Estimations of plant water use can provide great assistance to growers, irrigators, engineers and water resource planners. This is especially true concerning the introduction of a new crop into irrigated agriculture. Growing hybrid poplar trees for wood chip stock and veneer production under agronomic practices is currently being explored as an alternative to traditional forestry practices. To this author's knowledge, no water use estimates or crop coefficients, the ratio of a specified crop evapotranspiration to a reference crop evapotranspiration, have been verified for hybrid poplars grown under drip irrigation. Four years of weekly, neutron probe measured, soil water data were analyzed to determine averaged daily, monthly and seasonal plant water use, or crop evapotranspiration. The plantation studied was located near Boardman, Oregon on the arid Columbia River Plateau of North-Central Oregon. Water was applied by periodic applications via drip irrigation. Irrigation application data, weekly recorded rainfall and changes in soil water content permitted the construction of a soil water balance model to calculate weekly hybrid poplar water use. Drainage was estimated by calculating a potential soil water flux from the lower soil profile. Sites with significant estimated potential drainage were removed from the analysis so that all sites used in the development coefficients were calculated using reference evapotranspiration estimates obtained from a nearby AGRIMET weather station. Mean crop coefficients were estimated using a 2nd order polynomial with 95% confidence intervals. Plant water use estimates and crop curves are presented for one, two and three year old hybrid poplars. Numerical simulation of irrigation practices was attempted using weekly soil water content and soil physical characterization data. Parameter optimization and numerical simulations were attempted using the HYDRUS-2D Soil Water and Solute Transport model. Parameter optimization and numerical simulations were largely unsuccessful due to lack of adequate soil physical and root zone system representation and dimensional differences between drip irrigation processes and the model design used in this study. / Graduation date: 1998

Veratrum californicum (common name: corn lily) is a wild plant species that grows in the Intermountain West, its range extending from British Columbia to Mexico. Corn lily is of interest because it has the potential to provide pharmaceutical precursors for use in the treatment of cancer. Pharmaceutical companies are currently running clinical trials of new drugs that use these precursors. As such, a sustainable supply of corn lily is needed if these drugs are ever to enter the market. Unfortunately, wild populations of corn lily will not be able to meet the market demand. Therefore, it is necessary that horticultural guidelines be established so that corn lily can be grown in an agricultural setting. Establishing irrigation criteria is one crucial component in this process, as corn lily grows in naturally wet areas and will most likely require supplemental irrigation in an agricultural setting. In order to determine the appropriate level of irrigation for corn lily, an appropriate range of irrigation levels to test in a field trial must be determined. Plant success as a function of irrigation level can then be measured. In order to determine what irrigation levels should be tested, the OSU Malheur Experiment Station monitored the natural environment of corn lily at a variety of locations over the course of four seasons. Results showed that for the majority of its growing season, corn lily occupies a narrow environmental niche where soil water tension ranges from 0 kPa to 30 kPa. With this information, irrigation levels ranging from 5 kPa to 30 kPa were chosen for irrigation trials. In 2009, corn lily plots were established at Ontario, Oregon and McCall, Idaho. Irrigation trials were run in 2010, 2011, and 2012 at Ontario and McCall. Plots were assigned to five irrigation treatments: 5 kPa (added halfway through the 2010 growing season), 10 kPa, 15 kPa, 20 kPa, and 30 kPa. Collectively, the data indicate that the 5 and 10 kPa treatments are most conducive to corn lily survival and growth. In addition, the observed data are consistent with the hypothesis that soil moisture levels in the first month of growth may be the most important determinant in plant growth and survival. / Graduation date: 2013

Water allocation in the upper Klamath Basin of Oregon and California has been challenging. Irrigators have increasingly turned to groundwater to make up for surface water shortages because of shifts in allocation toward in-stream flows for Endangered Species Act listed fishes. The largest increase in groundwater pumping has been in and around the Bureau of Reclamation's Klamath Irrigation Project, which includes the Tule Lake subbasin in the southern part of the upper Klamath Basin. Previous groundwater flow model simulations indicate that water level declines from pumping may result in decreased flow to agricultural drains in the Tule Lake subbasin. Agricultural drains on the Klamath Project are an important source of water for downstream irrigators and for the Tule Lake and Lower Klamath Lake National Wildlife Refuges. To better assess the impact of increased pumping on drain flow and on the water balance of the groundwater system, flow data from agricultural drains were evaluated to investigate the changes that have taken place in groundwater discharge to drains since pumping volumes increased. Additionally, a fine-grid groundwater model of the Tule Lake subbasin was developed based on the existing regional flow model. The fine-grid model has sufficient vertical and horizontal resolution to simulate vertical head gradients, takes advantage of time-series data from 38 observation wells for model calibration, and allows agricultural drains to be more explicitly represented. Results of the drain flow analysis show that the groundwater discharge to agricultural drains has decreased by approximately 4000 hectare-meters from the 1997-2000 average discharge. Most of this decrease takes place in the northern and southeastern portions of the subbasin. Results of the groundwater model show that the initial source of water to wells is groundwater storage. By 2006, approximately 56% of the water from wells is sourced from agricultural drains.