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L Deep Percolation (Rainfall Recharge).The Nitrate Loading Study used a value of 17.01 <br /> inches per year as the assumed average annual deep percolation(i.e.,rainfall recharge)for <br /> use in the water-nitrogen mass balance analysis. On page 5,the report explains that this was <br /> determined from average monthly precipitation and evapotranspiration rates for the area. <br /> However,this is not reflected in the data and calculations presented in Appendix B. <br /> Appendix B presents monthly CIMIS data for the 2018-2019 water year,which was an <br /> unusually wet rainfall year,and not indicative of average rainfall conditions.It is also not <br /> clear from these data how the value of 17.01 inches deep percolation was calculated. <br /> I prepared an independent water balance calculation using average monthly rainfall data for <br /> Lodi and published average monthly evapotranspiration(ETo)data for CIMIS Zone 12, <br /> which is attached. By my analysis for a"hypothetical'development site in the area,I <br /> calculated an average annual rainfall recharge/deep percolation value of 8.79 inches/year, <br /> considerably less than the 17.01 inches assumed in the Dillon&Murphy study.Note that in <br /> my water balance calculation I include an adjustment for actual evapotranspiration based on <br /> typical land surface conditions.This is important,since the published ETo values represent <br /> the estimated ET(water demand)for lawns and other uniform turf areas,which are generally <br /> much higher than the ET for most types of vegetation,e.g.,trees,shrubs,ground cover, <br /> perennials,etc. The ET associated with buildings and paved areas is even less(e.g.,<10%of <br /> ETo). Since rural development sites will commonly have a mix of vegetation and landscape <br /> features,the water balance-recharge calculations will be more accurate by adjusting the ETo <br /> (downward),according to the mix of developed landscape conditions. In my attached <br /> example I used hypothetical values,not necessarily those for the 7151 Peltier site,which <br /> Dillon&Murphy would be able to estimate more accurately. <br /> Substituting my deep percolation value of 8.79 inches/year along with the other Dillon& <br /> Murphy assumptions,gives a resultant nitrate-nitrogen estimate of 9.69 mg-N/L for the <br /> projected wastewater flow of 1.240 gpd. Using 17.01 inches deep percolation,Dillon& <br /> Murphy calculated a resultant value of 9.89 mg-N/L for a potential flow of 2,480 gpd,which <br /> underestimates the potential nitrate impact at this artificially higher level of wastewater flow. <br /> However,since 2,480 gpd is double the actual wastewater flow projection,this can be <br /> ignored. Since my attached calculations and resultant nitrogen value of 9.89 mg N/L are for <br /> hypothetical site development-landscape conditions,I recommend that Dillon&Murphy <br /> consider these suggested changes to the water balance—deep percolation methodology,and <br /> submit revised project calculations for final review. <br /> 2. Wastewater Flow and Nitrate Concentration.In the Hantzsche/Finnemore methodology, <br /> the values for wastewater flow and nitrogen concentration are meant to approximate long- <br /> term average conditions. The wastewater flow assumptions by Dillon&Murphy are <br /> representative of maximLun daily flow,commordy used for system design,and over-estimate <br /> the average wastewater discharge for the property. On the other hand,the wastewater effluent <br /> nitrate concentration assumption of 35 mg-N/L is on the low side. However taken together, <br /> the over- and under-estimations cancel each other to produce a reasonable estimate of total <br /> wastewater mass nitrogen loading,which is the relevant factor. For future reference,a <br /> typical per person mass nitrogen loading rate of 13 to 14 g/person/day can be used as a check <br /> 2 <br />