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Page Title: E.4 Macintyre Analytical Method for CDF Discharge in Riverine Conditions
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integral model that accounts for most near-field and some far-field steady state
dynamics. CORMIX is presently designed for use in shallow water systems
where the jet mixing processes are expected to encounter bottom boundary
interaction. CORMIX is capable of representing negatively buoyant plume
dynamics through application of mirroring principles; however, the present
version does not include sediment settling and deposition.
The current version of the CORMIX model requires some modifications to
extend its capabilities to simulate the characteristics of dredged material
discharges. Efforts are underway for adaptations of the CORMIX model for
simulating the mixing hydrodynamics of several types of dredged material
discharges. When these efforts are completed, the revised CORMIX model will
be included in subsequent revisions of this appendix.1
E.4 Macintyre Analytical Method for CDF
Discharge in Riverine Conditions
E.4.1 Introduction
This section presents a simplified approach that is applicable to relatively
shallow confined riverine water bodies. The method involves a simplistic two-
dimensional (2-D) calculation based on dispersion principles (MacIntyre 1987).
If the mixing-zone size as calculated using simple approximations is within
mixing-zone guidelines specified by regulatory agencies, more precise
calculations may not be necessary. The mixing-zone calculations depend on a
number of assumptions that are difficult to satisfy for estuaries and the tidally
influenced portions of rivers. The difficulties are discussed after the presenta-
tion of the procedure to be used for a riverine environment.
The analytical solution technique for calculating mixing-zone size described
in this section is based on theoretical and empirical relationships for dispersion
as summarized by Fischer et al. (1979). Only equations for calculating mixing-
zone size resulting from a single-point discharge are presented.
A schematic illustrating a typical single-source effluent discharging into a
receiving water body is shown in Figure E-1. For such a condition, the mixing-
zone length extends downstream and the body of the mixing zone remains close
to the shoreline of the receiving water body.
1
The latest release of CORMIX (Version 2.10) can be obtained without charge from
U.S. EPA Office of Research and Development, Center for Exposure Assessment
Modeling (CEAM), Athens Environmental Research Laboratory, 960 College Station
Road, Athens, Georgia 30605-2720. CORMIX can be either downloaded from CEAM's
on-line Bulletin Board System by calling 1-706-546-3402 (FTS 250 3402), or sent
through the mail by sending user-supplied diskettes or 9-track magnetic tapes to the
CEAM Model Distribution Coordinator at the above address. User documentation is also
available from the same source.
E6
Appendix E Evaluation of Mixing in Surface Waters

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