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<br />In a number of economic and environmental issues, <br />some say, resources shared in common with few <br />restrictions are ultimately overused, as all partici- <br />pants are encouraged to maximize their use and no <br />participant has an incentive to consider the long-term <br />consequence of overuse. When the consequences <br />of over-pumping are severe for at least five years, <br />groundwater users can ask the court to "adjudicate," <br />define the rights that various entities have to ground- <br />water in the basin. The court can limit pumping to <br />the "safe yield" of the basin. which is the amount at <br />water that can be pumped without causing un- <br />desirable results to the aquifer. Through adjudIca- <br />tions, the courts can assign specific water rights to <br />water users and can compel the cooperation of <br />pumpers who might otherwise refuse to limit their <br />pumping. Watermasters often are assigned to ensure <br />that pumping conforms to the limits defined by the <br />adjudication. Litigation, however, IS time-consuming <br />and costly, in part because it is difficult to determine <br />all of the pumpers and their historic pumping <br />amounts. <br /> <br /> <br />WHAT THE COURTS HAVE SAID <br /> <br />One of the first controversies that had to be resolved <br />was how far water had to seep under a streambed <br />before It stopped being surface water and started <br />being groundwater. Early in the 20th century. the <br />courts divided groundwater into two broad catego- <br />ries - subsurface flow and percolating groundwater. <br /> <br />Subsurface flow is water moving through the sands <br />and gravels under or next to a stream channel. Sub. <br />surface flow is considered to be part of the stream <br />and subject to the <br />same riparian and <br />appropriative rights <br />that guide the use of <br />the stream itself. As <br />a result. the pumping <br />of subsurface flows, <br />while constituting <br />only a small portion <br />of the groundwater <br />in California, is regu- <br />lated by the State <br />Board. <br /> <br />Percolating water is <br />often defined as <br />water moving through <br />the soil by gravity <br />along the path of <br />least resistance. In <br />California, the term <br />covers the vast <br />majority of ground- <br />water. And with few <br />exceptions, the State <br />Board does not gov- <br />ern the use of percolating water. The legal distinc- <br />tion, however, is a sharper line than the hydrological <br />distinction. As a result, determining when water fits <br />into each category has been a source of controversy <br />in some water disputes. <br /> <br /> <br />I <br />I <br />'--- <br /> <br />__ __J <br /> <br />A dOlllestic lI'el/ ill <br />Wood/mul. 1I'l1icl1 relies <br />solely 011 grollJ/(hl'ateJ: <br />Grol/lldWOler is tile sole <br />source (~ll\"atcr supply <br />for more thall 9 <br />fIIil/ioll Californians. <br /> <br />A 1903 ruling established that for landowners over- <br />lying an aquifer, each property had a "correlative" or <br />co-equal right to a "Just and fair proportion" of the <br />resource. That standard is different than the one <br />governing surface water rights, which limits the <br />amount of water that can be used and establishes a <br />priority system for allocating water during shortages. <br />Correlative rights. while acknowledging that <br />shortages may occur, only require that all property <br />owners share equally in the resource until it is <br />exhausted - irrespective of the consequences. <br /> <br />8 <br /> <br />Through this process. the courts have adjudicated <br />16 basins in California. One of them is near the <br />Oregon border. the Smith River system. where <br />groundwater was adjudicated to help resolve a <br />surface water controversy. Another is the Santa <br />Margarita River watershed. where the court did not <br />limit pumping. The remaining 14 adjudications have <br />all been in southern California, where development <br />pressures quickly overwhelmed limited aquifers: <br />Central Basin, West Coast Basin. Upper Los Ange- <br />les River Area (San Fernando). Raymond Basin. <br />Main San Gabriel Basin, Cummings Basin. <br />Tehachapi Basin. Warren Valley Basin. Chino Basin, <br />Cucamonga Basin, Puente Basin, Mojave River <br />Basin, the San Bernardino Basin and the Santa <br />Paula Basin. <br /> <br />In adjudicating these basins, early court decisions <br />affirmed the concept of correlative rights and estab- <br />lished two other kinds of groundwater entitlements. <br />If water is available after the needs of property <br />owners have been satisfied. the courts have allowed <br />for water to be pumped and exported from those <br />lands by an appropriative user. The courts ruled that <br />among appropriators, the first to pump has the first <br />entitlement to export water. When it is necessary to <br />limit pumping by appropriative users, those limits <br />should be based on how much the users pumped <br />historically. Creating limits based on past use. <br />however, provides an incentive to pump more water <br />