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A field subirrigation experiment, using saline-sodic water, was carried out on a loamy sand soil in southwestern Quebec. The experimental field was divided into 16 plots with 4 treatments; saline-sodic water, "fresh" water, controlled drainage and non-irrigated. Each treatment had four replicates. Maize yield, hydraulic conductivity, salt concentration, and salt movement through the soil were recorded in all plots. / No significant difference in maize yield occurred between plots irrigated with saline-sodic or fresh water in any of the three years. Irrigated maize plots yielded approximately 30% more than non-irrigated plots. / Hydraulic conductivity reductions in the saline plots were noted in May 1986, after the first snowmelt. From statistical analysis carried out, it appears that the saline-sodic water had an effect on hydraulic conductivity, significant at the 0.05 level. / From the measurements taken from piezometer stations, located throughout the field, salt concentrations and salt movement through the saturated soil profile were determined. Using salt concentration data from both irrigation water and soil water, an average effective field porosity was calculated with a computer program. The results obtained were within 4% of those obtained in laboratory tests. Moreover, the program was then used to model the salt balance of the soil from May 85 to May 87. Results indicated that most salts were removed with the rainfall and snowmelt of the winter months of 85/86 and 86/87.

A field study was conducted for two years in three semi-arid regions of Syria in order to define, under field conditions, the wheat (Triticum aestivum L.) yield response function to irrigation water salinity and to study the process of soil salt accumulation. The three regions experience similar climatic conditions (semi-arid Mediterranean climate) but have different soil textures, varying from sandy loam to clay. The study involved 74 farms all of which had been irrigating for more than 3 years prior to this study, with well water of different salinity values (0.44 to 14.1 dS/m). All of these farms operated with similar cultural practices. / Results indicate that the wheat yield response function to irrigation water salinity differs between the three regions. The irrigation water threshold salinity value beyond which wheat yield started to decline, was found to be 6.5 dS/m, 3.5 dS/m and 1.2 dS/m in the Khabur low plains; Aleppo south plains and Shedadeh area respectively. Wheat was more salt tolerant to irrigation water salinity in sandy loam soils than clay loam soils. The three threshold values obtained in this study are different from the "universal" value of 4 dS/m which is proposed in current literature. The "universal" value was obtained from artificially salinized field plots seeded under non-saline conditions. / In addition, it was found that salt accumulation in the soil profile increases as soil clay content increases. / The results demonstrate the necessity of establishing regional water quality criteria when planning the use of saline water sources for irrigation in semi-arid regions.

Typescript. / Thesis (Ph. D.)--University of Hawaii at Manoa, 1979. / Bibliography: leaves 145-157. / Microfiche. / xii, 157 leaves ill. 29 cm

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Thesis (PhD (Soil Science))--University of Stellenbosch, 2005. / Approximately 45% of apricot tree plantings in South Africa are centered on Montagu, Koo and Barrydale in the Little Karoo. Below average production in this area could be ascribed to the deteriorating water quality of the Breede River and highly saline groundwater from boreholes which provide this area with irrigation water. Profit margins for farmers are such that decreased yields cannot be tolerated. Correct management of low quality water could improve production and net farm income and could decrease irrigation return flow into the river system. The objective of this work was to establish whether international water quality guidelines for apricot are applicable under a different set of climatic conditions for a locally important cultivar and to revise guidelines if necessary for the management of irrigation with saline water. A drainage lysimeter was used to evaluate the effect of saline irrigation on apricot (Prunus armeniaca cultivar Palsteyn) trees over a period of four years at Stellenbosch (S33° 55’; E18° 53’) in the Western Cape.