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Kansas Geological Survey, Open-file Report 2017-4


Testimony--Rolfe Mandel, Kansas Geological Survey, to House Water and Environment Committee on HB2272, 9 February 2017

by Rolfe Mandel

KGS Open File Report 2017-4
The document is also available as an Adobe Acrobat PDF file, 37 kb.

Mr. Chairman, members of the Committee, thank you for the opportunity to appear before you in regards to HB2272. I am Rolfe Mandel, interim director of the Kansas Geological Survey, University of Kansas. The Kansas Geological Survey is a research and service division of KU, and is charged by statute with studying and reporting information about the state's geologic resources, which includes water. The KGS has no regulatory authority and does not take positions on natural resource issues, including this bill.

However, I do endorse concepts embedded within the bill, of collaboration between water researchers, water agencies and stakeholders to identify water priorities, and the data and studies necessary to address them. Water data, analysis and models inform policy makers, managers, and water users. It provides a strong basis for decision makers to evaluate options and add confidence to their decisions.

The Kansas Geological Survey provides support on several levels:

Basic Data:

Transparency and Accessibility:

Support for decision makers: The breadth and depth of Kansas' data on the High Plains aquifer allows for evaluations not otherwise possible. For example:

An appendix is provided that itemizes many of our current studies that directly support program and management decisions.

Lastly, I'd like to note the maps and charts attached. We were asked to provide the committee information that illustrates High Plains aquifer water use to water levels. The first map shows the water level change over the past 10 years, and the second map shows the density of water use for the same period. As might be expected, the larger declines are where the greater withdrawals occur. The Groundwater Management Districts are shown on the maps.

Interpolated water-level change, High Plains Aquifer, average 2004-2006 to average 2014-2016.

The next page illustrates water level use with average water level change within each Groundwater Management District. The variation in annual water use is primarily driven by the weather; crops require more irrigation in hot dry seasons than cool, wet seasons.

Density distribution (5-mi radius) of the average reported ground-water use, 2005-2015, in the Kansas High Plains Aquifer region.

The last page illustrates the relationship between water use and water level change. Applying the best-fit line, the KGS researchers identified the water use reduction needed in each groundwater management district to achieve roughly stable groundwater levels, allowing for annual fluctuations.

Reported groundwater use (solid line - left y-axis) and average water-level change (dashed line - right y-axis) through time for the GMDs.  These data are used for the sustainability assessments in the following figures.

Results of sustainability assessments for Kansas GMDs.

Reference

Fenichhel, Eli P., and others, 2015, Measuring the value of groundwater and other forms of natural capital: Proceedings of the National Academy of Sciences, v. 113, no. 9, p. 2382-2387

Appendix

Current and Potential Impact of Kansas Geological Survey's Research and Data on Kansas Water Resource Policy, Management, and Planning

Ogallala-High Plains Aquifer Assessment

Kansas River Alluvial Aquifer Assessment (proposed program)

Groundwater-Surface Water Modeling in the Lower Republican River Basin

Groundwater Assessment for Missouri River Regional Planning Area

Arkansas River Water Quality Assessment in Southwest Kansas

Aquifer Site Characterization

Groundwater Contamination Analysis


Kansas Geological Survey
Placed online Feb. 13, 2017
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