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Middle Snake River productivity and nutrient assessment 1994. Technical research completion report Item Info

Title:
Middle Snake River productivity and nutrient assessment 1994. Technical research completion report
Authors:
Falter, C. Michael; Burris, Chris
Date Created (ISO Standard):
1996-06
Description:
In 1994, the University of Idaho conducted a third year of research on the water quality-limited section of the middle Snake River from Twin Falls downstream to Upper Salmon Falls Dam (RM 614.8 - 581.0). This study focused on the highly productive shallow Crystal Springs Reach (Rm 599.5 - 601.3), rich in aquatic macrophyte development. In research during 1992 and 1993, the Crystal Springs Reach (CSR) was determined to be the most productive reach in the water quality-limited section. In the 1994 study described herein, we emphasized relationships in these plant beds and between the plants, water quality variables, and sediments. [...] This reach of the Middle Snake River is classified as eutrophic based on chlorophyll a concentrations, dissolved nitrogen and phosphorus concentrations, dense aquatic macrophyte growths, and sediment nutrient levels.
Subjects:
Water quality Aquatic macrophytes Primary productivity Sediments Shallow water
Location:
Middle Snake River; Southern Idaho
Latitude:
42.76
Longitude:
-114.9
Collection:
Boise Basin
IWRRI number:
199601
Rights:
Rights to the digital resource are held by the University of Idaho. http://www.uidaho.edu/
Publisher:
Idaho Water Resources Research Institute; University of Idaho
Contributing Institution:
University of Idaho
Type:
Text
Format:
application/pdf
Cataloger:
KIT
Date Digitized:
2017-09-25

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Source
Preferred Citation:
"Middle Snake River productivity and nutrient assessment 1994. Technical research completion report", Idaho Waters Digital Library, University of Idaho Library Digital Collections, https://www.lib.uidaho.edu/digital/iwdl/items/iwdl-199601.html
Rights
Rights:
Rights to the digital resource are held by the University of Idaho. http://www.uidaho.edu/