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1988-04-11_PERMIT FILE - C1981008A (15)
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1988-04-11_PERMIT FILE - C1981008A (15)
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Last modified
1/5/2021 12:09:42 PM
Creation date
4/19/2012 10:23:47 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981008A
IBM Index Class Name
PERMIT FILE
Doc Date
4/11/1988
Doc Name
Probable Hydrologic Consequences
Section_Exhibit Name
Tab 17
Media Type
D
Archive
Yes
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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is most commonly associated with the top soil layer and the sandstone units. The highest <br /> pH, 8.9 occurs in #882E in the lowest part of the sandstone directly over the upper Dakota <br /> coal 's thin encapsulating shale. <br /> Acid-base potential (ABP) ranges from -48 to 239. The more acidic ( 0 ABP) material <br /> occurs most commonly above the upper Dakota coal . The more basic (+0 ABP) material most <br /> commonly occurs in the upper 10 ft of overburden material or in the soil layer. Core <br /> #871E contains both of the extreme ABP numbers where the +239 ABP is found in the upper 3 <br /> ft of soil , and the -48 ABP if found directly above the 0.5 ft thick shale layer <br /> encapsulating the upper Dakota coal . Pyrite occurs within the coals, in the few feet of <br /> material surrounding the coals, and occasionally in isolated pockets higher in the <br /> overburden sequence. The percent pyritic sulfur calculated for the overburden ranges from <br /> .03 to 1.6. <br /> Interburden Material . The interburden is defined as all material above the lower <br /> Dakota coal seam up to and including the upper Dakota coal seam. It is divided into three <br /> separate units, Units 2, 3, and 4; Unit 2 consists of the upper Dakota coal and <br /> encapsulating shale or sandstone layers. Unit 4 consists of only the shale layer directly <br /> above the lower Dakota coal, and Unit 3 comprises the remaining material which is most <br /> commonly a thick sandstone. <br /> The thickness of the interburden remains fairly constant throughout the study area varying <br /> from 17 ft in the southwestern part to about 14 ft in the central and eastern part. The <br /> thickness of upper Dakota coal varies from 7.3 ft in the west to less than 0.5 ft in the <br /> east (Table 17-7). <br /> Core #870E contains naturally-occurring low concentrations of Cu, Pb, Zn, Ni, Mg, B, Se, <br /> Mo, Fe and Mn. Analyses of soil pH show a range in Unit 2 from 3.5 to 8.9, in Unit 3 from <br /> 6.0 to 9.0, and in Unit 4 from 4.2 to 7.9. The most acidic material occurs in #871E (3.5) <br /> within the shales surrounding the upper Dakota coal . The shale above the coal has a pH of <br /> 3.6 and below the coal a pH of 3.5, with a total thickness including the coal of about <br /> 7.1 ft. For the entire Nucla East area this is the most acidic material that is found. <br /> The most basic material occurs in #882E Unit 3 with a pH of 9.0 and thickness of 2.9 ft <br /> and in Unit 2 with a pH of 8.9 and thickness of 2.8 ft. Again, these anomalously high pH <br /> values are found in the encapsulating shales or sandstones of the upper Dakota coal . <br /> 17-35 Revised 04/11/88 <br />
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