32
ERDC/CRREL TR-02-14
Table 2. Soil types at monitored sites. (From
Simon et al. 1999.)
Major soil
Riverbank toe
series
sediment
Site
Culbertson, RM 1621
Havrelon
Sandy silt
Tveit-Johnson, RM 1624
Lohler
Clay
Vournas, RM 1632
Banks
Sandy silt
Mattelin, RM 1646
Trembles
Sandy silt
Pipal, RM 1716
Havre
Sandy silt
through mid-April 1999. One bathymetric survey was completed before the ice
cover formed over the river. Two were conducted when the river was ice cov-
ered. A final bathymetric survey was carried out shortly after ice departed the
river in early spring. Two additional site visits were carried out to observe chan-
nel conditions before and after the river became ice covered. The survey dates
were as follows:
Fall observation of channel conditions and site selection (October 1417,
1998);
Early winter, open water channel bathymetric survey (October 1622,
1998);
Early winter observation of ice formation at RM 1621, Culbertson
(December 2023, 1998);
Early winter covered-channel bathymetric survey (January 2628, 1999);
Mid-winter covered-channel bathymetric survey (February 2123, 1999);
and,
Early spring open water bathymetric survey and observations (April 47,
1999).
The bathymetric surveys before freeze-up (cover formation) and shortly after
breakup (cover departure) revealed the extent to which ice affects channel
bathymetry. The two bathymetric surveys during winter provide insights as to
when and how the channel changes occurred. It was desirable, but not critical,
that the surveys be conducted when the river conveyed approximately the same
flow rate.