Woodsum v. Pemberton Tp.

412 A.2d 1064, 172 N.J. Super. 489
CourtNew Jersey Superior Court Appellate Division
DecidedJanuary 29, 1980
StatusPublished
Cited by26 cases

This text of 412 A.2d 1064 (Woodsum v. Pemberton Tp.) is published on Counsel Stack Legal Research, covering New Jersey Superior Court Appellate Division primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Woodsum v. Pemberton Tp., 412 A.2d 1064, 172 N.J. Super. 489 (N.J. Ct. App. 1980).

Opinion

172 N.J. Super. 489 (1980)
412 A.2d 1064

RICHARD WOODSUM AND JUDITH WOODSUM, HIS WIFE, PLAINTIFFS,
v.
TOWNSHIP OF PEMBERTON, A MUNICIPAL CORPORATION OF THE STATE OF N.J., MUNICIPAL UTILITIES AUTHORITY OF THE TOWNSHIP OF PEMBERTON; HAROLD C. GRIFFIN, MAYOR, TOWNSHIP OF PEMBERTON, FRED DETRICK, HAROLD GRIFFIN, CHARLES JONES, ELMER D'IMPERIO AND ANTHONY ZOPPINA, AS MEMBERS OF THE TOWNSHIP COMMITTEE OF THE TOWNSHIP OF PEMBERTON AND INDIVIDUALLY, AND R. LEWIS GALLAGHER AND LAYNE-NEW YORK CO. INC., DEFENDANTS.

Superior Court of New Jersey, Law Division — Burlington County.

Decided January 29, 1980.

*494 Richard M. Sevrin for plaintiffs (Gertner & Sevrin, attorneys).

Frederick W. Hardt for defendant R. Lewis Gallagher (Sever, Hardt & Main, attorneys).

Donald E. Williams, for defendant Township of Pemberton (Polino & Williams, attorneys).

HAINES, J.S.C.

Plaintiffs' residence, purchased in 1968 and situate in Pemberton Township, Burlington County, New Jersey, was supplied with water for domestic use by a well extending into the Wenona-Mt. Laurel aquifer. In 1972 defendant township constructed a water plant and two wells, drawing from the same aquifer, to provide water for public consumption. Required approvals were obtained from state agencies. Bonds were issued in the amount of $1,370,000 to finance the project. It was estimated that the new plant would extract 18,800,000 gallons of water a month. It is the plaintiffs' contention, taken as true for *495 present purposes, that the operation of the new plant lowered the water table reached by their well to the point where they were deprived completely of any water supply. As a result they were obliged to vacate the house and to rent other quarters. The dwelling has been vacant ever since and, despite efforts by plaintiffs, has been vandalized and substantially damaged. Plaintiffs' water supply could have been restored by deepening their well at a cost of $750 to $1,700 (depending on whether a "packer" could be removed without damage). They had no funds for that purpose and were unable to borrow; consequently, the work was never performed. They claim damages from the township, the individual members of its governing body, its municipal utilities authority, the members of that authority, and its engineer. (Suit against defendant Layne-New York was previously dismissed.)

The basic issue in this controversy concerns the respective rights of the parties in the subterranean waters used by both of them. The law concerning such rights, at least in a contest between overlying owners and a merchandiser of water, as here, was last established by Meeker v. East Orange, 77 N.J.L. 623 (E. & A. 1909). Significant changes in scientific knowledge, demand for water and legislation have occurred in the 70 years since Meeker was decided. Hanks, "The Law of Water in New Jersey: Ground Water," 24 Rutg.L.Rev. 621, 649 (1970); Restatement, Torts 2d, c. 41 at 255 (1979). Nevertheless, no court has had an opportunity to interpret Meeker in the light of those events, until now.

Plaintiffs' claims for damages are based upon two theories: (1) the township's interference with their water supply was a "taking" of their property without due process, contrary to U.S.Const., Amend. V and N.J.Const., Art. 1, par. 20, permitting recovery in a direct constitutional action, and under the Federal Civil Rights Act, 42 U.S.C.A. § 1983, and (2) the actions of defendants were negligent in their construction of the new water plant and in their breach of a duty to correct plaintiffs' *496 water problem once it became known. Consequential and punitive damages are sought. The complexity of these issues invited a pretrial conference at which defendant was ordered to move for summary judgment. That motion was made, considered and denied. As trial approached, additional information was received. The court reopened the summary judgment proceedings, required and received additional briefs, heard further oral argument and, in this opinion, readdresses the issues which are subject to resolution by summary judgment pursuant to R. 4:46. The facts were stipulated for the purpose of the motion.

I. Water Rights; the Background

The issues here concern ground water as opposed to diffused surface water and surface stream water. Ground water consists of underground streams and percolating waters. It is the presumption in New Jersey, as in most states, that underground water is percolating water and not a stream. Ocean Grove Camp Meeting Ass'n v. Asbury Park, 40 N.J.E. 447 (1885); Hanks, supra at 626. No party here argues for the existence of an underground stream; all refer to an aquifer as the source of supply of plaintiffs' and the township's wells. In this opinion, all references to ground water are intended to mean percolating water.

Changes in our understanding of the nature of water and its movements through the earth are illustrated by the following quotations, 113 years apart, noted in Hanks, supra:

Water, whether moving or motionless in the earth, is not, in the eye of the law, distinct from the earth. The laws of its existence and progress, while there, are not uniform, and cannot be known or regulated. It rises to great heights, and moves collaterally, by influences beyond our apprehension. These influences are so secret, changeable and uncontrollable, we cannot subject them to the regulations of law, nor build upon them a system of rules, as has been done with streams upon the surface. Roath v. Driscoll, 20 Conn. 532, 540 (1850).
Water gets into the ground wherever and whenever it is available in excess of the field capacity of the soil and can move downward by gravity through the *497 zone of aeration to the water table, or wherever and whenever water in a surface body has a higher head than the adjacent ground water; [it] moves through the rocks around, over, under and through obstacles formed by zones of lower permeability; it approaches the land surface or a body of surface water where the head is lower; and it is discharged by seepage or spring flow into streams, lakes or the ocean or is dissipated by water-loving plants or by evaporation from the soil. As a phase of the hydrolytic cycle the ground water reservoir serves as nature's great delaying and storage medium for water. In it water is relatively safe from evaporation and contamination. It furnishes large supplies of water and can furnish more. And, of great importance to the comprehensive multiple-purpose developments of the future, its storage and water-transmitting properties in many places offer a means for integrated management of ground and surface water. That is, floodwaters can be stored underground while they are available, and water supplies can be sustained by natural or artificially assisted ground water discharge in dry weather. The Role of Ground Water in the National Water Situation, U.S. Geological Survey, Water Supply Paper 1800 (1963), reprinted in part in Sax, Water Law: Cases and Commentary, 243-44 (1965); see also, Rest., Torts 2d, Ch. 41, at 254. [at 624-625]

We are dealing here with the use of an aquifer, defined as follows:

The term `aquifer' describes a body of rock (as used in this report, `rock' includes unconsolidated material such as sand, gravel, clay and soil) that is filled with water and is permeable enough to carry or yield water in useful quantities.

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412 A.2d 1064, 172 N.J. Super. 489, Counsel Stack Legal Research, https://law.counselstack.com/opinion/woodsum-v-pemberton-tp-njsuperctappdiv-1980.