One-dimensional transport with inflow and storage (OTIS) a solute transport model for streams and rivers by Robert L. Runkel

Cover of: One-dimensional transport with inflow and storage (OTIS) | Robert L. Runkel

Published by U.S. Dept. of the Interior, U.S. Geological Survey, Information Services [distributor] in Denver, Colo .

Written in English

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  • Sediment transport -- Mathematical models,
  • Streamflow -- Mathematical models

Edition Notes

Book details

Other titlesOne dimensional transport with inflow and storage (OTIS)
Statementby Robert L. Runkel.
SeriesWater-resources investigations report -- 98-4018.
ContributionsGeological Survey (U.S.)
The Physical Object
Paginationv, 73 p. :
Number of Pages73
ID Numbers
Open LibraryOL17565167M

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2 One-Dimensional Transport with Inflow and Storage (OTIS): A Solute Transport Model for Streams and Rivers INTRODUCTION This report describes the development and use of a solute transport model incorporating One-Dimensional Transport with Inflow and Storage (OTIS).

The OTIS solute transport model was originallyCited by: Get this from a library. One-dimensional transport with inflow and storage (OTIS): a solute transport model for streams and rivers.

[Robert L Runkel; Geological Survey (U.S.)]. OTIS is a mathematical simulation model used to characterize the fate and transport of water-borne solutes in streams and rivers.

The governing equation underlying the model is the advection-dispersion equation with additional terms to account for transient storage, lateral inflow, first-order decay, and sorption. One-dimensional transport with inflow and storage (OTIS): a solute transport model for streams and rivers [Runkel, Robert L.] on *FREE* shipping on qualifying offers.

One-dimensional transport with inflow and storage (OTIS): a Author: Robert L. Runkel. One-Dimensional Transport With Inflow and Storage (OTIS): A Solute Transport Model for Streams and Rivers Article (PDF Available) January. OTIS, or one-dimensional transport with inflow and storage, is based on the earlier work of Bencala () and Bencala and Walters ().

Modeling low-temperature geochemical processes Chapter. To investigate the effects of flow rate variation on solute transport in a karst conduit, three pipe structures of a constant diameter pipe, the pipe connected to a symmetrical pool and an asymmetrical pool respectively were chosen, and several tracer experiments were conducted separately in each of the three pipe structures at nine flow : Xiaoer Zhao, Yong Chang, Jichun Wu, Xiaofeng Xue.

Runkel, R.L.,One-dimensional transport with equilibrium chemistry (OTEQ) — A reactive transport model for streams and rivers: U.S. Geological Survey Techniques and Methods Book 6, Chapter B6, p. One-Dimensional Transport with Equilibrium Chemistry (OTEQ) - A reactive transport model for streams and rivers.

OTEQ is a mathematical simulation model used to characterize the fate and transport of waterborne solutes in streams and rivers. The model is formed by coupling a solute transport model with a chemical equilibrium submodel. Michelle A. Baker, Jackson R. Webster, in Methods in Stream Ecology (Third Edition), Transient Storage.

A number of solute transport models can be used to simulate the BTC, which allow estimation of transient storage parameters (Eq. ).One such model is a program called OTIS (One-dimensional Transport with Inflow and Storage; Runkel, ). OM-MADE is an open-source software that simulates one-dimensional solute transport.

Its specificity is to allow multiple advective-dispersive parallel flow zones, or channels, that can exchange with each others, as well as storage, or immobile, zones ().All zones are identically described, the difference between mobile and immobile regions is done through the input Author: Anne Julie Tinet, Pauline Collon, Camille Philippe, Lorraine Dewaide, Vincent Hallet.

OTEQ is a mathematical simulation model used to characterize the fate and transport of waterborne solutes in streams and rivers.

The model is formed by coupling a solute transport model with a chemical equilibrium submodel. The solute transport model is based on OTIS, a model that considers the physical processes of advection, dispersion, lateral inflow, and. This page was last edited on 15 Juneat Content is available under GNU Free Documentation License unless otherwise noted.

Privacy policy. Analytical solutions for one- two- and three-dimensional solute transport in ground-water systems with uniform flow, by Eliezer J. Wexler. pages. Fluvial sediment concepts, by H.P. Guy. 55 pages. Field methods of measurement One-dimensional transport with inflow and storage book fluvial sediment, by H.P.

Guy and V.W. Norman. 59 Size: 2MB. The Coupled Routing and Excess STorage (CREST) model is a distributed hydrologic model developed to simulate the spatial and temporal variation of atmospheric, land surface, and subsurface water fluxes and storages by cell-to-cell simulation.

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OTIS - USGS - One-dimensional transport with inflow and storage (OTIS): A solute transport model for streams and rivers.

About Otis Elevator Company - Sweets - Otis Elevator Company. Otis is the world s leading manufacturer of elevators, escalators and other people-moving equipment. For years Otis intelligent design/5(). The transport of solute between the storage zone and the channel is determined simply by the difference in con- centrations and an exchange coefficient.

It is possible to measure the cross-sectional area of the storage zone, the concentration of solute within the storage zone, and the exchange coefficient. One-Dimensional Transport with Inflow and Storage (OTIS): A Solute Transport Model for Streams and Rivers: Bed-material sediment transport and storage dynamics on river networks.

Czuba, Jonathan: E-book: program for computing bedload transport in gravel rivers with a Manning-Strickler relation for flow resistance. We continued this study by modeling solute transport of the tracer injection data collected at two different discharges with the One-Dimensional Transport with Inflow and Storage model (OTIS).

The resulting modeled parameter estimates showed greater transient storage along the reach at the lower of the two discharges that were modeled. Dirichlet boundary conditions at the inflow and out flow ends of the flow system and initial condition in the Gaussian form is considered for Numerical solution of one dimensional contaminant transport equation 2 2 0,0 X 1,0 T T.

C e C C. mT T Pe X X. w w w. c d d d d w w w (12) where. 0 0. vL Pe D. is the Peclet number and. mL m. Each experimental data set was simulated with the one‐dimensional transport with inflow and storage (OTIS) model and analyzed with Monte Carlo‐based techniques to investigate differences in global sensitivity and time‐varying identifiability of the model by:   A stream tracer approach was used to compute the rates at which stream water is exchanged for water in storage zones (total storage) in short reaches of two small, sand-bed streams.

Tracer curves were fit to the one-dimensional transport with inflow storage (OTIS-P) model. Networks of minipiezometers were used to measure hyporheic exchange. “Flow or Temp time series date is not sufficient to run requested time window.” This one has been around for a while, but it just showed up again on the Facebook HEC-RAS User’s Group, so I thought I’d show the fix(es) here.

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Services include a comprehensive link section, a jobs database and a discussion forum. This is the largest CFD site on the net. AbstractThe hydrologic processes of advection, dispersion, and transient storage are the primary physical mechanisms affecting solute transport in streams. The estimation of parameters for a conservative solute transport model is an essential step to characterize transient storage and other physical features that cannot be directly measured, and often is a preliminary step in the Cited by: EFDC1D - A One Dimensional Hydrodynamic and Sediment Transport Model for River and Stream Networks: Model Theory and Users Guide By John M.

Hamrick Tetra Tech, Inc. Eaton Place, Suite Fairfax, VA Project Officer: Earl J. Hayter Ecosystems Research Division U.S. Environmental Protection Agency Athens, GAFile Size: KB. The physical process of "transient storage" has implications for nutrient cycling as the storage process affects residence time and the extent of biogeochemical processing.

This 4-hour workshop provides an overview of OTIS (One-dimensional Transport with Inflow and Storage), a solute transport model that is often used to quantify transient storage.

EPA//R/ September One-Dimensional Hydrodynamic/Sediment Transport Model for Stream Networks By Earl J.

Hayter1, John M. Hamrick2, Brian R. Bicknell3, and Mark H. Gray4 ^U.S. Environmental Protection Agency Office of Research and Development National Exposure Research Laboratory Ecosystems Research Division Athens, Georgia. Our model used the same finite difference approach as the One‐dimensional Transport with Inflow and Storage (OTIS) model [Runkel, ] available from the USGS.

We note that because they were performed in a tidal river, Cited by:   However, to provide a comparison of the two approaches, the One‐dimensional Transport with Inflow and Storage (OTIS) model (Runkel ) (Eq. 20) was used simulate the transport of all “A” experiments at I8 Inlet and Peat Inlet.

The model is governed by the following set of coupled differential equationsCited by: 7. • Writing python scripts to run batch simulations of the One-Dimensional Transport with Inflow and Storage (OTIS) model • Analyzing water samples in a Dionex ion chromatograph (IC)Title: Technical Professional at.

Mass balances help us answer questions about the rate convenient to express the storage and transport terms in the above equation based on and, in general, is different from the concentrations in the various inflow and outflow streams. The dimensions of each term in the above mass balance are mass/time.

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