Kleinman v. City of Austin

310 F. Supp. 3d 770
CourtDistrict Court, W.D. Texas
DecidedMarch 6, 2018
Docket1:15–cv–497–RP
StatusPublished
Cited by1 cases

This text of 310 F. Supp. 3d 770 (Kleinman v. City of Austin) is published on Counsel Stack Legal Research, covering District Court, W.D. Texas primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Kleinman v. City of Austin, 310 F. Supp. 3d 770 (W.D. Tex. 2018).

Opinion

ROBERT PITMAN, UNITED STATES DISTRICT JUDGE

On September 20 and 21, 2017, the Court held a non-jury trial in this case. During the trial, the Court took evidence and heard sworn testimony. On November 20, 2017, Plaintiff submitted his proposed findings of fact and conclusions of law. (Dkt. 105). On November 22, 2017, Defendant submitted its proposed findings of fact and conclusions of law. (Dkt. 106). Having considered the evidence, testimony and oral argument presented during the trial, the post-trial submissions, and the applicable law, the Court now enters the following findings of fact and conclusions of law. Any finding of fact that should be construed as a conclusion of law is so adopted. Any conclusion of law that should be construed as a finding of fact is so adopted.

I. INTRODUCTION

Michael Kleinman ("Kleinman") has sued the City of Austin ("the City") for violations of the Clean Water Act ("CWA"), 33 U.S.C. §§ 1251 et seq. Those violations stem from ongoing discharges of sand, soil, rock, and other sediment that are being washed into the Colorado River from the bed and banks of a channel running through a city park.

Kleinman also alleges that construction materials from the City's work on that channel are being discharged into the river, but the evidence suggests that those discharges have ceased. Nonetheless, sediment is a pollutant under the CWA, and there is no question that sediment from the channel continues to be washed into the river during even minor rain events.

The Court therefore agrees with Kleinman that the City's discharges of sediment violate the CWA. The finding of a violation, however, does not end the inquiry, for the Court must also fashion a remedy. The Court finds that the evidence does not justify the injunction the Kleinman requests; a nominal civil penalty will do.

II. FINDINGS OF FACT

The Court finds the following facts. The Colorado River is a navigable body of water of the United States that passes through Austin, Texas. Roy G. Guerrero Colorado River Park borders a stretch of the river in southeast Austin. Country Club Creek West runs through the park and empties into the river. The Country Club Creek Bypass Channel (the "Channel") extends from a bend in the creek to a discharge point across the river from Kleinman's backyard.

The Channel originally existed as a natural gully that brought water to the river from a different manmade channel that did not extend to the river. In the late 1970s, before the City owned the land on which the park now sits, a private developer dug a channel to divert water away from land slated for residential development. The developer's channel stopped about 1,000 feet short of the river. The developer's channel *775also stopped at an elevation 20 feet above the river. Water running through the developer's channel therefore found its own way to the river.

For the most part, water from the developer's channel found its way to the river along a dominant flow path to the east of the channel's endpoint. This dominant path became County Club Creek West. But water would overflow the creek's banks during large rain events, forming a natural gully heading due north to a point across the river from what is now Kleinman's property.

As it happens, the soil underneath much of the park is sand and other fine sediment deposited by the Colorado River over hundreds of years at a slow-moving bend in the river. The natural gully traced its path to the river through this sandy soil. Due to the elevation at which the developer's channel abruptly ended, the natural gully's path through the sandy soil had a slope of 2 percent.

A stable slope through sandy soil is about 0.25 percent. The gully's path was therefore an unstable one; water moving through that soil naturally eroded the gully as it sought its longer, more gradual, and more stable form. Had the City done nothing, natural erosion would have continued until the gully reached its stable slope of 0.25 percent which, accounting for the 20-foot drop to the river, would extend 8,000 feet inland. Naturally occurring erosion had already deposited enough sediment into the Colorado River to form a visible sandbar at the gully's delta as early as 1997, long before the City began work on the Channel. Left unchecked, natural erosion would have continued to deposit considerable amounts of sediment into the river.

After the City acquired the land now constituting Roy G. Guerrero Park, it recognized that the gully posed an erosion problem and secured funding to improve the gully. In 2010, the City began construction of the Channel along the footprint of the gully in order to reduce erosion and define the contours of the gully. To construct the Channel, the City excavated dirt and sand to shape the Channel, filled in the top of the Channel bed with less erosive material, covered the Channel bed with erosion-control fabric, and installed rock berms. The City used temporary erosion controls during the construction period. The City also built a pedestrian footbridge that spanned the Channel about 1,000 feet upstream of the river. The City completed its work on the Channel and the pedestrian bridge in 2012.

The City's construction project failed to arrest the erosion problem. The Channel bed is now at least 10 to 12 feet lower than it was when construction began. The Channel's headcut-a highly erosive elevation drop at which fast-moving water scours out soil-is moving inland by hundreds of feet every year. City expert Mike Kelly1 admits that it is "extremely unusual" for a headcut to move upstream so rapidly. (Tr., Dkt. 104, at 68:23-25). City engineer Janna Renfro characterized this rate of headcut progression as "completely off the charts."2 (Renfro Presentation, Dkt. 102-9, at 8:20 (Pl.'s Ex. P-25) ). Even minor rain events of one to two inches are now moving the headcut 30 or 50 feet upstream-rates of progression that would *776be considered fast over a full year. (Id. at 8:30-9:00).

The headcutting is ongoing. As the headcut continues to move, the Channel continues to erode, depositing sediment from the Channel into the river at the point where the two meet. At that point there exists a visible sandbar, the present shape and constitution of which is attributable at least in part to the City's construction of the Channel and the ongoing erosion stemming from that project.

Kleinman lives directly across the river from the mouth of the Channel. From his backyard, which abuts the river's northern bank, he can see the sandbar that lies across the river at the mouth of the Channel. Kleinman dislikes the sandbar. He says the sight of the sandbar makes it "very frustrating" to go out to his backyard and that seeing the sandbar makes it less enjoyable for him to use his decks or swim in the river. (Tr., Dkt. 103, at 31:11-23).

The City has a plan to address the ongoing Channel erosion. The City will soon construct three concrete drop structures that will step the Channel down to the river.

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310 F. Supp. 3d 770, Counsel Stack Legal Research, https://law.counselstack.com/opinion/kleinman-v-city-of-austin-txwd-2018.