0EUSGEDOKP2T/DSC02588.JPG</image:loc>
      <image:title>Home - Buehler EcoMet 30 polisher</image:title>
      <image:caption>We embed rock, tailings, and sediment samples into epoxy, polish, and examine using techniques such as scanning electron microscopy.</image:caption>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1640620278168-COHHVPRELA1MTY3H85UK/IMG_3162.JPG</image:loc>
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      <image:title>Home - Micronizing and pulverizing</image:title>
      <image:caption>In the PowerGeoLab, we use this micronizing mill to finely grind samples for mineralogical analyses by X-ray diffraction.</image:caption>
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    <image:image>
      <image:loc>https://images.squarespace-cdn.com/content/v1/5806b872ff7c50adea9acb25/1585094199686-C7SCTE7IVN21VDUI7VQ0/DSC02593.JPG</image:loc>
      <image:title>Home - FLSmidth Essa LM2 Pulverizing Mill</image:title>
      <image:caption>This mill is able to pulverize a kilogram of rock in less than a minute!</image:caption>
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