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VOLUME XX, ISSUE 2 <br />June 2006 <br />'ATER RESOURCES <br />DE*RTMENT OF NATURAL <br />Dick Wolfe, P.E., Assistant State Engineer <br />The material in this article is based <br />on the study report prepared by S.S. <br />Papadopulos and Associates, Inc. <br />(SSPA), 2006, entitled " Coalbed <br />Methane Stream Depletion Assess- <br />ment Study — Northern San Juan <br />Basin, Colorado'. A copy of the <br />study is available for viewing at the <br />Division of Water Resources website <br />at: www.water.state.co.us. This <br />study was a joint effort by the <br />Colorado Oil and Gas Conservation <br />Commission ( COGCC), the Colo- <br />rado Geological Survey (CGS), the <br />Colorado Division of Water Re- <br />sources (DWR) and SSPA. <br />The purpose of this study was to <br />develop a quantitative assessment of <br />the levels of stream depletion or <br />reduction in formation outflows <br />(spring flows or flowing stream <br />systems gaining from contact with <br />formations) that may be occurring as <br />a result of the removal of water by <br />coalbed methane (CBM) wells. This <br />water historically has been disposed <br />by one or more methods, including <br />re- injection into deep formations, <br />discharge to the surface stream <br />system, and ponding /evaporation. <br />The concern has been raised that the <br />removal of ground water from <br />aquifers that may be tributary to the <br />surface stream system could be <br />resulting in stream depletions or a <br />reduction in spring flows and /or <br />formation outflows (accretions) that <br />are of a magnitude sufficient to <br />cause injury to senior water rights <br />holders on over - appropriated stream <br />systems. <br />This study sought to develop a <br />reliable assessment as to the levels <br />of depletion, definition of the areas <br />where CBM is ongoing that might <br />be classified as non - tributary, <br />definition of any potential corre- <br />lations of water quality, geology, <br />aquifer geometry, or formation/ <br />well depth that could lead to <br />general guidelines about the <br />potential for stream depletion that <br />would be useful in either prompt- <br />ing or avoiding more detailed <br />studies, and development of <br />recommendations for further data <br />collection or investigations. <br />The San Juan Basin is a produc- <br />9 <br />5 <br />tive source of CBM. In conjunc- <br />tion with the production of CBM, <br />is the production of water. A <br />COGCC database of monthly <br />CBM gas and water production <br />for all wells in the basin from <br />1985 indicates that, through July <br />2005, more than 4.2 trillion cubic <br />feet of gas and 400 million <br />barrels (52,000 acre -feet) of <br />water have been produced from <br />CBM wells in the San Juan Basin <br />in Colorado. The annual rate of <br />gas production is continuing to <br />rise and is projected to be above <br />450 billion cubic feet in 2005. <br />Annual water production peaked <br />in 1993 at nearly 34 million <br />barrels (4,300 acre -feet) and has <br />been relatively steady at close to <br />23 million barrels (3,000 acre - <br />feet) since. <br />CBM in the San Juan Basin is <br />produced primarily from the <br />coals in the late Cretaceous <br />Fruitland Formation. The Fruit- <br />land Formation and the adjacent <br />Pictured Cliffs Sandstone, infor- <br />mally referred to as the Fruitland - <br />Pictured Cliffs aquifer, are the <br />source of the CBM produced <br />water. The Fruitland- Pictured <br />Cliffs aquifer is bounded to the <br />north by a well - delineated out- <br />crop of its component formations. <br />(Continued on page 2) <br />