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PERMFILE40232
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PERMFILE40232
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Entry Properties
Last modified
8/24/2016 10:43:14 PM
Creation date
11/20/2007 10:14:10 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2000032
IBM Index Class Name
Permit File
Doc Date
3/2/2000
Doc Name
SALES RECEIPT
From
DMG
To
MA CONCRETE CONSTRUCTION INC
Media Type
D
Archive
No
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ONTECHNIC <br />PORT <br />L <br />~I PTION R • <br />N <br />E <br />A <br />SOILS D <br />Mark AueCi^ <br />yap ~ So11 name and deeCriptSon <br />ymbol <br />Bc5 ~ Sagera silty clay loam, Saline, 0 [0 2 percent elopes <br />~ This wait ie poorly suited for irrigated trope. The <br />~ main limi[at ion is salinity. Most areas will need <br />~ extensive reclamation before trope can be grown. A <br />~ combirucion of leaching and drainage will he required <br />~ Eor reclamation. Salinity can be reduced by leaching <br />~ salts Erom the soil ue ing irrigation water that ie low <br />~ in content of salts. Tile drainage can be used to <br />~ lower the water table if a suitable outlet ie <br />available. intensive management ie required to reduce <br />the sal inky and ma incain soil productivity. <br />~ This unit cone iete of very deep, well drained soils on <br />~ old alluvial Eane and low terraces. These soils formed <br />in alluvium derived dominantly from Mancoe shale. The <br />~ surface layer ie silty clay loam 12 inches thick. The <br />upper 11 inches of the underlying material are silty <br />~ clay loam, and tae lower part to a depth of more than <br />~ 60 inches ie silty clay loam with few Eine gypsum <br />~ crystals. Permeability of Chia soil is slow. <br />~ Avaslable water capacity ie moderate. Effective <br />rooting depth ie 60 inches or more. RunafF ie slow, <br />~ and [he hazard of water erosion ie slight. Salta <br />~ moderately to severely affect plan[ adaptation, growth, <br />and water availability. Salta are al eo eeve rely <br />corrosive to concrete and unCreated steel pipe. <br />~ Capability Subcla ea BS; nonirzigaced <br />~ Capability class ification Se the grouping of soils to <br />~ show, in a general way, [heir suitability Eor moat <br />~ klnda of farming. It is a practical classification <br />~ based on limi cations of [he soils. Che risk of damage <br />when [hey are used, and the way they respond to <br />~ treatment. The soils are [lase if ied according co <br />degree and kind of permanent limi[aCion, but without <br />~ cone itle ra [ion of major and generally expensive <br />landEOrming that would change the elope, depth, or <br />~ other characterisci<s of the soils: without <br />~ considers [ion of possible unlikely major reel amat ion <br />~ projects. <br />
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