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<br />amount of water that can be withdrawn by <br />an overlying owner exist, but there is at <br />least a theoretical limit. <br />5) Water in place beneath the soil is not <br />protected from exploitation by others and <br />hence, little incentive to conser'lle <br />groundwater exists. <br />6) There is no clear indication of when a <br />"shortage" exists that would bring the <br />"sharing" language common to many <br />groundwater cases into play. <br />7) Neither those entitled to share in times of <br />shortage nor the method of sharing are <br />delineated. <br />8) A landowner has no means by which he <br />can quantify the rights he has in ground- <br />water found beneath his lands. <br />9) Limits that might be imposed on private <br />exploitation of groundwater in order to <br />protect public rights to the resource are <br />not articulated. <br />10) Rights to use groundwater are not freely <br />transferable to higher and better uses. <br />11) The property rights system does not <br />provide for correlating groundwater and <br />surface water rights. <br />Whether these points constitute strengths or <br />weaknesses is, of course, largely a matter of <br />individual value judgment. <br />FOOTNOTES <br /> <br />,. 208 Neb. 703, 305 NW.2d 614, rev'd, 50 <br />U.S.L.W. 5115 (U.S. July 2, 1982). <br />2. The Nebraska Supreme Court has repeat- <br />edly held that overlying landowners are <br />"entitled to appropriate subterranean <br />waters" found under their land. See, e.g., <br />Olson v. Wahoo, 124 Neb. 802, 811, 248 <br />NW. 304, 308 (1933) (emphasis added). <br />124 Neb. 802, 248 NW. 304 (1933). <br />See generally Chapter One, supra. <br />124 Neb. at 811, 248 N.W. at 308. <br />The groundwater right would thus be an- <br />alogous to common law riparian surface <br />water rights. Such rights are not acquired by <br />use, nor are they lost by nonuse. They are <br />defined in relation to the reasonable and <br />correlative needs of all other landowners <br />abutting a stream. <br />7. The constitutional difficulty arises from the <br />existence of a property right in groundwater <br />that is separate and distinct from an interest <br />in land, although intimately tied to an in- <br />terest in land. Landowners, under the <br />theory, acquire a proportional interest in the <br />waters of an underlying aquifer by virtue of <br />their land ownership. This interest, however, <br />is subject to the paramount right of the state <br />to direct that water be used elsewhere, or <br />not at all. To the extent that some ground- <br /> <br />3. <br />4. <br />5. <br />6. <br /> <br />2-4 <br /> <br />water use is permitted, however, land- <br />owners each may have an equal right to a <br />fair share of the aquifer's production. Well <br />drilling moratoria would deny some land- <br />owners access to the aquifer thereby <br />destroying their proportional interest in the <br />aquifer production. The destruction of the <br />groundwater right could thus be an uncon- <br />stitutional taking unless compensation was <br />paid. <br />To the extent that new well moratoria could <br />be characterized as merely regulation of <br />land use, a taking might not arise since the <br />right in question would be the right to land, <br />and not the right to water. Since the value of <br />the property right in land would be diminish- <br />ed, but not extinguished, by the regulation, <br />the regulation might not be characterized as <br />a taking. <br />Olson provides that a landowner cannot <br />extract water "in excess of a reasonable and <br />beneficial use upon the land which he owns, <br />...." See Olson v. Wahoo, 124 Neb. 802, 811, <br />248 NW. 304, 308 (1933). <br />10. Current statutory direction is limited to run- <br />off controls. See NEB. REV. STAT. Ij 46- <br />664(1) (Reissue 1978). <br />1,. A common law action could presumably <br />correlate the rights of all users to maintain <br />an existing supply of groundwater, but the <br />users would not gain a quantified right to <br />continue a specified level of withdrawals <br />indefinitely. Given public ownership of the <br />water, correlation would only establish an <br />upper limit on groundwater withdrawals; the <br />state would remain free to set more <br />stringent requirements. <br />12. See generally W. Rodgers, Environmental <br />Law Ij 2.16 (1977). <br />13. See The Institutes of Justinian 2.1.1 (T. <br />Cooper trans, & ed. 1841). <br />14. See generally Johnson, Public Trust Pro- <br />tection for Stream Flows and Lake Levels, <br />14 U.C. Davis L. Rev. 233 (1980). <br />15. Seeid. <br />16. See generally Wilkinson, The Public Trust <br />Doctrine in Public Lands Law, 14 U.C. Davis <br />L. Rev. 269 (1980). <br />But cf. City of Eau Clare v. Dep't of Natural <br />Resources, 2 E.L.R. 20,512 (1972) (holding <br />the public trust doctrine applies only to <br />navigable waters, and hence not to ground- <br />water). <br />18. See Niles Sand & Gravel v. Alameda County <br />Water District, 37 Cal. App. 3d 924, 112 Cal. <br />Rptr. 846 (1974), hearing denied (Cal. Sup. <br />Ct., May 8, 1974),cert. denied,419 U.S.869 <br />(1975). <br />19. See Johnson, supra note 12, at 242-44. <br />20. See generally Johnson, supra note 12. <br /> <br />8. <br /> <br />9. <br /> <br />17. <br />