Brummund v. Vogel

168 N.W.2d 24, 184 Neb. 415, 1969 Neb. LEXIS 562
CourtNebraska Supreme Court
DecidedMay 16, 1969
Docket37154
StatusPublished
Cited by3 cases

This text of 168 N.W.2d 24 (Brummund v. Vogel) is published on Counsel Stack Legal Research, covering Nebraska Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Brummund v. Vogel, 168 N.W.2d 24, 184 Neb. 415, 1969 Neb. LEXIS 562 (Neb. 1969).

Opinion

Ronin, District Judge.

This is an action in equity wherein Wilbert Brummund, plaintiff herein, seeks to enjoin Robert Vogel and Gloria Vogel, defendants, from constructing an earthen dam in a spring-fed creek on defendants’ land. After trial, the district court entered judgment for the defendants and denied an injunction. From an order overruling his motion for new trial, the plaintiff has appealed.

Plaintiff is the owner of 200 acres of land in the west half of Section 23, Township 24 North, Range 1 East of the 6th P.M., in Stanton County, Nebraska. The defendants are the owners of the northeast quarter of Section 22, which tract lies immediately west of the north one-half of plaintiff’s land and is separated by a county road on the section line.

There are two separate, small spring-fed creeks which have their sources on the defendants’ farm, flow in a general southeasterly direction, and merge into one stream near the east section line of their land. This stream then proceeds under a bridge on the county road onto the plaintiff’s farm and continues in a southerly di *417 rection along the west edge of his farm and eventually flows into Pleasant Run Creek south of plaintiff’s land. These two creeks on the defendants’ land are identified as West Creek and East Creek. The springs which supply West Creek are larger than East Creek. Its ditch channel varies from 2% to 6 feet deep and during rains or melting snows becomes a good-size creek. East Creek becomes dry during part of the summer when there is no run-off of surface water and after the merger of the two creeks, portions of the creek bed on plaintiff’s land tend to become dry for some time in the summer. The proposed location of defendants’ dam is on West Creek above its merger with East Creek. The evidence further shows that the plaintiff was pasturing 28 head of cattle and their calves whose main source of water was the creek that came from the defendants’ land. Plaintiff also has a small spring-fed creek which source is on his land, but which dries up in summer weather.

Plaintiff testified he had never previously seen the plans for the proposed dam, which were received in evidence. The plans are for an earthen dam 16 feet high from the bottom of the West Creek bed, 520 feet in length, 10 feet wide at the top, and with a width of about 80 feet at its base. The primary overflow in the dam is a 30-inch vertical pipe or morning glory intake located 10% feet above the bed of the creek, which connects with a 24-inch horizontal pipe for conducting water through the dam. There is a provision for an emergency spillway at 13% feet above the creek bed. In addition, a 24-inch vertical pipe with gravel was placed 6% feet above the bed of the stream, this being attached to a 1%-inch pipe which was 20 feet in length and which ran into the interior of the dam and joined with the 24-inch pipe which served the primary overflow outlet.

Plaintiff’s engineer, Harvey Johnson, testified that he had made a visual inspection of the area surrounding the proposed dam, and made general reference to the *418 plans and specifications of the dam which are in evidence. He did not relate any measurements that he personally took. Neither did he measure the rate of flow of West Creek either above or below the proposed site of the dam, nor could he estimate it. Further, the witness was not informed as to the size and steepness of the run-off area, the usual amount of rainfall in this locality during the pasture season, the nature of the soil or of the terrain above the dam, nor the quantity of water that might percolate through, under, or around the dam, nor the depth of the bed of West Creek at the site of the dam. Plaintiff’s engineer stated that there would be a loss of water by evaporation, and that by observation it was his opinion that the amount of water that would go through the 1%-inch pipe would not be as ample as the supply that generally flows downstream. He agreed with defendants’ witness that %-inch run-off would fill the pond, and once the pond was filled he could not positively state that there would be any impediment whatever tO' the normal flow of the stream below the dam just prior to its entry on plaintiff’s land.

Gene Phillips, the Stanton County soil conservationist, was the only witness for the defendants. He related that he had 9 years of experience working with approximately 100 different dams, of which 25 to 30 dams had been in Stanton County. His signature as technician appears on exhibit 9B which is a profile of the drain-way with detailed measurements of the immediate watershed involved. Exhibit 9A is a cross-section drawing of the proposed dam, giving detailed specifications. Phillips testified that the proposed dam met the requirements of the federal government; would provide for a pond 1.3 acres in maximum surface area with a maximum storage capacity of 3.6 acre feet; that the pond would be below and not reach the area of the fountainhead of the springs; and that the sources of the water would be a 155-acre drainage area of the defendants’ land and the water from the springs of their land. The *419 witness took various readings on June 7, 1967, and determined the rate of flow of West Creek was 25 gallons per minute at the dam site and 20 gallons per minute below the dam site and just about the junction of these creeks, and that the rate of flow in the East Creek was 12 gallons per minute. Phillips testified that the 1%-inch pipe was usually not included in these dam structures, but occasionally were inserted as a device for livestock watering and he inferred that it was- included for plaintiff’s benefit; that 3/10 of an inch run-off water over the 155-acre drainage area would completely fill the pond if empty, independent of any water from the spring, and the water level would then be at the primary overflow 30-inch riser on the dam.

We find that the waters from the springs on defendants’ land which are the source of West Creek flow generally, although not continuously, in a well-defined channel and in a sufficient quantity and direction across plaintiff’s land into another stream of water to constitute a watercourse within the meaning of section 31-202, R. R. S. 1943. The owner of the land upon which springs are located whose waters are the source of a definite watercourse does not have an exclusive right to control and use the waters therefrom to the injury of a lower riparian owner or senior appropriator. Rogers v. Petsch, 174 Neb. 313, 117 N. W. 2d 771; Slattery v. Dout, 121 Neb. 418, 237 N. W. 301.

This being an action in equity, we are required to determine the issues of fact complained of de novo and reach an independent conclusion without reference to the findings of the district court. § 25-1925, R. R. S. 1943. The factual situation presented in this case involves a further application of competing water claims by an upstream appropriator with one who is a downstream domestic user under the guidelines detailed in Wasserburger v. Coffee, 180 Neb. 149, 141 N. W. 2d 738.

The evidence in this case is undisputed that plaintiff and his immediate predecessors have for many years. *420 watered their cattle from the water that came from West Creek which flowed through or on their pasture land.

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Cite This Page — Counsel Stack

Bluebook (online)
168 N.W.2d 24, 184 Neb. 415, 1969 Neb. LEXIS 562, Counsel Stack Legal Research, https://law.counselstack.com/opinion/brummund-v-vogel-neb-1969.