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Research Detail

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A. Khatun
Chief Scientific Officer and Head, IWM Division, BARI, Gazipur 1701

K. K. Sarker
Scientific Officer, IWM Division, BARI, Gazipur 1701

S. S. A. Kamar
Scientific Officer, RARS, BARI, Rahmatpur, Barishal

M. Mainuddin
Principal Research Scientist, CSIRO Land and Water, Canberra, ACT

Farmers are being encouraged to represent the conjunctive use of fresh water (FW) and saline water (SW) irrigation for the future of agriculture in the coastal saline prone areas of Bangladesh. Therefore, the conjunctive use of fresh and saline water irrigation experiments for maize were performed over two years of 2016-2017 and 2017-2018 at the farmers' field of the village of Pankhali and Khatail at Dacope, Khulna and Sikandorkhali at Amtali, Barguna. The objectives of this study were (i) to evaluate the effect of soil moisture, soil salinity (ECe), osmotic pressure, pH and plant biomass at different growth stages, (ii) to assess the effect of fresh and saline water irrigation on the crop performances, water use and water productivity and (iii) to find out the scope of saline and fresh water irrigation for maize crop cultivation. The experiments were carried out in two farmer’s field at Pankhali and three farmers’ field with six irrigation treatments and replicated thrice. The treatments were: (i) T1:2 irrigations (IR) at vegetative stage and grain development stages with FW;  T2:2 IR at vegetative stage with FW and grain development stage with SW; T3: 2 IR at vegetative stage with FW and tasseling stage with SW; T4:3 IR at vegetative, tasseling and grain development stages with FW; T5: 3 IR at vegetative stage with FW and tasseling and grain development stages with SW; T6: 3 IR at vegetative and tasseling with FW and grain development stages with SW. Results showed that the conjunctive use of fresh water (0.5 ≤ salinity ≤ 1.2 dS/m) at early growth stages and saline water (1.5 ≤ salinity ≤ 5 dS/m) at later growth stages had insignificant difference compared to the treatment of fresh water irrigation during crop growing season at the both locations of Dacope and Amtali. The more changes in soil water occurred at top layer of the soil (0-15 cm) than lower depth of soil profiles at Amtali. On average, the soil water contents ranged was observed from 22 to 32% among the treatments from the month of January to March 2017 and lower moisture was obtained in February 2017. On average, the soil salinity (ECe) ranged from 9.3 to 13.9 dS/m during the crop growing season from January to March 2017. The highest changes in soil salinity occurred at mid (February 2017) of the crop growing season of maize compared to the beginning and later growth stages of maize in 60 cm soil profiles. On average, the osmotic potential ranged among the treatments was -333 kPa (T2) to -503 kPa (T5) from January to March 2017. The changes in soil pH occurred averagely 6.9 to 7.2 in the soil profiles 60 cm with 15 cm increments during the growing season from January to March 2017. Results showed that the lowest and highest values of maize yield were 6.6 t/ha using FW and SW irrigation in T3 and 7.7 t/ha  using FW irrigation in T4 in at Dacope and 6.5 t/ha using FW and SW irrigation in T3 and 7.6 t/ha (T6) using FW and SW irrigation in T3. No significant difference in yield was observed among the treatments in both locations. The method of fresh water (EC≤0.5 dS/m) and saline water (EC≥1.5 dS/m) irrigation to maize was observed similar trend of maize grain yield at Dacope and Amtali. Seasonal crop water use of maize ranged was estimated from 203 mm (T3) to 273 mm (T6) with an average of 244 mm at Dacope and from 241 mm (T1) to 300 mm (T4 and T6) with an average of 274 mm. Water productivity of maize under different irrigation treatments ranged was found from 2.7 (T5) to 3.3 kg/m3 (T1) with an average of 2.9 kg/m3 at Dacope and from 2.3 (T5) to 2.8 kg/m3 (T1) with an average of 2.8 kg/m3. WP had no significant difference between the treatment with FW at earlier growth stages and SW irrigation at later growth stages of maize crop in both locations. SWC was found lower in T1, T2 and T3 than others treatments and the trend of soil water content decreased from sowing to harvest in 45 cm soil depth. The highest soil salinity was found in T3 at around 8.3 dS/m at end of the crop growing season in the top 15 cm soil profile due to evaporation from soil surface and accumulated salt in the upper soil layer, and the consequence use of alternative medium saline water (1.5 to 3 dS/m) irrigation from canal to crop. The osmotic potential was found higher in T2 and T3 than other treatments which was slightly effected on plant growth and yield at later growth stages of maize because of insufficient soil moisture as well as lack of irrigation water in the project sites during 2018. Total grain yield was found higher in T4 and T5 compared to other technique of T1, T2, T3 and T6 at both locations 2017-2018. Farmers are being encouraged to represent the conjunctive use of fresh water (FW) and saline water (SW) irrigation for the future of agriculture in the coastal saline prone areas of Bangladesh. Therefore, the conjunctive use of fresh and saline water irrigation experiments for maize were performed over two years of 2016-2017 and 2017-2018 at the farmers' field of the village of Pankhali and Khatail at Dacope, Khulna and Sikandorkhali at Amtali, Barguna. The objectives of this study were (i) to evaluate the effect of soil moisture, soil salinity (ECe), osmotic pressure, pH and plant biomass at different growth stages, (ii) to assess the effect of fresh and saline water irrigation on the crop performances, water use and water productivity and (iii) to find out the scope of saline and fresh water irrigation for maize crop cultivation. The experiments were carried out in two farmer’s field at Pankhali and three farmers’ field with six irrigation treatments and replicated thrice. The treatments were: (i) T1:2 irrigations (IR) at vegetative stage and grain development stages with FW;  T2:2 IR at vegetative stage with FW and grain development stage with SW; T3: 2 IR at vegetative stage with FW and tasseling stage with SW; T4:3 IR at vegetative, tasseling and grain development stages with FW; T5: 3 IR at vegetative stage with FW and tasseling and grain development stages with SW; T6: 3 IR at vegetative and tasseling with FW and grain development stages with SW. Results showed that the conjunctive use of fresh water (0.5 ≤ salinity ≤ 1.2 dS/m) at early growth stages and saline water (1.5 ≤ salinity ≤ 5 dS/m) at later growth stages had insignificant difference compared to the treatment of fresh water irrigation during crop growing season at the both locations of Dacope and Amtali. The more changes in soil water occurred at top layer of the soil (0-15 cm) than lower depth of soil profiles at Amtali. On average, the soil water contents ranged was observed from 22 to 32% among the treatments from the month of January to March 2017 and lower moisture was obtained in February 2017. On average, the soil salinity (ECe) ranged from 9.3 to 13.9 dS/m during the crop growing season from January to March 2017. The highest changes in soil salinity occurred at mid (February 2017) of the crop growing season of maize compared to the beginning and later growth stages of maize in 60 cm soil profiles. On average, the osmotic potential ranged among the treatments was -333 kPa (T2) to -503 kPa (T5) from January to March 2017. The changes in soil pH occurred averagely 6.9 to 7.2 in the soil profiles 60 cm with 15 cm increments during the growing season from January to March 2017. Results showed that the lowest and highest values of maize yield were 6.6 t/ha using FW and SW irrigation in T3 and 7.7 t/ha  using FW irrigation in T4 in at Dacope and 6.5 t/ha using FW and SW irrigation in T3 and 7.6 t/ha (T6) using FW and SW irrigation in T3. No significant difference in yield was observed among the treatments in both locations. The method of fresh water (EC≤0.5 dS/m) and saline water (EC≥1.5 dS/m) irrigation to maize was observed similar trend of maize grain yield at Dacope and Amtali. Seasonal crop water use of maize ranged was estimated from 203 mm (T3) to 273 mm (T6) with an average of 244 mm at Dacope and from 241 mm (T1) to 300 mm (T4 and T6) with an average of 274 mm. Water productivity of maize under different irrigation treatments ranged was found from 2.7 (T5) to 3.3 kg/m3 (T1) with an average of 2.9 kg/m3 at Dacope and from 2.3 (T5) to 2.8 kg/m3 (T1) with an average of 2.8 kg/m3. WP had no significant difference between the treatment with FW at earlier growth stages and SW irrigation at later growth stages of maize crop in both locations. SWC was found lower in T1, T2 and T3 than others treatments and the trend of soil water content decreased from sowing to harvest in 45 cm soil depth. The highest soil salinity was found in T3 at around 8.3 dS/m at end of the crop growing season in the top 15 cm soil profile due to evaporation from soil surface and accumulated salt in the upper soil layer, and the consequence use of alternative medium saline water (1.5 to 3 dS/m) irrigation from canal to crop. The osmotic potential was found higher in T2 and T3 than other treatments which was slightly effected on plant growth and yield at later growth stages of maize because of insufficient soil moisture as well as lack of irrigation water in the project sites during 2018. Total grain yield was found higher in T4 and T5 compared to other technique of T1, T2, T3 and T6 at both locations 2017-2018. On average, the treatment T5 produced highest yield by 6.6 t/ha at Dacope and 6.3 t/ha at Amtali during 2018 when irrigation water applied with the technique of conjunctive use of fresh water at early growth stages and saline water at  later growth stages of maize. In 2018, SCWU was found averagely 201 mm at Dacope and 188 mm at Amtali. Water productivity of maize was found averagely 2.9 kg/m3 at Dacope and 3.1kg/m3 at Amtali. The conjunctive use of fresh water (pond/controlled canal water: 1.2 ≤ EC ≥ 0.5 dS/m) at early and medium saline water (canal water: EC ≥ 1.2 dS/m) at later growth stages of maize could be an effective irrigation technique to cultivate the maize at salt affected areas of coastal region in Bangladesh. 

  Fresh water, Saline water, Irrigation, Crop performances, Soil salinity, Crop, Saline, Water irrigation, Irrigation
  The village of Pankhali and Khatail at Dacope, Khulna and Sikandorkhali at Amtali, Barguna, Bangladesh
  00-00-2014
  00-00-2018
  Crop-Soil-Water Management
  Water management, Water salinity, Maize, Water quality

Objectives

  • To assess the effect of fresh and saline water irrigation on the crop performances
  • To evaluate the effect of soil salinity at different growth stages of crop
  • To find out the scope of saline and fresh water irrigation

The experiments were conducted during 2016-2017 and 2017-2018 at the farmers' fields of the village of Pankhali and Khatail at Dacope, Khulna and Sikandorkhali at Amtali, Barguna under the ACIAR-KGF project which is situated in the coastal regions of Bangladesh. The experiments were carried out at two farmer’s field at Pankhali and three farmers’ field with six irrigation treatments and replicated thrice. The plot size was (30 m2) which depended on existing farmers’ plot.

Experimental design and treatments:

The field experiment was laid out in randomized complete block design (RCBD) with six treatments replicated thrice. The treatments consisted of two and three irrigation levels were:

T1=  2 irrigations (IR) at vegetative stage and grain development stages with FW

T2 = 2 IR at vegetative stage with FW and grain development stage with SW

T3 = 2 IR at vegetative stage with FW and tasseling stage with SW

T4 = 3 IR at vegetative, tasseling and grain development stages with FW 

T5 = 3 IR at vegetative stage with FW and tasseling and grain development stages with SW

T6 = 3 IR at vegetative and tasseling with FW and grain development stages with SW

 

Soil physical and chemical properties:

Before crop sowing, soil samples were randomly collected from the desired depth (0-60 cm) of the experimental plots to determine the soil physical and chemical properties at the farmers' field of the village of Pankhali at Dacope, Khulna and Sikandorkhali at Amtali, Barguna under the ACIAR-KGF project sites. The physical properties of field capacity (%), percentage of clay and silt and soil texture were determined from the Soil Science Laboratory, BARI, Gazipur. The percentage of organic matter (OM), pH, total nitrogen (N), phosphorous (P), potassium (K), sulpher (S), zinc (Zn) and Boron (B) were also determined in the Soil Science Laboratory, BARI, Gazipur. All chemical properties were found greater than critical values. The bulk density and initial gravimetric soil water content and soil salinity were measured in both locations.

Crop management:

Standard crop management practices were followed. Recommended fertilizer dose and applied in the form of urea, triple supper phosphate, muriate of potash, gypsum, zinc sulfate and borax, respectively (Fertilizer Recommendation Guide, 2012) and application methods were applied. In this study, ZT is considered as one of the many types of CT for row crops. Mixed fertilizers were placed into the soil uniformly and soil packed to minimize fertilizers tie up with manually. Sub-surface placement of band fertilizer was placed. Half of the nitrogen and potassium and all phosphorous, sulphur, zinc and boron were applied as basal doses below the soil surface as horizontal and vertical separation of seed during planting. Remaining nitrogen and potassium were applied as earthing up operation followed by irrigation. Adequate plant protection measures were taken at vegetative stages. 

Application of irrigation water and water use:

Irrigation scheduled was followed according to BARI IWM recommendations. Irrigation frequency was considered at every certain interval depending on the different growth stages (initial stage, vegetative stage, flowering and grain development stages (Sarker et al, 2016) from plant establish to before final harvest. Irrigation water was applied based on the pan evaporation method at Dacope at different crop growth stages.  A class A pan evaporation was placed near to the experiment was used to estimate irrigation water requirement (I, mm) for full irrigation using the following equation.

p  Kp A.  Where, I is the amount of irrigation water amount (litre), A is the area of the plot (m2), Ep is the cumulative pan evaporation (mm) and Kp is the pan coefficient and was considered 0.7 (Michael, 1978). 

Yield and water productivity: 

The yield contributing characters and seed yield of maize were recorded from the plants during the experimental period. Five plants were randomly chosen to measure the seed yield components from each treatment. Economical grain yield (t/ha) were measured from the plants harvested from the selected two rows of each plot. Maize grain yield was manually harvested. Water productivity (WP) was calculated as the ratio of seed yield and total seasonal water use which was expressed by the following equation: WP = (GY x100) / (SCWU)

Where, WP is the water productivity (kg/m3), GY is the seed yield of maize (t/ha) and SCWU is the amount of seasonal crop water use (mm).

Statistical analysis:

Data on yield attributes, crop yield and water productivity were statistically analyzed to test the effects of irrigation levels and methods using R software version 3.5.0. All the treatment means were analyzed and compared for any significant differences using R-statistical models at 5% (P≤0.05) probability level of significant.

  Annual Research Report 2017-2018, Irrigation and Water Management Division, Bangladesh Agricultural Research Institute (BARI), Gazipur
  
Funding Source:
1.   Budget:  
  

Based on two years (2017 and 2018) study in the salt affected coastal areas of Bangladesh, the technique of conjunctive use of fresh water (EC ≤ 1.2 dS/m) at early crop growth stages and saline water (EC ≥1.2  and EC ≤ 5 dS/m) at later growth stages of maize crop in coastal areas of Bangladesh could be an alternative irrigation scheduled and method for increasing yield and water productivity with a little reduction in crop yield compared to the no crops (fallow lands during rabi season) in the salt affected coastal areas of Bangladesh. However, further studies are needed to expand of maize crop in salt prone areas of Bangladesh where fresh water (non-saline) is not available for rabi crops cultivation.

  Report/Proceedings
  


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