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SU0004304_SSNL
EnvironmentalHealth
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2600 - Land Use Program
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PA-0200146
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SU0004304_SSNL
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Last modified
11/19/2024 3:46:23 PM
Creation date
9/9/2019 10:27:57 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0004304
PE
2632
FACILITY_NAME
PA-0200146
STREET_NUMBER
9301
Direction
W
STREET_NAME
STATE ROUTE 12
City
LODI
ENTERED_DATE
5/17/2004 12:00:00 AM
SITE_LOCATION
9301 W HWY 12
RECEIVED_DATE
1/24/2003 12:00:00 AM
QC Status
Approved
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SJGOV\sballwahn
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\MIGRATIONS\T\HWY 12\9301\PA-0200146\SU0004304\NL STDY.PDF
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EHD - Public
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.� than 7)with a high base exchange(more than 50% ize an equivalent amount of acid and would be a <br /> calcium).This is typical for soils forming in an and good choice when potassium fertilization is neces- <br /> environment. Groundwater is also predominately sary and the soil is too acidic. <br /> .� alkaline as groundwater chemistry reflects the <br /> chemistry of surrounding soil and parent rock. Water Infiltration: Low salinity water(less than <br /> Severe soil acidification(to pH 5 or lower)is not a 0.5 dS/m and especially below 0.2 dS/m) tends to <br /> widespread problem in San Joaquin Valley vine- leach surface soils free of soluble minerals and <br /> yards,but it is becoming more and more common, salts, especially calcium, reducing their strong <br /> particularly with drip irrigation.Acidic soils(below stabilizing influence on soil aggregates and soil <br /> pH 5 to 5.5)can impact vine growth,yield,and fruit structure. Without salts and without calcium, the <br /> quality. soil disperses,and the dispersed finer soil particles <br /> fill many of the smaller pore spaces, sealing the <br /> Vineyards at risk of acidulation are those vineyards surface and greatly reducing the rate at which water <br /> on soils with low buffering capacity, irrigated infiltrates the soil surface. Very low salinity water <br /> primarily with canal water,and fertilized with acid- (less than Ecw=0.2 dS/m)almost invariably results <br /> forming fertilizers. In Tulare County, soil types at in water infiltration problems. <br /> greatest risk are sandy soils associated with alluvial <br /> fans and with no free lime in the profile(Cajon and Slow water infiltration is a serious problem in some <br /> Tujunga series); also, highly weathered, east side vineyards, especially with drip irrigation. <br /> noncalcareous hardpan soils developed on old With drip irrigation,irrigation water must infiltrate <br /> alluvial fans and terraces (San Joaquin and Exeter a small surface area to satisfy the vines' <br /> series). Canal water is low in salt(25 to 50 ppm of evapotranspiration needs. If infiltration is inade- <br /> total soluble salts)and calcium,has no neutralizing quate, puddling occurs and the vines will show <br /> power, and can dissolve and remove calcium water stress even though more than adequate <br /> carbonate from the soil,potentially lowering pH.In amounts of water have been applied. Waterlogging <br /> contrast, typical groundwater on the east side of near the surface kills vine roots,and the inadequate <br /> Tulare County contains moderate levels of salinity distribution of water in the profile limits the volume <br /> (250 to 500 ppm).Much of the pump water actually of the root zone effectively wetted making matters <br /> adds calcium carbonate(200 to 600 pounds of lime worse. <br /> per acre-foot) which can neutralize an equivalent <br /> input of acid. Gypsum and other soluble compounds can double <br /> or triple the infiltration rate over that of untreated <br /> Acid input to the soil comes from a variety of low-salt water. Gypsum is the amendment most <br /> + sources.Most significant is the use of ammoniacal often used, but other calcium sources are also <br /> fertilizers which produce H" (acid) when ammo- effective.Calcium nitrate and CAN-17 are effective <br /> nium (NH4*) is oxidized to nitrate (NOS). The but can only be used in limited amounts: the nitro- <br /> acidification potential of nitrogen fertilizer should gen applied must not exceed the vines'requirement <br /> be considered when applied to acid soils. This is for nitrogen fertilizer. <br /> shown in the table as the amount of pure lime <br /> (pounds calcium carbonate)needed to neutralize the Calcium must be added continuously to the irriga- <br /> equivalent of 1 pound of nitrogen for each fertilizer tion water in order to maximize infiltration. When <br /> material.Materials with a high acidification poten- application of gypsum to irrigation water is discon- <br /> L tial should be avoided on soils with pH of less than tinued, infiltration rates drop to near control levels <br /> 6. Instead, use compounds with an alkaline soil within a few weeks. The occasional addition of <br /> reaction that raise pH such as calcium nitrate. calcium to the irrigation water is not effective in <br /> LPotassium carbonate is very soluble and can easily maintaining infiltration rates. To optimize infiltra- <br /> be applied through the drip system. It will neutral- tion rate using canal water, finely ground gypsum <br /> LGrape Notes # January 2002 # Page 2 <br />
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