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Long-term prediction of regional groundwater and salt dynamics is important for the agricultural sustainability in Hetao Irrigation District, where the water resources supply and demand contradiction is prominent. The mulched drip irrigation with the well-canal conjunctive irrigation will be applied to save water and control soil salinity. In this study, the improved mass balance model SaltMod by a loosely coupled strategy was used to simulate the long-term groundwater and salt dynamics under current situation and future situation under well-canal conjunctive irrigation with mulched drip irrigation to evaluate the agrucultural sustainability. In the loosely coupled model, 2 SaltMod models were used to simulate the canal-and well- irrigated areas separately. An exchange flux was added in the aquifer mass balance equation to link the canal- and well-irrigated areas. The improved SaltMod could handle with multiple irrigation sources and different groundwater levels in the groundwater aquifer, which makes it possible to be used in the well-canal conjunctive irrigated areas. Then the model was calibrated and validated with 15 years' observation data of the Longsheng well-canal irrigated area in Hetao Irrigation District, Inner Mongolia, China. The data in years between 2002 and 2005 were used as the calibration period and 2006—2016 were used as the validation period. Root mean squared error (RMSE) and relative error (RE) were used to evaluate the results. The results showed that the improved model performed well for calculating the groundwater depth and soil salinity for both canal-and well- irrigated areas. Then the model was used to predict the water flow and soil salinity dynamics in the next 100 years under the current irrigation condition. The results showed that it could sustain a long-term stabilization under the present irrigation practice in the Longsheng well-canal irrigated area. Then the model was applied to simulate the water and salt dynamics with different senarios under the well-canal conjunctive irrigation and the mulched drip irrigation. With the satisfactory result of soil salinity in the canal-irrigated area, the well-irrigated area was the concern, especially the root zone in the well-irrigated area. Different autumn irrigation frequency schemes, irrigation quotas in the crop growing season, groundwater depth in the well irrigation area and groundwater mineralizations were considered to be the impact factors on the soil salinity in the root zone of the well irrigation area. The results showed that, the irrigation quota and groundwater depth had little effects on the variation trend of soil salinity in the root zone of well irrigation area. The autumn irrigation frequency scheme and groundwater mineralization played very important roles on the variation trend of soil salinity. When the autumn irrigation frequency (AIF) was once every two years and the groundwater mineralization increased to 2.0 g/L, the root zone soil salinity would still be less than 3.0 g/kg after 100 years. It would exceed 3.0 g/kg after 60 years when the groundwater mineralization increased to 2.5 g/L. Considering the groundwater mineralization of 90% well-canal irrigated area was less than 2.0 g/L, we recommended that when exploiting groundwater for irrigation in Hetao Irrigation District, it was necessary to apply the water from Yellow River for autumn irrigation to wash out the soil salt. The autumn irrigation frequency was once every two years and the autumn irrigation quota was 180 mm. [ABSTRACT FROM AUTHOR]

To understand the salt movement mechanism in the freezing-thawing soil and the salt transport in the frozen layer, an experiment is carried out in Yonglian experiment station, Hetao Irrigation District, China. The soil temperature, frozen layer depth, water table depth, groundwater salinity and the ion components, soil water content and soil salinity and its ion components during the freezing-thawing period were observed and measured. The data were analyzed to demonstrate the soil salt transport variations in the soil and groundwater as well as its impact factors. The correlation analysis was implemented to calculate the relationship between the soil content and the ion components and the relationship among those ions, and then to obtain the major ions and major salt composition of the soil soluble salts to control soil salt change. The transport mechanism of soil soluble salts in the freezing-thawing soil was discussed by using the binary phase diagram of water-salt system. The experiment results show that the soil temperature change within the depth of 0-1.0m. There are three stages during the freezing-thawing period in the study area as quickly freezing period (from December 6th, 2017 to February thh, 2018), slowly freezing period (from February 4th, 2018 to March 12th, 2018) and thawing period (from March 12th, 2018 to April, 13th, 2018). The water table depth showed the change as quick increase-slow increase-decrease in the 3 stages, while the average groundwater salinity significantly decreased. Na+, Cl– and SO42– had the greatest variability among all the 8 ions both in the groundwater. These demonstrated that the ions change in the groundwater was caused by the advection of ions in the soil solute. The correlation coefficients of Na+, Cl–, SO42– with soil salt content were larger than 0.9, and the correlation coefficients among Na+, Cl–, SO42– were larger than 0.9, which showed the major ion components of soil salt were Na+, Cl– and SO42–, and the major soil soluble salts were sodium sulfate and sodium chloride. The soil salt transport in the frozen layer depended on the initial soil salt gradient and co-saturated points of sodium sulfate and sodium chloride. The max mass fractions of sodium sulfate and sodium chloride were 2.01% and 1.55%, smaller than their co-saturated points. In this case, the salt would accumulate in the frozen layer when the initial soil salt gradient was positive (the salt content increase along depth). Otherwise, the soil salt would decrease in the frozen layer. This work is significant important to illustrate the relationship between the ion components with the soil salt change and the salt accumulation mechanism in the frozen layer. [ABSTRACT FROM AUTHOR]