Experimental study of methane emission from lake seeps of Western Siberia permafrost zone
Authors: Krivenok Liudmila , Kazantsev Vladimir , Dvornikov Yury 
Published: March 2020

&lt;p&gt;Methane is one of the most potent greenhouse gases affecting climate change. According to different estimates, natural sources contribute 35&amp;#8211;50% to global CH&lt;sub&gt;4&lt;/sub&gt; emission. Among them, the third-biggest source is lakes emitting to the atmosphere 10&amp;#8211;50 TgCH&lt;sub&gt;4&lt;/sub&gt; per year [Anderson et al., 2010].&lt;/p&gt;&lt;p&gt;We have discovered two gas seeps during the summer 2019 field campaign within the lake near the Vas&amp;#8217;kiny Dachi research station (Central Yamal, Western Siberia). Measurement of the ebullition intensity in tenfold replicate and gas sampling were carried out using a bubble trap of the original design. The concentration of methane in seep gas was determined by a Crystal 5000.2 gas chromatograph with a flame ionization detector; each sample was diluted tenfold with air. We calculated the annual CH&lt;sub&gt;4&lt;/sub&gt; flux from seep to the atmosphere with the consideration of the intensity of seep ebullition and the methane concentration in gas equal during the year. To determine the potential source of the gas, we analyzed the isotopic composition of CH&lt;sub&gt;4&lt;/sub&gt; (&lt;em&gt;&amp;#948;&lt;/em&gt;&lt;sup&gt;13&lt;/sup&gt;C and &lt;em&gt;&amp;#948;&lt;/em&gt;D) by a Delta-V mass spectrometer.&lt;/p&gt;&lt;p&gt;The values (median &amp;#177; SD) of the gas ebullition are 175 &amp;#177; 26 mL/min and 127 &amp;#177; 10 mL/min for the first and second seeps respectively. The methane concentration in gas is 95&amp;#8211;100%. The intensity of CH&lt;sub&gt;4&lt;/sub&gt; emission from the first seep is 89.7 thousand L or 64 kg per year; from the second seep is 65.1 thousand L or 46.5 kg per year.&lt;/p&gt;&lt;p&gt;Analysis of the content of &lt;em&gt;&amp;#948;&lt;/em&gt;&lt;sup&gt;13&lt;/sup&gt;C and &lt;em&gt;&amp;#948;&lt;/em&gt;D isotopes in methane gives the following results.&lt;/p&gt;&lt;ul&gt;&lt;li&gt;For the first seep: &lt;em&gt;&amp;#948;&lt;/em&gt;&lt;sup&gt;13&lt;/sup&gt;C vs VPDB, &amp;#8240; = &amp;#8722;75.73, &lt;em&gt;&amp;#948;&lt;/em&gt;D vs VSMOW, &amp;#8240; = &amp;#8722;226.68.&lt;/li&gt;
&lt;li&gt;For the second seep: &lt;em&gt;&amp;#948;&lt;/em&gt;&lt;sup&gt;13&lt;/sup&gt;C vs VPDB, &amp;#8240; = &amp;#8722;76.97, &lt;em&gt;&amp;#948;&lt;/em&gt;D vs VSMOW, &amp;#8240; = &amp;#8722;222.31.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;According to the classification from [Whiticar, 1999], seep methane is of biogenic origin. Potentially, gas could migrate to the lake surface through sub-lake talik from the underlying geological horizon containing methane hydrates in self-preserved form as widely documented for this area [Chuvilin et al., 2000].&lt;/p&gt;&lt;p&gt;To summarize, lake seeps of the Western Siberia tundra zone have been studied as a source of the atmospheric methane for the first time. Considering the occurrence of methane hydrates withing permafrost in the study area, we describe a path of the CH&lt;sub&gt;4&lt;/sub&gt; release from decomposing gas hydrates into the atmosphere in the northern part of Western Siberia.&lt;/p&gt;&lt;p&gt;The study was partially supported by the RAS Program no. 20 and the state contract of the IAP RAS no. 075-03-2019-628.&lt;/p&gt;&lt;p&gt;References:&lt;/p&gt;&lt;p&gt;Anderson B., Bartlett K., Frolking S. et al. Methane and nitrous oxide emissions from natural sources. Washington: EPA. 2010. 194 p.&lt;/p&gt;&lt;p&gt;Chuvilin E.M., Yakushev V.S., Perlova E.V. Gas and possible gas hydrates in the permafrost of Bovanenkovo gas field, Yamal Peninsula, West Siberia // Polarforschung. 2000. V. 68. P. 215&amp;#8211;219.&lt;/p&gt;&lt;p&gt;Whiticar M. Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane. Chemical Geology. 1999. V. 161. P. 291&amp;#8211;314.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;