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ARCHIVED REPORTS_XR0008213
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0504943
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ARCHIVED REPORTS_XR0008213
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Last modified
6/18/2020 12:53:26 PM
Creation date
6/18/2020 12:16:05 PM
Metadata
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EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0008213
RECORD_ID
PR0504943
PE
2951
FACILITY_ID
FA0004032
FACILITY_NAME
AMERICAN MOULDING & MILLWORK (FRMR)
STREET_NUMBER
2801
STREET_NAME
WEST
STREET_TYPE
LN
City
STOCKTON
Zip
95204
APN
11709001
CURRENT_STATUS
02
SITE_LOCATION
2801 WEST LN
P_LOCATION
99
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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The choice of the deficiency of 5 tons of calcium carbonate equivalent per <br /> 1000 tons of material as the division between toxic and non-toxic material . <br /> obviously is arbitrary. However, when applied to the large number of samples <br /> studied during the past several years of minesoil research at West Virginia <br /> University, it corresponds to other supporting laboratory information about <br /> these samples as well as to extensive field experiences with minesoils <br /> developing in the different rock types. If rock or soil samples were defined <br /> to be toxic at much lower calcium carbonate equivalent deficiencies than 5 <br /> tons per 1000 tons, we would be declaring many of our native soils to be <br /> toxic. On the other hand, with deficiencies much greater than 5 tone per <br /> 1000 tons, toxic concentrations of plant-available aluminum and pH values <br /> below 4.0 often develop rapidly. <br /> Rock type is incorporated with the acid-base account because it is useful <br /> to categorize the materials which comprise coal overburdens. Knowledge of <br /> the rock types can provide an estimate of the texture and base status of <br /> a future minesoil, as well as stability of rock fragments. For example, <br /> sandstones containing moderate amounts of pyrite and lacking sufficient <br /> neutralizers become active acid producers when exposed to the atmosphere. <br /> The properties previously discussed are represented graphically in Figure 1. <br /> There are two zones of acid--toxic materials (the 16.2 to 17.1 m and the 20.7 <br /> to 21.6 m depths) indicated by pH values of less than 4.0. Both zones <br /> contain enough sulfur to continue to overwhelm the small amount of neutra- <br /> - liters present. - Thus, these materials have the potential for remaining <br /> acid-toxic unless large amounts of neutralizers (50 and 80 tons calcium <br /> carbonate equivalent per 1000 tons of material, respectively) are added. <br /> In addition, there is a zone of potentially toxic matefial at a depth of • <br /> 13.4 to 16.2 m and two zones below the 23 m depth (underlying the first <br /> coal add overlying the bottom coal) , which are defined by a calcium carbonate <br /> deficiency of more than 5 tons per 1000 tons of material even though the pH <br /> is above 4.0. <br /> Non-toxic zones, which exhibit varying amounts of excess neutralizers, exist <br /> -T-- _-from-the-surface-to--a=depth-of=13.4-m, from-the17:1to--21-m-depth,—and -- <br /> from the 24.4 to 25.4 m depth. These materials can be removed and replaced <br /> - in sequential-order, -selectively blended before-replacement,-or totally <br /> blended before replacement. Other methods of handling the overburden <br /> materials would include utilization of the limestone, after crushing, as a <br /> source of neutralizers to be -blended-with the potentially toxic materials. <br /> The acid-base accounting method provides a useful tool for evaluating over- <br /> burdens in the humid areas of the United States, since it is useless to look <br /> for plant toxicities from elements such as aluminum, boron, etc. , until the <br /> acid problem is-eliminated.- <br /> 4 <br /> seliminated. 4 <br />
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