Depletion of the Southern High Plains Aquifer: Simulating the Effects of
Conserving Irrigation Water through Reduced Irrigated Area and Limited
Application
Abstract
Groundwater resources of the Southern High Plains/Ogallala Aquifer in
Texas and New Mexico are being depleted due to groundwater mining for
irrigation. Inevitably, resource depletion leads to calls for water
conservation in agriculture. Conservation can take two forms: a
reduction in irrigation depth, and a reduction in irrigated area, which
in economics are termed the “intensive margin” and “extensive
margin” of agricultural water use. In the Southern High Plains, we find
different effects on water table elevation arising from these two
approaches. This research presents a coupled model of landscape and
groundwater hydrology. Model results indicate that a 50% reduction in
irrigation water application would limit loss in irrigable area to about
1% of existing irrigable land per year. This is approximately half the
rate of depletion from a ‘business as usual’ scenario. Relative benefits
of each conservation approach varied: areas with a high density of
irrigated land experienced greater benefits from a reduction in
irrigation depth, whereas reducing irrigated acreage maintained water
tables more in areas with a low density of irrigated land. This project
demonstrates that strategies for irrigation water management can support
conservation goals. However, model results also demonstrated that even a
50% reduction in irrigation water use –which would be politically and
economically unfeasible in Texas and New Mexico – would still result in
overall depletion of the regional aquifer.