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Surface Water <br /> Surface water samples were last retrieved on March 4, 2009. All concentrations of monitoring and <br /> field parameters were below established concentration limits where the limits could be <br /> determined. <br /> HISTORICAL TIME SERIES PLOTS AND STIFF DIAGRAMS <br /> Constituents not detected are plotted at a value of half their respective detection limits in the <br /> Historical Time Series Plots(Appendix F). Outliers were included in the plots as directed by <br /> RWQCB staff. <br /> Stiff diagrams are submitted annually with the second semester and annual report. The stiff <br /> diagrams submitted for the first and second semesters indicate a calcium-bicarbonate water type <br /> since these ions have the highest concentrations in the six wells (Appendix F). The water type is <br /> similar in all wells as indicated by similarity in concentrations of the various constituents and the <br /> similarity in diagram shapes. This similarity indicates that the groundwater is not impacted as it <br /> moves under the landfill. The shapes of the diagrams between the first and second semesters are <br /> also very similar indicating that the general groundwater quality has not changed throughout the <br /> year, which is also an indication of no impact from the landfill. <br /> PROGRESS OF EVAPOTRANSPIRATION COVER VEGETATION <br /> The purpose of the evapotranspiration cover is to capture rain water during the wet months, <br /> AML <br /> 1p allowing the vegetation growing on that cover to remove the water from the soil during the dry <br /> months. <br /> For all practical purposes, the evapotranspirative(ET) cover was established in December 2008 <br /> when soil in areas without sufficient growth were amended, fertilized and reseeded. Growth in the <br /> spring of 2009 was successful. Weeds were pulled in early May 2009 to reduce intrusion of wind- <br /> blown seeds into the preferred species. In June 2009, growth was between three and four feet <br /> high. <br /> Early rains of November 2009 allowed the germination of annual seeds and revitalizing perennial <br /> grass roots. <br /> A key component of this method is the root structure established. Perennial plants, such as purple <br /> needle grass and California Brome grow deep roots that can gather moisture from deep within the <br /> closure soil layer. In contrast, annual species, such as rye grass, produce shallow roots. The <br /> survival"strategy"of annual grasses is to produce a significant quantity of seed in the spring <br /> before dying. This seed then germinates in the rains of the following winter. <br /> For the purposes of maximizing evapotranspiration, deep-rooted perennial species are much <br /> preferred over shallow-rooted annual species. <br /> The County is contemplating allowing grazing by sheep during the spring of 2010,timed to reduce <br /> the annual grass stalk and seed crop, thereby enhancing the proliferation of perennial species. <br /> Foothill Sanitary Landfill 15 Department of Public Works/Solid Waste <br /> 2"d Semester and Annual 2009 Groundwater Monitoring County of San Joaquin—January 31,2010 <br />