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SU0013451
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SU0013451
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Entry Properties
Last modified
5/17/2021 4:00:53 PM
Creation date
6/23/2020 11:17:55 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0013451
PE
2600
FACILITY_NAME
WC-90-1
STREET_NUMBER
2248
Direction
W
STREET_NAME
LAKE FOREST
STREET_TYPE
RD
City
ACAMPO
APN
00306001
ENTERED_DATE
6/17/2020 12:00:00 AM
SITE_LOCATION
2248 W LAKE FOREST RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\dsedra
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EHD - Public
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out that there is no linear relationship between the values and that a value of five may have <br /> several hundred times more phosphate content than a sample with a value of two (Woods <br /> 1975:23). <br /> Carbonates testing is an integral part of overall soil analysis. As middens develop, relatively <br /> high levels of calcium, nitrogen, carbon and phosphates accumulate in the soil. Carbonates <br /> result from interaction of calcium, carbon dioxide and phosphates. Age estimates for <br /> archaeological sites have been done using the depth of leached carbonates as a chronological <br /> control (Johnston 1975). One problem is that carbonates will not last long in acidic soil. <br /> Therefore, its use as a chronological indicator would be limited to sites with neutral or alkaline <br /> soils. <br /> The carbonates testing was made using a 2.5 g soil sample on a clean glass sheet. Three drops <br /> of muriatic acid were added to the sample and the observed reaction was subjectively recorded: <br /> None=O; Weak=l; Medium=2; Strong=3. <br /> The pH reading is an important component of soil analysis. In acid soils (pH values below 7.0) <br /> the phosphate is bound with iron and aluminum compounds. With alkaline soils (pH above 7.0), <br /> phosphate will usually be bound with calcium. These phosphate compounds will remain in the <br /> soil where deposited and generally are not subject to leaching. Of course, if the soil itself is <br /> disturbed, so is the phosphate. <br /> Studies have been done on the relationship of the soil pH to prehistoric sites. In general, the <br /> evidence shows that midden sites tend to have higher pH values than the surrounding soils. <br /> Although the initial occupation of the site would lower the pH because of humic and fulvic acids <br /> formed in the midden soil, after site abandonment the soil pH will increase as a result of <br /> complex chemical processes. <br /> The pH of each soil sample was determined using a Coleman Metrion IV pH meter. A volume <br /> of 25 ml of distilled water was added to a 20 g air-dried soil sample which had been screened <br /> through a #28 Tyler screen. The mixture was stirred every fifteen minutes for one hour prior <br /> to taking the pH reading. <br /> RESULTS <br /> Phosphate Testing <br /> Sixty-five samples were positive for phosphates and fifteen were negative. The highest PO, <br /> values, a 6.00 reading, were from depressions at site The four samples from <br /> depressions in off-site contexts in the vicinity of . were minimal (one was negative). Five <br /> of the fifteen negative readings came from boundary loci at site, The mean value <br /> of the sixty-five positive samples was 4.45 with a standard deviation of 1.22 and a variance of <br /> 1.49. <br /> A3-2 <br /> '1 <br />
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