Stuthman v. Adelaide D. Hull Trust

447 N.W.2d 23, 233 Neb. 586, 1989 Neb. LEXIS 409
CourtNebraska Supreme Court
DecidedOctober 20, 1989
Docket88-004
StatusPublished
Cited by6 cases

This text of 447 N.W.2d 23 (Stuthman v. Adelaide D. Hull Trust) 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
Stuthman v. Adelaide D. Hull Trust, 447 N.W.2d 23, 233 Neb. 586, 1989 Neb. LEXIS 409 (Neb. 1989).

Opinion

White, J.

This is an appeal from an order of the Cuming County District Court dismissing plaintiff’s petition for equitable relief. We affirm.

*587 On December 1, 1986, plaintiff filed a petition alleging that the defendants constructed a ditch which drained accumulated surface water from a depression or basin area located on defendants’ land, across the defendants’ land, and ultimately onto plaintiff’s land. This drainage water caused the plaintiff’s land to become soggy, preventing 11 acres of corn from being harvested by the tenant in 1986. The plaintiff sought a permanent injunction ordering defendants, in effect, to return defendants’ land to its condition prior to the ditch’s construction. The petition also requested $660 in money damages for rental loss for 1986.

The trial judge reviewed the evidence, which was received by stipulation, and made specific findings, including findings that the defendants brought themselves within the protection of Neb. Rev. Stat. § 31-201 (Reissue 1988) and that the plaintiff did not allege or prove negligence or lack of reasonable care on the part of the defendants. Consequently, he ordered that plaintiff’s petition be dismissed at plaintiff’s costs. From this order, the plaintiff appeals to this court.

On appeal, plaintiff alleges 11 assignments of error, all of which concern alleged erroneous factual findings. All assigned errors will be considered in our de novo review.

An action for an injunction sounds in equity. Selection Research, Inc. v. Murman, 230 Neb. 786, 433 N.W.2d 526 (1989). In an appeal of an equity action, this court tries the factual questions de novo on the record and reaches a conclusion independent of the findings of the trial court; provided, where the credible evidence is in conflict on a material issue of fact, we consider and may give weight to the fact that the trial judge heard and observed the witnesses and accepted one version of the facts rather than another. In its de novo review of the record, this court is guided by the rule that a party seeking an injunction must establish by a preponderance of the evidence every controverted fact necessary to entitle the claimant to relief. Federal Land Bank of Omaha v. Swanson, 231 Neb. 868, 438 N.W.2d 765 (1989).

We have reviewed the record de novo and make the following findings of material fact. The plaintiff, Pearl Stuthman, owns a parcel of farmland described as the west half of the *588 southwest quarter of Section 23, Township 23 North, Range 4 East of the 6th P.M., less approximately 4.6 acres owned by Melvin Brokaw, all in Cuming County, Nebraska. Since 1971, this land has been rented to Vernon Schultz, who has farmed the property.

The defendant Adelaide D. Hull Trust owns a parcel of farmland legally described as the southeast quarter of Section 22, Township 23 North, Range 4 East of the 6th P.M., in Cuming County, Nebraska. Since 1981, this land has been rented to Willis and Weslie Geu, who have farmed the property. Henry E. Hull, who is also a defendant, is the trustee.

The trust property lies immediately west of the Stuthman property, and the two properties are separated by a county road which runs to the north and south. A drainage culvert, which was installed by someone other than the defendants, lies under the surface of this road. The natural slope of the surrounding land deposits water into the road ditch on the west side of the road, and the water flows through the culvert from the west to the east onto the Stuthman land.

To the south and east of the Stuthman property lies the Anderson property. The Anderson and Stuthman properties are separated by a county road which runs to the east and west. A drainage culvert lies under the surface of this road and drains water from the north to the south and southeast into a creek which eventually flows into the Elkhorn River.

There is a natural basin or depression area located in the northwestern area of the trust property. Land surrounding the depression to the north, west, and south is higher in elevation than the depression. The east rim of the depression has a ridge about 2 feet higher than the lowest point of the depression. Surface waters accumulate in the depression during periods of above-normal moisture from either rainfall, irrigation runoff, or melting snows. Water which does not flow over the top of the eastern rim or ridge remains in the depression until it evaporates or percolates down through the soil. Water retention in the depression is only temporary, and the depression does not constitute a permanent lake or pond. This depression has periodically and temporarily accumulated surface water.

In July of 1986, Henry Hull, as trustee, directed that a *589 drainage ditch be dug to facilitate drainage by preventing the accumulation of surface water in the depression. The general direction of the flow of surface waters on the trust property is from the west to the east and southeast. The ditch was constructed through the ridge on the east side of the basin. The ditch terminates on the trust property, and the water flowing from this ditch empties into a natural drainage course or draw also located on the trust property. After the water leaves the trust property, it flows into the county road ditch, through the culvert, and across the Stuthman land, following the natural course of drainage in an east to southeast direction. After following this natural drainage course across the Stuthman property, the water flows through the drainage culvert under the east-west county road into a creek on the Anderson property, eventually draining into the Elkhorn River.

At the time the ditch was dug, the depression contained no water, and there was no sudden release of impounded waters. By constructing the ditch, the defendants have not diverted any water upon the lands of any others except into a natural draw or drainageway where the water would generally flow.

The wet areas on the Stuthman land would have been present even without the construction of the drainage ditch. Charles Mahnke, a soil scientist and soil specialist for the Soil Conservation Service for 29 years, testified for the defendants that there has been increased irrigation and precipitation runoff in the area since the early 1980s. The soil in the area of both properties is sandy. Sandy soil, because of its porous character, allows water to travel downward until it reaches “hardpan.” When the water reaches the hardpan, it begins to migrate toward the general course of drainage, which is usually toward lower elevations, where it congregates or accumulates. Eventually, water will begin to appear on the surface of the land when the accumulations come to a point where the elevations have leveled out in the course of drainage. He testified that even without the construction of the ditch, both properties would have had wet areas in 1986 and 1987 and possibly into later years. This is because the wet areas on both properties are migrating to the east, following the natural course of drainage.

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Bluebook (online)
447 N.W.2d 23, 233 Neb. 586, 1989 Neb. LEXIS 409, Counsel Stack Legal Research, https://law.counselstack.com/opinion/stuthman-v-adelaide-d-hull-trust-neb-1989.