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INTRODUCTION <br />1.0 INTRODUCTION AND PROPOSED DEVELOPMENT <br />1.1 Description of Site: The project will consist of dividing a ten acre parcel into two five acre <br />parcels. The project is address is 11250 Micke Grove Rd., Lodi, CA 94240 and is zoned AL -5. <br />The project Assessor's Parcel Number is 059-140-57. <br />Description of proposed development: The purpose of this project is to subdivide the existing <br />ten acre parcel into two five acre parcels. Once the two parcels are created, the owner intends to <br />build some residential units. <br />1.2 Parcel vicinity location map: (See Appendix). <br />1.3 Site map: (See Appendix). <br />2.0 PAST, PRESENT, AND PROPOSED FUTURE USES OF THIS SITE <br />2.1 Discussion of Past, Present uses at the site to assess potential problems: The present owner, <br />Jack Kautz, has maintained the past use of the subject property as undeveloped. The future use of <br />this site is to develop the site by building residential units. <br />3.0 CHEMICAL AND PHYSCAL PROPERTIES OF SOIL <br />3.1 Description of existing chemical and physical properties of soil: For a description of the <br />chemical and physical properties of the soils underlying the site, refer to Section 5 of the Soil <br />Suitability Study prepared by Dillon & Murphy attached in the Appendix. <br />3.2 Description of the mass transport properties of the soils underlying the site with respect <br />to the nitrate and/or any other constituent of concern identified for the project site: The <br />results from the percolation test prepared by Dillon & Murphy have determined that the site is <br />permeable to a maximum depth of exploration of 42 inches. The soil type allows for infiltration <br />of water through the top soils. The infiltration rate will limit the natural treatment of the sites soils <br />as they drain rapidly from the surface layers. <br />The soil survey by US Department of Agriculture (USDA) indicates that there are two types of <br />soil types. The first is Jack Tone Clay and the other is Stockton Clay. Both soils have a top layer <br />of 0-34 inches that is composed of clay. The following layers in these soils are composed of more <br />indurated material past the initial 34 inch layer, reducing the transmissivity and should be <br />monitored. <br />4.0 GROUNDWATER ANALYSIS <br />4.1 Description of the depth to groundwater, seasonal fluctuations of groundwater depth, <br />directional flow and gradient: Description of depth to groundwater, seasonal fluctuations of <br />groundwater, directional flow and gradient are referred to in Section 4 of the Soil Suitability Study <br />prepared by Dillon & Murphy that is attached in the Appendix. <br />