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<br /> <br /> <br />000299 <br /> <br />For Irrigated agriculture to be sustainable, <br />salt balance must be achieved so that <br />salts added equals salts removed. <br /> <br />(Jacobsen and Adams 1958). Declining <br />yields and shifts toward cultivating <br />more salt-tolerant crops paralleled in- <br />creasing salinity. Meanwhile, cities <br />were devastated by yield reductions, <br />and the resulting inability to meet the <br />food needs of a considerable super- <br />structure of priests, admi'nistrators, <br />merchants, soldiers and craftsmen. <br />The southern part of the alluvial plain <br />never recovered and many great <br />Sumerian cities dwindled into villages <br />or were left in ruins. <br />The story of Mesopotamia is an- <br />cient, but it could be repeated in Cali- <br />fornia. Approximately 4.5 million <br />acres of irrigated croplcmd - prima~ <br />rily on the West Side of the San <br />Joaquin Valley - are affected in Cali- <br />fornia by saline soils or saline irriga- <br />tion wnter. Predictions vary for the <br />rate at which salinization is occurring, <br />but tens of thousands of productive <br />agricultural acres are clearly at risk <br />(CAST 1996). <br />Irrigation in sem.iarid regions such <br />as CCllifornia invariably lends to soil <br />saUnization unless mitigated by ap- <br />propriate management. . <br />Three factors contribute to <br />salinization: <br />. All irrigation waters contain dis- <br />solved salts, with concentrations <br />varying considerably according to <br />the origin of the water. <br />. Plants extract negligible amounts of <br />s.1lt, so the soil solution becomes <br />concentrated as water is removed <br />by evapotranspiration. <br /> <br />. Water quantities in excess- <br />of evapotranspiration <br />must be appliedto.leach <br />salts beyond 'the root zone <br />to prevent reduced crop <br />yields. <br />Saline water leaving a <br />plant's root zone may also <br />percolate down until it <br />reaches groundwater, result~ <br />ing in degraded ,vater qual- <br />ity. Or, it may migrate and <br />seepto a lower land surface. <br />When the iatter occurs, the seepage <br />area becomes salin!~.~d as water ' <br />evaporates and the slI1ts concentrate. <br />Water percolating below the root <br />zone can cause the water table to rise. <br />Without the ability to leach salt from <br />the root zone, concentrations rise to <br />detrimental levels, Additionally, high <br />water content interferes with the oxy. <br />gen supply to the roots, resulting in <br />further crop damage. When a water <br />table reaches the root zones, yields can <br />be sustained only by draining to re- <br />move excess salt, water and other dis: <br />solved compounds. <br />Sustainable irrigated agriculture in <br />areas where salinity poses a problem <br />can be achieved by adhering to two <br />basic principles: (1) salt balance, de- <br />fined as salts removed must equal <br />salts added, must be achieved, and (2) <br />systems must be installed to remove <br />drainage water and di"solved salts <br />when the water table reaches the root <br />zone. These principles can be applied <br />on a field, farm or regional basis. <br />Most surface'wate" supplies in Cali- <br />fornia are relatively low in salinity. Inw <br />deed, some irrigation waters derived <br />predominantly from snowmelt and <br />rainwater from the Sierra Nevada con~ <br />tain extremely low concentrations of <br />dissolved salts. In contrast., irrigation <br />water from the Colorado River is the <br />most saline. Irrigation wa ter pumped <br />from wells varies considerably in sa- <br />linity, depending upon the geologic <br />strata from which it is extracted. <br />Although salinity is a concern in <br />isolated areas, the Imperial Valley and <br />the western San Joaquin Valley are of <br /> <br />44 CALIFORNIA AGRICULTURE. VOLUME 54. NUMBER 2 <br /> <br />particular concern to agricultural pro- <br />ductivity, each with its own uniqlle set <br />of features. <br /> <br />Imperial Valley and Salton Sea <br /> <br />The Imperial Valley, located in <br />southeast California, has a hot desert <br />climate, allowing some agricultural <br />productivity year-round. Very little <br />precipitation occurs, and the evapo- <br />transpiration rate is high. An elaborate <br />irrigation and drainage system has <br />been implemented in the Imperial Val- <br />ley. Crops are irrigated with Colorado <br />River water and drainage water is <br />then discharged into the Salton Sea, <br />which is fed predominantly by this <br />source. The 3S-mile-long, lS-mile-wide <br />sea initially came into existence when, <br />at the turn of the 20thcentury, Colo- <br />rado River waters were diverted to the <br />flood-prone region for agriculture. An <br />irrigation <;:anal subsequently broke <br />and flooded the basin for 2 years. <br />While those waters would have e"apo- <br />rated years ago, the sea has since been <br />fed by drainage wafer, sewage and <br />other sources of water. With no outlet, <br />the Salton Sea's salinity has continu- <br />ously increased as the water evaporates. <br />The Salton Sea area serves as an im- <br />portant link on the Pacific Flyway, <br />North America's West Coast route for <br />migrating birds. The sea and adjacent <br />wetlands, rivers and croplands pro- <br />vide foraging and nesting for more <br /> <br />Agriculture has a history <br />of increasing productivity <br />per unit of land area so <br />that a growing human <br />population can be fed <br />without large expansions <br />of acreage. Attention <br />should now be directed to- <br />ward increasing wildlife <br />production per unit of <br />habitat area. <br />