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Last modified
9/26/2011 8:53:06 AM
Creation date
6/10/2008 3:56:22 PM
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Decision Support Systems
Title
Geological Logging to Determine Construction, Contributing Zones, and Appropriate Use of Water Levels Measured in Confined-Aquifer Network Wells, San Luis Valley, Colorado, 1998-2000
Description
USGS Water-Resources Investigations Report 02-4058
Decision Support - Doc Type
Report
Date
7/5/2005
DSS Category
Groundwater
DSS
Rio Grande
Basin
Rio Grande
Contract/PO #
C153863
Grant Type
Non-Reimbursable
Bill Number
HB98-1189, SB99-173
Prepared By
HRS
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ANALYSIS OF GEOPHYSICAL LOGS <br />Well flow recorded on the logs is the flow that <br />passes through the measurement section of the flow- <br />Geophysical logging and analysis of the driller?s <br />meter. A flow-diverting skirt can be used to concen- <br />and geophysical logs were performed to provide better <br />trate all flow in a well through the measurement <br />information about wells in the CAWN. The logs <br />section of the flowmeter when flows are small. Flow- <br />provided information on (1) construction of the wells, <br />diverting skirts were not used during this study <br />(2) lithologies or lithologic zones open to the wells <br />because (1) the diameter of most wells in the CAWN is <br />through saw- or torch-cut slots or stainless-steel <br />too large to successfully use a skirt, (2) discharges <br />screens or in uncased portions of boreholes, and <br />under free-flowing conditions were too large to allow <br />(3) inflow or outflow zones providing water to the <br />the use of a skirt, (3) the annular space of many wells <br />wells. The logs recorded in each of the wells were <br />appeared to lack gravel or sand packing that poten- <br />plotted side-by-side on graphs. This method of plot- <br />tially could allow flow to bypass the casing and occur <br />ting the logs allows data at particular depths to be <br />in the annular space, (4) the tops of some well liners <br />correlated between the logs. The logs plotted in the <br />were bent, or (5) the inside of most wells is rough, <br />figures for each well do not start at zero on the charts <br />reducing the effectiveness of the skirt. <br />because it was necessary to lower the logging tools <br />Flowmeter data plotted in the figures showing <br />10?20 ft into the well before the logs could begin to be <br />all well logs for a well are shown in gallons per minute <br />recorded. The upper, unlogged 10?20 ft of the wells <br />or feet per minute, as measured through the measure- <br />typically does not yield additional information that <br />ment section of the flowmeter. Stationary and trolling <br />would change the analyses that are presented in this <br />flowmeter measurements were selected for presenta- <br />report. <br />tion in the figures, based on which logs showed clearly <br />In the description of the logs for each well, <br />definable information about flow zones within the <br />reference is made to features of the well casing or the <br />wells. These flow measurements are used to identify <br />generalized lithologic layers that occur at depth. All <br />zones of inflow rather than to quantify the amount of <br />depths given in the well descriptions are depths below <br />flow from each of the zones contributing flow to wells. <br />land surface. <br />Thus, the flow logs show differences or changes in <br />In most cases, the flowmeter logs are the <br />flow within each well as the flowmeter was advanced <br />primary logs used to indicate zones of inflow to the <br />upward or downward in each well to record logs or to <br />wells. Specific-conductance and temperature logs are <br />obtain stationary measurements. <br />useful in indicating inflow to the wells, but these logs <br />Most of the figures showing trolling flowmeter <br />are supplementary to the flowmeter logs. Specific- <br />logs contain a reference line called the ?tool-velocity <br />conductance and temperature logs are the primary logs <br />line.? This line shows the response the flowmeter <br />used to define zones of inflow to wells when no flow- <br />would record if there was no flow in a well and the <br />meter logs are available for a particular well. <br />only velocity was that induced by the downhole move- <br />ment of the flowmeter. When the trolling logs are Thirty-two wells in the CAWN were logged; <br />recorded in shut-in wells and if there is no flow in the 10 other wells were not logged because (1) known <br />well among flow zones (interzonal flow), the flow- well construction indicated that the zone of inflow to <br />meter log should match the tool-velocity line. Quanti- the well was very narrow, (2) well owners denied <br />tatively, the velocity of water through the flowmeter is USGS access to the wells, (3) too much oil was <br />equal to the velocity at a point minus the downhole floating on the surface of the water column, (4) wells <br />velocity of the flowmeter during logging (usually were obstructed, or (5) well construction prevented <br />20 ft/min). The tool-velocity line is not shown on access for logging. A complete set of geophysical logs <br />graphs with a large range in flow rates because the line consisted of video, caliper, water specific-conduc- <br />at 20 ft/min approximately coincides with the left-axis tance, water-temperature, and free-flowing or pumped <br />of the graph in those cases and is of little use in the and shut-in or static water-column well-flow logs. <br />analysis. The tool-velocity line is also not shown for Logging was attempted in several wells but the logs <br />wells in which the trolling rate was less than 20 ft/min yielded insufficient data for analysis, and several wells <br />due to the shallowness of the well or due to the need to were constructed in a way that prevented complete <br />slow the flowmeter down to get past irregularities in logging. Table 1 lists the availability of logs for each <br />the casing or borehole. well in the CAWN. <br />ANALYSIS OF GEOPHYSICAL LOGS <br />7 <br />
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