Stream reach definition

Stream reach means a segment of a stream channel having a defined upstream and downstream point.
Stream reach. 8 means the length of a watercourse with similar channel morphology, channel dimension, gradient;

Examples of Stream reach in a sentence

  • Stream reach inventory and channel stability evaluation: a watershed management procedure.

  • NOTE: Stream reach for single 600 gpm foam nozzle = 150 feet max• 3 tank cars on fire = 1,500 gallons of foam concentrate; apply solution at a target rate of 1,680 gpm for 15 minutes; and reapply as necessary to maintain foam blanket;Total water supply required = (+/-) 80,000 gallons for foam and cooling water.

  • NOTE: Stream reach for single 1000 gpm foam nozzle= 200 feet max• Use cooling water on exposed and involved cars; minimum rate = 200 gpm applied to the exterior of the vapor space of each car during extinguishment and maintain for 30 minutes thereafter.

  • Minimum mean weekly nitrogen concentrations in the Kahahakuri Stream reach over 25 mg/L towards the end of the period of weekly flow simulation (Fig.

  • Page 2:15 Section 2.4.4.2 Stream reach numbering Third paragraph (also applies to Standards for Fish and Fish habitat Maps Version 3.0, Section 2.2.1, first paragraph, sentences 5-7 and Figure 3): Replace: “Reach numbers start at 1 at the mouth or the downstream end of the stream in the project area and increase sequentially upstream (e.g., 1, 2, 3, …).

  • Id. The Refuge Stream reach accounted for the highest density of Moapa dace, with the Plummer, Pedersen, and Apcar Units containing the second, third, and fourth highest densities, respectively.4 Id. at 24, 26.

  • Stream reach assessments group channels into segments (reaches) that reflect their similar slope and planform characteristics.

  • Unit conversions will need to be done by the user.o The following relevant reach properties are calculated by HEC-HMS: length & slopeo Stream reach cross-section geometry must be determined by the user.

  • Id. The Refuge Stream reach accounted for the highest density of Moapa dace, with the Plummer, Pedersen, Ctr.

  • The field parameters that are necessary to calculate RBS include the following:• Pebble count• Thalweg depth• Bankfull height• Bankfull width• Large woody debris• Stream reach length• Residual depth According to the results presented above, measurements for numerous variables could be eliminated or condensed.

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