Comparison of Drainage Water Quality and Soil Salinity in Irrigated Areas with Surface and Subsurface Drainage Systems (original) (raw)

Impact of the Irrigation Water Use on the Groundwater Environment and the Soil Salinity

Aside from the positive impact of irrigation on increasing crop production, in the downstream part of a river basin, irrigation can cause salinity to build up with the increasing depth of the groundwater. The visible influence of the groundwater environment on soil resulting from irrigation can only be observed at the advanced stages of salinity buildup, when expensive measures must be implemented. Irrigation also can cause upstream and downstream problems, such as water shortages downstream, drainage problems, and the drainage of contaminants. Thus, in order to prevent soil salinization, it is very important to assess the impact of irrigation on the groundwater environment in arid and semiarid regions. This study was conducted in a large irrigation district that covers over 130,000 ha, in which soil salinization has occurred downstream. First, we studied the impact of irrigation water use on the groundwater environment. Then, we determined the effect of irrigation water use on soil...

An overview of impact of subsurface drainage project studies on salinity management in developing countries

Applied Water Science, 2015

Subsurface drainage has been used for more than a century to keep water table at a desired level of salinity and waterlogging control. This paper has been focused on the impact assessment of pilot studies in India and some other countries from 1969 to 2014. This review article may prove quite useful in deciding the installation of subsurface drainage project depending on main design parameters, such as drain depth and drain spacing, installation area and type of used outlet. A number of pilot studies have been taken up in past to solve the problems of soil salinity and waterlogging in India. The general guidelines that arise on the behalf of this review paper are to adapt drain depth [1.2 m and spacing depending on soil texture classification, i.e., 100-150 m for light-textured soils, 50-100 m for medium-textured soils and 30-50 m heavy-textured soils, for better result obtained from the problem areas in Indian soil and climatic conditions. An attempt has been made in the manner of literature survey to highlight the salient features of these studies, and it is hopeful to go a long way in selecting design parameters for subsurface drainage problems in the future with similar soil, water table and climatic conditions.

Subsurface Drainage Rates and Salt Leaching in Irrigated Fields

A field experiment to quantify the effect of subsurface drainage on soil salinity was conducted in a pilot area in the Nile Delta of Egypt. A clear relation was established between the crop cultivated in the drainage area of the lateral drains and the discharge characteristics (discharge and leached salts). The lowest rates were associated with wheat (in winter) and cotton (in summer), intermediate rates with berseem (in winter) and maize (in summer) and the highest rates with rice (in summer). The application of the water and salt balances showed that the area is subject to a natural drainage rate of about 0.5 mm/d. The difference between the amount of salts brought in by the irrigation water and the amount of salts leached from the soil profile indicate that during the monitoring period salt leaching from the deeper parts of the clay layer was still continuing.

Salinity and water table control in dry drainage

Irrigation without drainage is not sustainable. In certain circumstances, the conventional drainage solution may be questionable due to economic and/or environmental limitations. ‘‘Dry drainage’’, which is leaving parts of the land retired forever adjacent to the cropped land, has been postulated as an alternative (Konukcu et al. 2006). Water scarcity along with abundance of saline soils in arid and semiarid regions, makes it possible to retire parts of the land to control water table and accumulate salts in the retired parts of the land. While Gowing and Wyseure (1992) believe that the method is a sustainable and cost-effective solution, Konukcu et al. (2006) doubt about it. They indicate that the water table can be maintained at about 1.5 m if cropping is concentrated on 50% of the area. This general statement, however, is questionable because of the wide range of combination of soil, climate, water quality, surface conditions etc. The purpose of this research is to show where the dry drainage is effective and to verify its sustainability.

Drainage and salinity assessment in the Huinong Canal Irrigation District, Ningxia, China

Irrigation and Drainage, 2005

In the Huinong Canal Irrigation District, Ningxia, China, annually almost half of the amount of irrigation water, which is supplied from the Yellow River, is drained back to the river through an open drainage system. Waterlogging and salinization occur in parts of the irrigated area and part of the water drains to the surrounding desert. While 85-90% of inflow to the area is irrigation water there are good possibilities for water saving.

Drainage Water Salt Load Variations Related to the Salinity and Leaching Ratios of Irrigation Water

Tarım Bilimleri Dergisi, 2018

Solubility of salts and leaching fractions have different effects on drainage water quality. Knowing the quality of drainage water is extremely important in terms of environmental factors and quality of water resources for the reason that this water is transferred to various sources. In this study, were studied the changes of drainage water salinity and salt load under lyzimeter (soil columns) conditions using different irrigation water salinity and with different leaching fractions. The study was carried out with sunflower in PVC soil columns with 40 cm diameter and 115 cm length with 3 different irrigations and 5 irrigation waters with different salinity level. The three irrigation treatments were 75%, 115% and 135% of the required irrigation water. The irrigation water salinities were 0.25 dS m-1 as control treatment, 1.5 and 3.0 dS m-1 with NaCl+CaCl 2 salts and 1.5 and 3.0 dS m-1 with NaCl+CaSO 4 salts as saline treatments. In this study investigated drainage water quality variations and salt load with irrigation water and some individual ions load and their leaching by drainage water as well. Drainage water salinities variated with both irrigation water salinity and leaching fractions. It was higher under the effect of soluble salts and with the 15% leaching fraction. However, salt load was higher at 35% leaching fractions level. When discuss the individual ions; while Cl-, (CO 3-2 +HCO 3-) and Ca +2 were accumulated in the soil profile, SO 4-2 , Na + ve Mg +2 were leaced from the profile, and all these ions variated by interaction for irrigation waters, and by leaching fractions for the drainage water.

Monitoring and assessing of changes in soil and groundwater salinity of Yemisli Irrigation District of Turkey using low quality irrigation water

Scientific Research and …, 2011

Low irrigation efficiency, high saline irrigation water, heavy soil texture, lack of adequate field drainage systems may cause soil salinity and drainage problems in irrigated agriculture. The mentioned problems are major treats for the sustainability of irrigated agriculture. This study carried out in 2007 was undertaken in 7,110 ha of area under the directive of Yemisli Irrigation Association (YIA) in Lower Seyhan Plain, on Southern coastal plains in Turkey. Growers in the area use low quality irrigation return flows of upstream areas for irrigation. Irrigation method commonly used in the region is flood irrigation with low field irrigation efficiency. This work examines if using low quality of irrigation water causes drainage and soil salinity problem. For this purpose, a year around survey of 55 groundwater observation wells was carried out. Groundwater depths in the observation wells in February, March, June, July and October were measured. Salinity of the water samples collected from the wells was measured as electrical conductivity (ECw at 25°C). Additionally, soil samples from 0 to 30, 30 to 60 and 60 to 90 cm depths at 34 randomly selected sites were analyzed for soil salinity (ECe at 25°C) and alkalinity (SAR). The mean groundwater depth was the minimum (0.97±0.29 m) in March, before starting of the irrigation season. In October, following completion of the irrigation season, the groundwater depth was the highest (1.59 ± 0.13 m). Groundwater EC, greater than 20 dS m-1 , was noted commonly. In 93% of the study area, ECw was higher than 5 dS m-1. Mean soil salinity ECe was higher below 1 m depth compared with that of surface layers. Likely occurrence of soil alkalinity (that is, sodium effect) was greater in subsoil below 30 cm depth compared with surface layers. The results of the study showed that the soils of the area may become salt or even sodium affected in the future unless the present practice of irrigation management is changed.

EFFECT OF VARYING SALT CONCENTRATIONS AND Na / Ca RATIOS IN THE IRRIGATION WATER ON THE SOIL SALINITY

The current study was conducted on two soils extremely varied in their textures ; i.e. sandy ( Meet Kennana area , Qalubia Governorate ) and clay soils ( El-Zankalon area , Sharkia Governorate ) to investigate the effect of saline irrigation water on soil salinity levels , as expressed by the ECe values in the saturation extract of these soils . Three irrigation water treatments containing total salt concentrations of 1000 ,2000 and 4000 ppm were used for irrigation. Moreover ,each of these salt concentrations contained three different ratios of Na / Ca, i.e. , 1 : 1 , 2 : 1 and 4 : 1 . The results revealed that increasing the total salt concentrations in irrigation water led to increase in soil salinity . Also , the Na / Ca ratios in the water did not cause in any significant difference in ECe . Salt accumulation in clay soil was much greater than in the sandy one. So, saline water could be used with a more efficiently under coarse textured soils . The period of irrigation was also greatly effected on the amounts of accumulated salts in both soils . The longer the period the higher will be the quantity of accumulated salts . The statistical analysis confirmed the above-mentioned results .

Soil Salinity and Its Management

Soil Moisture Importance, 2021

Soil salinity is a growing threat all over the world due to its toxic effect to reduce soil fertility and water uptake in the crops. An average of 418 million ha soil is saline in nature. Various climatic, geomorphic and rainfall pattern causes which involved in saline soil formation. To reduce the toxic effect proper management of saline soil is required. Irrigation water also a major concern regarding soil salinity management. Saline irrigation water enhances and maintains the severity soil salinity. Crop production aspects root zone salinity provides a strong negative impact on soil fertility. Salinity causes the reduction in nutrient ion, and water uptake has a significant negative effect on crop yields. Soil and water salinity interactions and their influence on crop growth and management of salinity are deliberated in this chapter.

The effect of water quality and irrigation methods on moisture and salinity distribution of soil

Current study was carried out with aim to evaluate the effect of pressurized irrigation methods and furrow irrigation method with municipal effluent on distribution of salinity and moisture in the soil profile. The experimental study was designed by split plot layout with three irrigation methods including furrow, surface drip (SD) irrigation and subsurface drip irrigation (SSD) and two water qualities (municipal effluent and fresh water) in a sugar beet field located in Corbal plain, Iran. Soil sampling was conducted in two sessions (prior to irrigation and after harvesting) at three depths of 0-20, 20-40, 40-60 cm and 15 points around areas where water leaked. Variance analysis of salinity showed a significant difference (p < 0.01) between irrigation methods, also between two water qualities in terms of salinity concentration, for three sampled depths of soil. The maximum value of salinity was found at the depth of 0-20 cm in subsurface drip irrigation by 1.66 dS/m, and the minimum value of salinity was found at the depth of 20-40 cm in furrow irrigation by 0.92 dS/m. Irrigation by municipal effluent caused a higher salinity concentration in the soil compared to fresh water regardless to the amount of water. Leaching operations, reducing the irrigation period and increasing the irrigation frequency, conducting researches and promoting the use of effluent are recommended in conclusion.