Agricultural irrigation has a substantial impact on water quantity and
quality in the lower Arkansas River valley of southeastern Colorado,
A two-dimensional now and solute transport model was used to evaluate
the potential effects of changes in irrigation on the quantity and qua
lity of water in the alluvial aquifer and in the Arkansas River along
an 17.7 km reach of the river, The model was calibrated to aquifer wat
er level and dissolved solids concentration data collected throughout
the 24 year study period (1971-95). Two categories of irrigation manag
ement were simulated with the calibrated model: (1) a decrease in grou
nd water withdrawals for irrigation; and (2) cessation of all irrigati
on from ground water and surface water sources, In the modeled categor
y of decreased irrigation from ground water pumping, there was a resul
ting 6.9% decrease in the average monthly ground water salinity, a 0.6
% decrease in average monthly river salinity, and an 11.1% increase in
ground water return flows to the river, In the modeled category of th
e cessation of all irrigation, average monthly ground water salinity d
ecreased by 25%; average monthly river salinity decreased by 4.4%; and
ground water return nons to the river decreased by an average of 64%.
In all scenarios, simulated ground water salinity decreased relative
to historical conditions for about 12 years before reaching a new dyna
mic equilibrium condition, Aquifer water levels were not sensitive to
any. of the modeled scenarios, These potential changes in salinity cou
ld result in improved mater quality for irrigation purposes downstream
from the affected area.