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SU0003923 SSNL
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SU0003923 SSNL
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Entry Properties
Last modified
5/7/2020 11:30:20 AM
Creation date
9/9/2019 9:02:34 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0003923
PE
2622
FACILITY_NAME
PA-0300125
STREET_NUMBER
517
Direction
S
STREET_NAME
REID
STREET_TYPE
AVE
City
LINDEN
ENTERED_DATE
5/11/2004 12:00:00 AM
SITE_LOCATION
517 S REID AVE
RECEIVED_DATE
4/11/2003 12:00:00 AM
QC Status
Approved
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SJGOV\rtan
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\MIGRATIONS\R\REID\517\PA-0300125\SU0003923\SS STDY.PDF
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EHD - Public
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pan Joaquin County, California 15 <br /> ;tockton and similar soils, and 13 percent components soils formed in alluvium derived from mi d rock <br /> ,f minor extent. sources. Levees have been construct to control <br /> Jacktone soils are in basins. They are 20 to 40 floodwater. They are used in conju ion with drainage <br /> fiches deep to a cemented hardpan and are somewhat ditches and pumps to reduce wet ss. <br /> poorly drained. Slope ranges from 0 to 2 percent. This unit makes up about 4 cent of the survey <br /> ypically, the surface layer is fine textured. The subsoil area. It is about 43 percent and and similar soils, 30 <br /> moderately fine textured. The shrink-swell potential is percent Devries and similar ils, 18 percent <br /> igh Depth to the water table is more than 5 feet. The Rioblancho and similar soi , and 9 percent components <br /> oils are subject to rare flooding. of minor extent. <br /> Hollenbeck soils are on basin rims. They are 40 to 60 Guard soils are very eep and poorly drained. Slope <br /> fiches deep to a cemented hardpan and are moderately ranges from 0 to 2 p ent. Typically, the surface layer <br /> cell drained. Slope ranges from 0 to 2 percent. and underlying ma ial are moderately fine textured. <br /> typically, the surface layer is fine textured. The subsoil The soils are cal eous throughout and have weakly <br /> is fine textured and moderately fine textured. The cemented layer elow a depth of 15 inches. A high <br /> shrink-swell potential is high. The soils are subject to water table is a depth of 1.5 to 3.0 feet in most <br /> rare flooding. areas, but i as been lowered to a depth of more than <br /> Stockton soils are in basins. They are 40 to 60 5.0 feet in reas where water from drainage ditches is <br /> inches deep to a cemented hardpan and are somewhat pumped ' to the adjacent sloughs and rivers. The soils <br /> poorly drained. Slope ranges from 0 to 2 percent. are su ct to rare flooding. <br /> Typically, the surface layer is fine textured. The subsoil D ries soils are 20 to 40 inches deep to a cementad- <br /> Is fine textured and moderately fine textured. The ha an and are somewhat poorly drained. Slope <br /> Shrink-swell potential is high. Depth to the water table is r ges from 0 to 2 percent. Typically, the surface la r <br /> more than 5 feet. The soils are subject to rare flooding. and subsoil are moderately coarse textured. Dept <br /> Minor in this unit are the Archerdale soils and Urban the water table is more than 5 feet. The soils ar <br /> ind. Archerdale soils are well drained and are on the subject to rare flooding. <br /> higher fan terraces. Urban land is covered by streets, Rioblancho soils are 20 to 40 inches deep a <br /> parking lots, buildings, and other structures. cemented hardpan and are somewhat poor drained. <br /> Areas of this unit are used mainly as irrigated Slope ranges from 0 to 2 percent. Typica , the surface <br /> Cropland or pasture. A few areas are used for homesite layer is moderately fine textured. The s soil is <br /> development. The major soils are suited to irrigated moderately fine textured and modera coarse <br /> crops and pasture. Limitations include slow permeability textured. Depth to the water table i ore than 6 feet. <br /> and depth to the hardpan. In most areas the growth of The soils are subject to rare floo " g. <br /> perennial, deep-rooted crops is limited by the hardpan. Minor in this unit are the Dell soils and Urban land. <br /> Where this unit is used for homesite development, Dello soils are very poorly dr ed and are in the lower <br /> the main limitations are slow permeability, a high shrink- landscape positions. Urban d is covered by streets, <br /> swell potential, low strength, and depth to the hardpan. parking lots, buildings, an ther structures. <br /> -fhe main hazard is rare flooding. Onsite sewage Areas of this unit are ed mainly as irrigated <br /> disposal is difficult because of the slow permeability and cropland or pasture. A w areas are used for homesite <br /> the hardpan. Structural damage can result from the high development. The m r soils are suited to irrigated <br /> shrink-swell potential and low strength. These crops and pasture. mitations include depth to the <br /> limitations should be considered when foundations, hardpan in the D ries and Rioblancho soils and a low <br /> (puildings, and roads are designed. Dikes and channels available water pacity in the Devries soils. Guard <br /> That have outlets for floodwater can protect buildings soils are limite by depth to the high water table, slow <br /> - rom flooding. permeability, nd weakly cemented layers. The growth <br /> of most per nial, deep-rooted crops is limited by the <br /> Guard-Devries-Rioblancho high wate able or the hardpan. <br /> Wher his unit is used for homesite development, <br /> 'oorly drained and somewhat poorly ed, moderately the m . limitations are depth to the high water table <br /> oarse textured and moderately fin tured soils that and t hardpan. The main hazard is rare flooding. <br /> re moderately dlbeendrain <br /> hardpan or are very Ons' sewage disposal is difficult because of depth to <br /> Peep and that hamost areas, on th ardpan and the high water table and may cause <br /> ,asin rims c tamination of the ground water. Dikes and channels <br /> This map unit long the eastern at have outlets for floodwater can protect buildings <br /> dge of the Sacruin Delta area. The rom flooding. <br />
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