by U.S. Dept. of the Interior, Geological Survey, Open-File Services Section, Western Distribution Branch] in Rolla, Mo, [Denver, Colo .
Written in English
|Statement||by Wayne R. Berkas ; prepared in cooperation with the Missouri Department of Natural Resources, Division of Environmental Quality|
|Series||Open-file report -- 83-275, U.S. Geological Survey open-file report -- 83-275|
|Contributions||Missouri. Division of Environmental Quality, Geological Survey (U.S.)|
|The Physical Object|
Get this from a library! Suspended-sediment data in the Salt River basin, Missouri. [Wayne R Berkas; Missouri. Division of Environmental Quality.; Geological Survey (U.S.)]. Suspended-sediment data collected at six stations in the Salt River basin during are presented. The estimated average annual suspended-sediment load is 1,, tons per year from a geomorphic examination, and 1,, tons per year from periodic sampling at Salt River near Monroe City, Mo. Suspended-sediment data in the Salt River basin, Missouri [microform] / by Wayne R. Berkas ; prepared in cooperation with the Missouri Department of Natural Resources, Division of Environmental Quality U.S. Dept. of the Interior, Geological Survey ; Open-File Services Section, Western Distribution Branch] Rolla, Mo.: [Denver, Colo Since , efforts have been conducted in Goodwater Creek Experimental Watershed to assess suspended sediment transport from this 73 km2 watershed located in the Salt River Basin, Missouri Cited by: 9.
This study investigates the dynamic behavior of suspended sediment load transport at different temporal scales in the Mississippi River basin. Data corresponding to five successively doubled temporal scales (i.e. daily, two‐day, four‐day, eight‐day and 16‐day) from the St. Louis gaging station in Missouri Cited by: About Cookies, including instructions on how to turn off cookies if you wish to do so. By continuing to browse this site you agree to us using cookies as described in . The Salt River basin drains 2, square miles of northeastern Missouri and lies in the Dissected Till Plains physiographic region. The North Fork, South Fork, and lower Salt River sub-basins compose 32%, 42%, and 27% of the basin, respectively. Clarence Cannon Dam, located on the Salt River approximately 63 miles upstream from itsFile Size: KB. Mississippi River Basin-Salt River: North Fork Salt River at Hagers Grove, MO: 05/31 CDT: -- North Fork Salt River near Shelbina, MO: 05/31 CDT Page Contact Information: Missouri Water Data Maintainer Page Last Modified: EDT.
Trends in streamflow and concentration of total nitrogen, nitrite plus nitrate, ammonia, total phosphorus, orthophosphorus, and suspended sediment were determined for the period from to at selected stream sites in the Missouri River Basin. Flow-adjusted trends in concentration (the trends that would have occurred in the absence of natural changes in streamflow) and non-flow . • The Missouri River carried over million tons of suspended sediment per year prior to dam construction era of to (MRD Sediment Ser Nov ). • The Missouri River now carries only 20 to 25 percent of the pre-dam sediment Size: 32KB. Salt River Watershed Inventory and Assessment (pdf, KB) The Salt River basin drains 2, square miles of northeastern Missouri and lies in the Dissected Till Plains physiographic region. The North Fork, South Fork, and lower Salt River sub-basins compose 32%, 42%, and 27% of the basin. Most suspended sediment transport in Indiana streams is silt and clay size (particles between and millimeter in diameter and particles less than millimeter in diameter). Discover.