National Wildlife Federation v. Gorsuch

693 F.2d 156, 224 U.S. App. D.C. 41, 18 ERC 1105, 13 Envtl. L. Rep. (Envtl. Law Inst.) 20015, 18 ERC (BNA) 1105, 1982 U.S. App. LEXIS 24289
CourtCourt of Appeals for the D.C. Circuit
DecidedNovember 5, 1982
DocketNos. 82-1335, 82-1337, 82-1351, 82-1352, 82-1353, 82-1354 and 82-1363
StatusPublished
Cited by89 cases

This text of 693 F.2d 156 (National Wildlife Federation v. Gorsuch) is published on Counsel Stack Legal Research, covering Court of Appeals for the D.C. Circuit primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

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National Wildlife Federation v. Gorsuch, 693 F.2d 156, 224 U.S. App. D.C. 41, 18 ERC 1105, 13 Envtl. L. Rep. (Envtl. Law Inst.) 20015, 18 ERC (BNA) 1105, 1982 U.S. App. LEXIS 24289 (D.C. Cir. 1982).

Opinion

Opinion for the Court filed by Circuit Judge WALD.

WALD, Circuit Judge:

The National Wildlife Federation petitioned the district court for a declaration that the Administrator of the Environmental Protection Agency (EPA) has a nondiscretionary duty to require dam operators to apply for pollutant discharge permits under § 402(a) of the Clean Water Act, 33 U.S.C. § 1342(a), and for an order directing her to perform that duty. The district court issued the requested declaration and order, 530 F.Supp. 1291 (D.D.C.1982), from which EPA and the numerous defendant-intervenors (principally electric utilities and water agencies) now appeal. The sole issue is whether certain dam-induced water quality changes constitute the “discharge of a pollutant” as that term is defined in § 502(12) of the Act, 33 U.S.C. § 1362(12). The Wildlife Federation, joined by plaintiff-intervenor State of Missouri, argues that in light of the remedial purpose of the Act, this phrase should be read broadly enough to cover these dam-induced changes. EPA argues for a narrower reading under which dams would not require discharge permits, but would instead be regulated under state-developed areawide waste treatment management plans pursuant to § 208 of the Act, 33 U.S.C. § 1288. Because we believe that EPA’s interpretation is entitled to great deference and that its view of the statute is reasonable, we reverse.

I. Background

A. Dam-Induced Water Quality Changes

Dams cause a variety of interrelated water quality problems, both in reservoirs and in river water downstream from a dam. The Wildlife Federation claims that five of these problems — low dissolved oxygen, dissolved minerals and nutrients, water temperature changes, sediment release, and supersaturation — require EPA to regulate dams under the § 402 permit program. The district court’s opinion, 530 F.Supp. at 1297-1303, describes these problems in detail, and we will only summarize them here.1

1. Low Dissolved Oxygen

Water released from a reservoir through a dam into downstream water may be low in dissolved oxygen. The river below the dam will remain oxygen-depleted for some distance, although the river will gradually become reaerated through wind mixing as it flows downstream.2 If the oxygen level is too low, fish cannot survive. Also, a river low in oxygen has limited ability to break down pollutants and other organic matter. Because dissolved oxygen is important both for fish and for breakdown of organic mat[47]*47ter, it is an important measure of water quality.3

Only large storage dams have low dissolved oxygen problems, and then only during warmer months and only when water is released from the lower part of the reservoir.4 During warm months, deep reservoirs, like deep natural lakes, stratify into a cold, dense lower layer and a warmer, lighter upper layer. The upper layer, called the “epilimnion,” is aerated by wind mixing; oxygen is also produced by photosynthesis. Thus, water quality in the upper layer is good. The lower level, called the “hypolimnion,” is too deep to be aerated by wind action and light levels are too low to support photosynthesis. Organic decomposition, which consumes oxygen, leads to a continual net depletion of dissolved oxygen. Depletion continues until “fall turnover,” when the two layers break up and the reservoir returns to full aeration.5

The rate of oxygen depletion depends primarily on the volume of water in the hypolimnion (the more water, the more oxygen is available for decomposition), its temperature (decomposition occurs more slowly in cold water and colder water also contains more dissolved oxygen), and the quantity of organic matter it contains (the more organic matter, the greater the oxygen demands for decomposition). In particular, if the river above the dam is high in plant nutrients or organic waste when it enters the reservoir — whether from pollution or from natural causes — oxygen depletion in the hypolimnion will be severe.6

Several techniques can be used to prevent release of oxygen-depleted water. First, for many dams, water can be released from the epilimnion (which occurs automatically for natural lakes). Older dams were built with reservoir outlets at one level only, usually deep in the dam so that the outlet would remain below the surface of the reservoir even in dry years when the reservoir was low. Many newer dams, however, have outlets at several levels, permitting the dam operator to release high-quality epilimnion water. In single-outlet dams, one can aerate the reservoir (by pumping compressed air down to the hypolimnion) or destratify it (by pumping cold water from the hypolimnion to the surface). Alternatively, one can aerate the hypolimnion water as it is released from the reservoir, either by injecting air or by creating turbulence.7

The record does not indicate the number of dams for which discharge of low-oxygen water is a significant problem, nor the cost of the various methods of mechanical aeration.8 But the problem is serious for at least some dams, and the cure is apparently expensive.9

[48]*48 2.Dissolved Minerals and Nutrients

If dissolved oxygen is totally depleted from the hypolimnion, a further problem develops. A number of minerals and plant nutrients, insoluble under normal “aerobic” conditions, are soluble in zero-oxygen “anaerobic” water. These compounds — including iron, manganese, and phosphates— therefore tend to be leached from bottom muds into the reservoir. High concentrations of these minerals and nutrients, released into the downstream river, can harm fish, make the water unpalatable for drinking, and foster undesirable plant growth.10

As for low-dissolved oxygen problems generally, whether mineral leaching will occur depends on a number of factors, including reservoir size, water temperature, and the quality of upstream water. In addition, mineral leaching depends on the amount of leachable matter in the reservoir bottom, which in turn depends partly on how old the reservoir is (for an older reservoir, most leachable minerals may have already been leached).11

Control of mineral leaching primarily involves destratifying or mechanically aerating the reservoir to prevent the hypolimnion from becoming totally depleted, or else discharging water from the epilimnion. When building a new dam, site preparation (e.g., removing organic soils) can reduce future leaching. Once again, the record reveals neither the number of dams for which mineral leaching is a significant problem nor the cost of cure.

3. Temperature Changes

In a thermally stratified reservoir, the lower hypolimnion layer will generally be colder than the upstream river, while the upper epilimnion layer will be warmer. Some species of fish can survive only in warm water; others can survive only in cold water.

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693 F.2d 156, 224 U.S. App. D.C. 41, 18 ERC 1105, 13 Envtl. L. Rep. (Envtl. Law Inst.) 20015, 18 ERC (BNA) 1105, 1982 U.S. App. LEXIS 24289, Counsel Stack Legal Research, https://law.counselstack.com/opinion/national-wildlife-federation-v-gorsuch-cadc-1982.