<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amount of water that can be withdrawn by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 />
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