Source: COLORADO STATE UNIVERSITY submitted to
MULTIDISCIPLINARY RESEARCH ON SALINITY ISSUES IN THE ARKANSAS RIVER VALLEY
Sponsoring Institution
National Institute of Food and Agriculture
Project Status
TERMINATED
Funding Source
Reporting Frequency
Annual
Accession No.
0192939
Grant No.
(N/A)
Project No.
COL00694
Proposal No.
(N/A)
Multistate No.
(N/A)
Program Code
(N/A)
Project Start Date
Jul 1, 2002
Project End Date
Jun 30, 2006
Grant Year
(N/A)
Project Director
Garcia, L. A.
Recipient Organization
COLORADO STATE UNIVERSITY
(N/A)
FORT COLLINS,CO 80523
Performing Department
ADMINISTRATION
Non Technical Summary
Upward flow from high water table has salinized the rich soils of the Arkansas River Valley causing crop yields to diminish and threatening socioeconomic stability. The research will be conducted by interdisciplinary teams of scientists which focus on: (a) data collection and modeling to assess the problems and predict the response of the system to alternative solutions; (b) develop a drip irrigation experimental site; and (c) expanding the emphasis on important social and economic elements and constraints.
Animal Health Component
(N/A)
Research Effort Categories
Basic
20%
Applied
80%
Developmental
(N/A)
Classification

Knowledge Area (KA)Subject of Investigation (SOI)Field of Science (FOS)Percent
1030110206115%
1110210202015%
1120210202015%
2050320202015%
4050210202015%
6016199301015%
8056030308010%
Goals / Objectives
As part of this project, research will be conducted to address problems associated with salinity in the Arkansas River Valley. The research will be conducted by interdisciplinary teams of scientists which focus on: (a) data collection (soil characteristics, aquifer properties, irrigation practices, depth to water table and water table salinity, soil salinity, crop yields) and modeling (field scale and sub-regional scale) that forms the essential foundation for accurately assessing the problems and for predicting the response of the river-valley system to alternative solutions; (b) develop a drip irrigation experimental site; and (c) expanding the emphasis on important social and economic elements and constraints. Together, these subprojects constitute a three-year multidisciplinary thrust to diagnose and solve irrigation-induced salinity, waterlogging, and pollutant loading problems in the lower Arkansas River Valley. Our aim is to coordinate our research efforts in a manner that will sustain the natural resource base for productive irrigated agriculture, support broader socioeconomic revitalization, and enhance the riverine environment. This project contains seven sub projects. The seven sub-projects are: 1) Social Benefits and Costs of Salinity Control in the Arkansas River Valley; 2) Correlation of Direct and Indirect Methods of Salinity Assessment in the Arkansas River Basin, Colorado; 3) Subregional-and Basin-Scale Technical Assessment of Irrigation-Induced Salinity and Pollutant Loading in the Arkansas River Valley; 4) Characterization of Soils for Field Scale Modeling of Salinity; 5) Organizational Analysis for Salinity Problem in the Arkansas Valley; 6) Digitizing for Update of Otero County Soil Survey Maps and Interpretation Data; and 7) Salinity Management in the Arkansas Valley with Drip Irrigation.
Project Methods
The approach that will be followed by the seven teams includes a mixture of laboratory experiments and data collection, field data collection, computer modeling, and data analysis and evaluation. The laboratory experiments will focus on characterizing soil properties for fields in the study area, and determining the salinity of the soils by analyzing core and soil samples collected at 100-200 locations in the area. The modeling will be based on numerical models for the field and sub-regional scales for water and salt movement. Also, spatial modeling will be conducted to estimate crop yields and for an integrated basin wide crop production model. A drip irrigation site will be established and data will be collected on salinity impacts of different irrigation regimes, yield impacts and cost of production. Data will be collected at regular time intervals (weekly during the growing season and monthly during the rest of the year) for water table elevation and groundwater salinity at points distributed through two sub-regions in the Arkansas River Basin. In addition, data will be collected on surface water salinity (irrigation and drainage) and aquifer characteristics will be estimated using pumping tests. To support some of the modeling efforts, soil maps (1:24,000) for some of the sub-regions of the study area will be digitized. In order to understand some of the organization issues related to this problem, key factors believed to be underlying reduced organizational cooperation in the valley to address salinity control, and ways to increase coordinated efforts on part of all organizations will be analyzed.

Progress 07/01/02 to 06/30/06

Outputs
This project uses various methods to attempt to diagnose and solve irrigation-induced salinity, waterlogging, and pollutant loading problems in the lower Arkansas River Valley in Colorado. High water tables are a factor in the region's salinity problems. Thousands of measurements of water table depth have been taken at wells around the study area. Water table depth has been found to vary greatly with the amount of precipitation and irrigation water available in the area. Irrigation has also been investigated as a factor in the salinity problem. Hundreds of irrigation events have been monitored to determine the amount of water applied to a given field, the amount of runoff, and the amount of deep percolation. Soil salinity has been examined. Soil samples from the area were collected an analyzed, and a correlation between soil salinity measurements from Electro Magnetic (EM) readings and laboratory ECe measurements was developed, allowing for a significant reduction in the amount of time it takes to determine soil salinity in a field. Soil properties, including texture and density have been analyzed, and the local soil survey maps were digitized in preparation for updating. Several models of different scales, including the basin scale, have been developed to investigate the effects of salinity and to examine the expected impact of various improvement strategies including: increased irrigation efficiency, altered pumping rates, canal lining to reduce seepage, subsurface drainage, and combinations of these alternatives. The models predict the impacts on water table depth, water table salinity, soil salinity, crop yields, return flow and salt loads to the river, and upflux from the shallow water table to nonbeneficial consumptive use. The basin scale model integrates artificial neural networks for estimating return flows to the river, based upon regional-scale model results, into the MODSIM-Q network model for routing flows and salt loads along the river. Finally, an economic model of crop production for existing acreage allocations in the Arkansas River Valley is in development. The model shows how changes in salt levels that are external to the farm influence on-farm profits, production levels, and water applications. Mathematical simulations of agricultural production indicate that saline conditions cost producers signficantly. More dynamic responses by growers may help or hurt the farmer's bottom line. Changes in irrigation technology due to saline conditions are of particular concern, since parallel econometric results indicate a positive and significant effect on the adoption of more advanced sprinkler irrigation systems when irrigators perceive soil salinity as an on-farm problem.

Impacts
Solution alternatives considered show promise both for boosting agricultural productivity on the land and enhancing the environmental health of the river. Results from the study suggest that strategies to reduce recharge to the water table by improving irrigation efficiency and reducing canal seepage would (a) lower the saline high water table leading to lower soil salinity and increased crop yields, (b) significantly reduce loading of salts and other pollutants to the river, and (c) markedly reduce nonbeneficial consumptive use under fallow land. As the results of this study are conveyed to farmers and land managers at public meetings and through demonstrations and publications, the stakeholders can make well-informed decisions about the adoption of techniques and technology while keeping in mind their economic bottom line.

Publications

  • Gates, T. K., Burkhalter, J. P., Labadie, J. W., Valliant, J. C., and Broner, I. 2002. "Monitoring and modeling flow and salt transport in a salinity-threatened irrigated valley". Journal of Irrigation and Drainage Engineering, ASCE, 128(2): 87-99.
  • Huber, D., G. Butters, and M.E. Stromberger. 2003. Short-term Effects of Poor Water Quality on Hydraulic Conductivity. In Annual meeting abstracts [CD-ROM]. ASA, CSSA, and SSSA, Madison, WI.
  • Burkhalter, J. P., and Gates, T. K. 2005. "Agroecological impacts from salinization and waterlogging in an irrigated river valley". Journal of Irrigation and Drainage Engineering, ASCE, 131(2): 197 - 209.
  • Burkhalter, J. P., and Gates, T. K. 2006. "Evaluating regional solutions to salinization and waterlogging in an irrigated river valley." Journal of Irrigation and Drainage Engineering, ASCE, 132(1): 21-30.
  • Wittler, J. M., Cardon, G. E., Gates, T. K., Cooper, C. A., and Sutherland, P. L. 2006. "Calibration of electromagnetic induction for regional assessment of soil water salinity in an irrigated valley". Journal of Irrigation and Drainage Engineering, ASCE, 132(5): 436-444.
  • Garcia, L.A., Foged, N., and Cardon, G. (2006) "A GIS-Based Model to Estimate Relative Reduction in Crop Yield Due to Salinity and Waterlogging: Philosophy and Development." ASCE Journal of Irrigation and Drainage Engineering, 132(6) 553-563.
  • Gates, T.K, L.A. Garcia, and J.W. Labadie (2006). "Toward Optimal Water Management in Colorado"s Lower Arkansas River Valley: Monitoring and Modeling to Enhance Agriculture & Environment." Colorado Agricultural Experiment Station, Technical Report TR-6-10.
  • BERRADA, A., HALVORSON, A.D., BARTOLO, M., VALLIANT, J. (2006). "The effect of subsurface drip and furrow irrigation on the movement of salts and nitrate in the root zone." Irrigation Associations Exposition and Technical Conference Proceedings. P. 1-13.
  • HALVORSON, A.D., BARTOLO, M., REULE, C.A., BERRADA, A. (2006). "Onion Response to nitrogen fertilization under drip and furrow irrigation." Proceedings National Allium Research Conference. December 7-8, 2006, College Station, TX p. 73-78.
  • HALVORSON, A.D., BARTOLO, M., REULE, C.A., BERRADA, A. (2006). "Onion response to nitrogen fertilization under drip and furrow irrigation." Proceedings of Great Plains Soil Fertility Conference. Denver, CO, March 7-8, 2006. Kansas State University, Manhattan, Potash and Phosphate Institute. Brookings, SD. 11:7-12.


Progress 01/01/05 to 12/31/05

Outputs
Extensive data collection continued in the 2005 season. In 2005 one of the major activities of this project was to concentrate in collecting detailed data on irrigation depths for 24 fields in the Arkansas Valley. Flumes were installed to measure the volume of water that was applied to each field as well as the volume of runoff from the fields. Over 100 irrigation events were evaluated in these fields and the application depths that were computed varied from 1.1 inches to 32.3 inches with the average being 7.3 inches. The runoff or outflow depths computed varied from 0.0 inches to 6.7 inches with the average being 0.8 inches. Based on the difference between the application depth and the runoff depth we calculated the infiltrated depths. The infiltrated depths varied from 1.1 inches to 31 inches with the average being 6.5 inches. This information has provided us with valuable insights into the distribution of irrigation amounts. Given that we had over 100 events we are studying if there are any meaningful temporal variations (differences between early, middle and late season) in irrigation practices. We are also using this information to estimate the deep percolation which will be very valuable for our field and regional scale modeling of groundwater return flows. We also collected biomass samples in all these fields and are developing relationships of soil salinity and biomass production for the Arkansas Valley.

Impacts
The information we collected last year on infiltration and outflow depths provides us with the first extensive data set of real data of irrigation practices in the Arkansas Valley. Given that over 100 irrigation events were monitored we are using this data in both our field scale as well as our regional modeling. More importantly it showed that the amount of surface outflow from the irrigation events is fairly limited (the average was 0.8 inches per event). Colorado has been in a severe drought and farmers might have altered their irrigation practices to maximize the use of their water. We are using the data collected to estimate the deep percolation which is a key parameter in our modeling of the groundwater modeling. The data we are collecting is invaluable in allowing us to calibrate our models based on extensive real data.

Publications

  • No publications reported this period


Progress 01/01/04 to 12/31/04

Outputs
Extensive data has been collected on to In Summer and Fall of 2004, laboratory and field work continued on assessing the impact of water quality changes on soil hydraulic properties of selected Arkansas Valley soils. The focus of the laboratory studies has been 1) comparison of chemical and water flow properties of soils sampled from high, medium, and low salinity regions (completed), and 2) evaluation of the change in water retention and hydraulic conductivity with changes in soil water EC and SAR (near completion). In the field, in-situ infiltration measurements were completed using water of contrasting EC to explore if lower EC water can be expected to cause reductions in the infiltration rates. These measurements were performed on soil with and without a surface application of gypsum (a recommended additive to prevent dispersion of soil particles and hence maintain infiltration rates against surface sealing when using low EC or high SAR irrigation water).

Impacts
The calibration that is underway for the EM probe will offer a reliable method of monitoring the management of soil salinity throughout this important agricultural region in a much faster and economical way. Based on the mathematical simulation models of agricultural production in the Arkansas River Basin conducted as part of this project, it appears that saline conditions cost producers approximately $94/acre in lost profits. However, these results are conditioned upon existing cropping patterns and irrigation systems. The measurement of soil hydraulic properties provides valuable information for field and basin scale modeling of irrigation and drainage in the Arkansas Valley. The characterization of soil properties in zones of high, medium, and low salinity allows for refinement of model input in accordance with soil salinity maps. The fundamental information on soil response to changing water quality, coupled with "what if" modeling scenarios, provides important insight to the effects of future changes in soil salinity. The field infiltration measurements provide a practical demonstration to farmers of the changes in water intake that can be anticipated in the event of a change in irrigation water quality.

Publications

  • No publications reported this period


Progress 01/01/03 to 12/31/03

Outputs
This project is comprised of several subprojects that attempt to diagnose and solve irrigation-induced salinity, waterlogging, and pollutant loading problems in the lower Arkansas River Valley in Colorado. One of the subprojects consists of measuring water table depth and salinity in the two major river reaches in the valley and using the information to model the system and evaluate possible solutions. Work has continued in calibrating, refining, and applying a regional-scale flow and salt transport model for the upstream study region near La Junta. The model has been used to examine the expected impact of several improvement strategies: increased irrigation efficiency, altered pumping rates, canal lining to reduce seepage, subsurface drainage, and combinations of these alternatives. The model predicts impacts on water table depth, water table salinity, soil salinity, crop yields, return flow and salt loads to the river, and upflux from the shallow water table to nonbeneficial consumptive use. A regional-scale steady-state flow and salt transport model currently is being developed and calibrated toward allowing similar investigations in the study region near Lamar. Major progress also has been made in developing a basin-scale model of the Lower Arkansas River. The model integrates artificial neural networks for estimating return flows to the river, based upon regional-scale model results, into the MODSIM-Q network model for routing flows and salt loads along the river. A second subproject involves developing a correlation between soil salinity measurements from Electro Magnetic (EM) readings and Laboratory ECe measurements. All lab analysis for ECe has now been completed for the upstream reach (years 1999 through 2003) and downstream reach (years 2002 and 2003). Soil texture is underway on remaining samples from the 1999 upstream study sites. In 2003, sampling for soil bulk density was undertaken on a large scale. Triplicate undisturbed soil cores using a hydraulic insertion probe were collected from approximately 40 upstream sites. Bulk density data will allow expression of water content on a relative saturation basis, thereby normalizing water content information in correlation analysis with field salinity probe data. Complete correlation analysis is expected to be completed in 2004. Once calibrated, the EM probe will offer a reliable method of monitoring the management of soil salinity throughout this important agricultural region. Another subproject deals with the development of an economic model of crop production for existing acreage allocations in the Arkansas River Valley. Based on mathematical simulation models of agricultural production in the Arkansas River Basin, it appears that saline conditions cost producers signficantly in lost profits. More dynamic responses by growers may increase or decrease these potential gains. Changes in irrigation technology due to saline conditions are of particular concern, since parallel econometric results indicate a positive and significant effect on the adoption of more advanced sprinkler irrigation systems when irrigators perceive soil salinity as an on-farm problem.

Impacts
The calibration that is underway for the EM probe will offer a reliable method of monitoring the management of soil salinity throughout this important agricultural region in a much faster and economical way. Based on the mathematical simulation models of agricultural production in the Arkansas River Basin conducted as part of this project, it appears that saline conditions cost producers approximately $94/acre in lost profits. However, these results are conditioned upon existing cropping patterns and irrigation systems.

Publications

  • Cardon G.E. 2003. Salinity Issues in Colorado. In: Berrada, A. and T. Houten (eds), Proceedings of the Third Annual Four Corners Irrigation Workshop. Colorado Agric. Exp. Station, Limited Technical Bulletin LTB03-1. pp 27-32.
  • Wittler, J, C. Cooper and G.E. Cardon. 2003. Calibration of Electromagnetic Salinity Probes in an Irrigated, Gypsum-Dominated System. Poster Presentation. American Society of Agronomy annual meeting, Nov 2-6, 2003, Denver, CO. Agron. Abstracts. ASA, Madison, WI.


Progress 01/01/02 to 12/31/02

Outputs
This project is comprised of several subprojects that attempt to diagnose and solve irrigation-induced salinity, waterlogging, and pollutant loading problems in the lower Arkansas River Valley in Colorado. One of the subprojects consists of measuring water table depth and salinity in the two major river reaches in the valley and using the information to model the system and evaluate possible solutions. Over the 2002 irrigation season, the average measured water table depth in the river reach between Manzanola and La Junta was about 2.80 m, an average increase of about 1 m over measured depths in 2001. The average measured water table salinity over the season was about 3.17 dS/m (2800 mg/L) in 2002, an average decrease of 0.46 dS/m (410 mg/L) compared to 2001. Both of these values show significant improvements and most of the improvement is probably because of the drought and the reduction in irrigation flows. In the river reach between Lamar and Holly, estimates of measured water table depth and salinity were 3.05 m and 4.86 dS/m (4300 mg/L). A second subproject involves developing a correlation between soil salinity measurements from Electro Magnetic (EM) readings and Laboratory ECe measurements. The EM readings are much faster and if a correlation can be developed this would help significantly reduce the time it takes to determine the soil salinity for a field. Preliminary correlations between lab ECe and field EM readings have been developed and the preliminary results show strong correlations. Best agreement was found with a quadratic formulation (vertical orientation, r-square=0.76; horizontal orientation, r-square=0.75). Measuring water quality effects in salinized soils is the third subproject. An experimental setup has been developed to obtain information on the salinity-water quality interactions on hydraulic properties of Arkansas Valley soils (using a continuous flow method developed at Colorado State University). The experiment has been set up, and the hydraulic properties of 16 samples have been determined. A fourth subproject deals with the development of an economic model of crop production for existing acreage allocations in the Arkansas River Valley. Currently a working static model of the basin's agricultural production as a function of ambient salt levels has been developed. This model shows how changes in salt levels that are external to the farm influence on-farm profits, production levels, and water applications. The fifth subproject deals with the digitizing a portion of the Soil Survey maps of the area. A procedure to do this has been developed, and about 15% of the digitizing has been completed.

Impacts
Solution alternatives considered thus far show promise both for boosting agricultural productivity on the land and enhancing the environmental health of the river. Results from the upstream study subregion suggest that strategies to reduce recharge to the water table by improving irrigation efficiency and reducing canal seepage would (a) lower the saline high water table leading to lower soil salinity and increased crop yields, (b) significantly reduce loading of salts and other pollutants to the river, and (c) markedly reduce nonbeneficial consumptive use under fallow land. This proposition will be verified and refined by data-calibrated subregional and basin-scale modeling. The relationships, thus far, are quite different from those previously established for the EM method in California and Australia and indicate the need for localized calibration. Drought conditions in Colorado for 2002 were the worst in recorded history, resulting in little irrigation water and very dry soils throughout the year. The influence of moisture, compounded by the sandier textures of soils in the downstream reach, will continue to be investigated in 2003. The preliminary results hold promise of an effective, reliable correlation between standard labor-and time-consuming laboratory salinity analysis, and the rapid field EM methods. Once calibrated, the EM probe will offer a reliable method of monitoring the management of soil salinity throughout this important agricultural region where estimates of crop yield reduction due to salinity average 10 to 30%

Publications

  • No publications reported this period