Study excerpts:
“The Washington State Department of Ecology has the responsibility for issuing permits to drill wells for the withdrawal and use of groundwater in the state.” (foreword)
“[I]n many cases, withdrawals exceed recharge with the result that water levels decline and pumping depths and costs increase. Early developers object because their costs are increased as a result, at least in part, of the action of others. Eventually the aquifer may be exhausted or the pumping depth become so great that it is no longer economically feasible to withdraw water.” (p.1)
“Instances of groundwater mining are now beginning to occur in Washington and with them have come some of the characteristic problems of recedence of static water levels and consequent increase in pumping depths and costs.” (p. 1)
“[A]n economy that is growing on the basis of groundwater mining may face painful decline if and when withdrawal is no longer economically feasible.” (p. 2)
“The current concern about groundwater problems is by no means the first attention given the topic in the state of Washington. The statutes of the state of Washington contain provisions regarding groundwater. Most important to these deliberations are the sections dealing with the regulations of withdrawals. The statutes provide that “No permit shall be granted for the develop or withdrawal of public ground waters beyond the capacity of the underground bed or formation in the given basin, district, or locality to yield such water within a reasonable or feasible pumping lift in a case of pumping developments, or within a reasonable of feasible reduction of pressure in the case of artesian developments. (90.44.070)” (pp. 2-3)
“[T]he Ritzville-Odessa area of eastern Washington was used as a typical area for testing the concepts involved. This area was selected because critical groundwater problems already exist here and because much information of the necessary type was already available. … The Ritzville-Odessa area is in the eastern Columbia Basin area of east-central Washington. The area has an average annual precipitation of about 10 inches. Most of the area is farmed by dryland methods, following a wheat/summer fallow regime.” (pp. 4-5)
“Since 1963, there has been a large and rapid increase in irrigation in the area using practices associated with groundwater pumped from deep wells. In the 5 years from 1963 to 1967, pumpage increases nearly four-fold in the Odessa-Lind portion of the model area. The rapid and widespread increase in pumpage has caused accelerated and alarming groundwater level declines in many parts of the area. This, in turn, has prompted the State’s water management agency to close a large part of the area to further appropriation while an intensive study can be made of the whole problem.” (p. 5)
“It now appears, however, that surface water importation is physically possible but economically marginal at this time and not likely in less than two decades. Even if surface water is imported it is likely that a demand for groundwater will remain. ... [I]n this area, it does not appear that groundwater irrigation developments will have either the ability to pay for the imported water or the capability of inducing the location in the area of industry having that ability.” (pp. 90-91)
“In the Columbia Basin basalt aquifers recharge is generally believed to be virtually nonexistent.” (p. 99)
“The results of this study indicate substantial gains may be realized from irrigation, even though the water may be obtained by groundwater mining. Even in an area where development had not already occurred, the apparent opportunity for sizeable economic gain would make “no development” highly unpopular. On the other hand the arguments for absolute preservation have merit. For one, there is no evidence to indicate that use of the water for irrigation is benefiting society members. There is no shortage of wheat, potatoes, beans, peas, or any of the commodities being produced with the water in question. Production of these crops in the study area merely displaces production in other regions of the state or outside the state. It would b easy to show that all of the production resulting from irrigation in the study area could be produced elsewhere without exploiting a scarce stock resource. Exploitation is occurring simply because the present cost and policy structure makes it slightly more profitable to produce the crop with mined groundwater reserves.” (p.99)
“The results show that substantial net return can be realized by irrigation of currently dry-farmed lands in the Odessa-Ritzville area. Costs of water, at current pumping depths (200-500 feet) are not prohibitively high for intensive cropping with high value crops, such as potatoes, or for judicious supplemental irrigation on dryland wheat. Eventually, if pumping depths reach 700-1,000 feet (depending on crops produced and type of farm) irrigation would be unprofitable.” (p.104)
“A second concept of control seeks to regulate withdrawals so that the decline of the aquifer does not exceed a specified rate per year. Alternatively, regulation may be imposed to assure an economic life of the aquifer of a least some specified number of years. This approach may be combined with a determination of economic pumping lift to define the depth at which the aquifer will have no further economic value. The rate or period of time should be chosen so as to permit full amortization of sunk investments.” (pp. 105-106)