Agro-meteorological Indices to Predict Plant Stages and Yield of Wheat for Foot Hills of Western Himalayas

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International Journal of Agriculture and Food Science Technology. ISSN 49-3050, Volume 4, Number 9 (013), pp. 909-914 Research India Publications http://www.ripublication.com/ ijafst.htm Agro-meteorological Indices to Predict Plant Stages and Yield of Wheat for Foot Hills of Western Himalayas R.K. Pal 1, M.N.N. Rao and NS. Murty 1 1 Department of Agrometeorology, G B Pant Uni. of Agri. & Tech., Pantnagar-63145, Uttarakhand, INDIA. Department of Meteorology and Oceanography, Andhra Uni., Visakhapatnam-530003, Andhra Pradesh, INDIA. Abstract In this study, agro-meteorological indices have been calculated and used for prediction of plant stages and yield of wheat under different sowing environments with various phenophases for foot hills of Western Himalayas. To reckon the above necessities, field experiments were carried out during Rabi season of 007-08 and 008-09 at the Norman E. Borlaug Crop Research Centre of G. B. Pant University of Agriculture & Technology, Pantnagar (9 N, 79.3 E and 43.8 m above msl). The study revealed that the Higher PTU and HTU were accounted in case of variety PBW-343 followed by WH-54 during all the phenophases of wheat for both the years. Wheat crop sown on 0 th November (normal) required less photothermal unit as well as heliothermal unit, while, 09 th January (late) sowing accounted higher values of PTU and HTU during crop growth period. Timely sown wheat crop (0 th November) produced highest yield, while, with every 5 days delay in sowings reduction in yield was accounted by 13 to 6.1 percent in the year 007-08, whereas, 14.6 to 9.3 percent in 008-09. Keywords: Growing degree days; phenothermal unit; heliothermal unit, wheat genotypes; sowing dates. 1. Introduction Crop physiological process dependent on integrated atmospheric parameters (Ko et al., 010), in which temperature is an important weather parameter that affects plant growth, development and yield. Winter crops are vulnerable to high temperature during reproductive stages and differential response of temperature change (rise) to various crops has been noticed under different production environments (Kalra, 008).

910 R.K. Pal et al The productivity of wheat is highly variable and mainly affected by rainfall, temperature and solar radiation. Crop is exposed to a variety of weather conditions during its different phenophases of growth, resulting in large variations in growth rate and yield. For quantifying the thermal relation of crops, thermal units approach is widely used (Ramteke et al., 1996) and has been further modified to include photothermal units and heliothermal units (Rao et al., 1999). The photothermal unit concept provides a reliable index for the progress of the crop that can be used to predict the yield of any crop. Therefore present investigation was undertaken to study the thermal effect on growth and yield of wheat under different sowing environments. Cool weather during vegetative period and warm weather during maturity are ideal requirements for wheat. Influence of different time of sowing as well as temperature on phenology and yield of crop plants can be studied under field conditions through the accumulated heat units system (Shanker et al 1996). The aim of the present study was to predict plant stages and yield of wheat using agrometeorological indices in foot hills of western Himalayas.. Materials and Methods To perceive the thermal impact on different phenophases and productivity of wheat, field experiments were carried out during Rabi season of 007-08 and 008-09 at the Norman E. Borlaug Crop Research Centre (CRC) of G. B. Pant University of Agriculture & Technology, Pantnagar (9 N latitude, 79.3 E longitude and at an altitude of 43.8 m above mean sea level). The experiments were taken in split-plot design (SPD) in alliance of 6 replications with two genotypes viz. PBW-343 and WH- 54 as influenced by three sowing dates i.e. 0 November, 15 December and 09 January along. Soil information of the experimental site used for the present study has been shown in Pal et al. (01). The area lies in the Tarai belt located in the foot hills of Himalayas and falls under sub-humid subtropical climate with an annual rainfall about 1400 mm, out of which 80 percent is received during mid June to September during SW monsoon. The number of days to attain various phenophases was determined from randomly selected five plants in all the plots visually by the number of days taken from the sowing date to attain respective phenophases upto maturity. Maximum and minimum temperatures used for study were taken from meteorological observatory of the University that is 0 m away from the experimental site. The growing degree days (GDD) and heliothermal unit (HTU) was calculated according to the formula of Rajput (1980) and photothermal unit was calculated by using the formula of Major et al. (1975) for different phenophases of wheat [viz. emergence (I), crown root initiation (II), tillering (III), jointing (IV), 50% flowering (V), milking (VI) and physiological maturity (VII)].

Agro-meteorological Indices to Predict Plant Stages and Yield of Wheat for Foot 911 GDD PTU HTU n T max T min Tb i1 n i1 n i1 GDD Daylength GDD BSS GDD Growing Degree Days HTU Helio Thermal Units PTU Photo Thermal Units RTD Relative Temperature Disparity Tmax Maximum temperature ( C) Tmin Minimum temperature ( C) Tb Base temperature ( C) = 10 C BSS Bright sunshine hours 3. Results and Discussions 3.1 Photo-thermal unit (PTU) Photothermal unit from date of emergence to jointing (Ist to IVth stage) accounted higher with 0 th November than 15 th December sowing, while lowest PTU were observed with the crop sown on 09 th January during both the years (Khichar and Niwas, 007). Moreover, from 50% flowering to physiological maturity higher PTU were recorded with 09 th January sowing than the rest during both the years. With maturity of the crop highest PTU (17374.18 in 007-08 and 17837.5 in 008-09) was accounted with 09 th January sowing than 15 th December sown crop (1414.13 in 007-08 and 1587.68 in 008-09), while the lowest PTU were recorded in case of crop sown on 0 th November (13658.05 in 007-08 and 15106.76 in 008-09). Variety PBW-343 accounted non-significantly higher PTU than WH-54 at all the phenological stages of the crop during both the years. PTU increased as the sowings were delayed for all the varieties in both the years (Table 1). Treatmen ts Nov. 0 95 Table 1: Photo-thermal unit (PTU) required for various phenophases of wheat as affected by different treatments. Photo-thermal unit (PTU) for various phenophases of wheat 007-08 008-09 I II III IV V VI VII I II III IV V VI VII Dates of sowing 51 319 505 85 108 137 80 56 337 548 9584 1186 1519 4 5 3 9 1 7 3 9 1 7 3 187 50 381 855 1087 144 81 09 64 440 9539 19 159 Dec. 15 7 9 8 8 9 1 7 1 6 6 4 7 Jan. 09 73 167 190 375 1018 1364 17 83 10 40 458 1140 1457 1788 5 6 3 7 4 0 7 3 0 3 SEm± 40 1 44 89 60 104 9 34 17 1 39 85 181

91 R.K. Pal et al CD at 5% 15 84 81 173 348 35 406 11 134 68 48 154 331 706 5 Varieties PBW-343 79 199 5 44 8974 1178 1539 80 7 83 483 10 195 1640 8 5 8 9 5 7 3 7 9 0 3 9 WH-54 81 05 54 417 880 1141 1484 83 3 78 480 1013 186 166 4 1 1 6 1 9 3 1 1 5 0 9 0 SEm± 1 8 6 46 88 106 161 5 8 6 3 65 48 99 CD at 5% 73 97 90 160 304 367 556 85 98 88 111 5 165 341 3. Helio-thermal unit (HTU) Among the sowing dates, heliothermal unit mostly decreased from date of emergence to jointing (Khichar and Niwas, 007), while, increment in HTU was accredited from flowering to maturity of the crop, during both the years. Furthermore, with the delayed in sowing HTU increased for all the varieties during both the years. During the study period, among the sowing dates, maximum HTU was recorded at 09 th January sowing (1107.39 and 1519.30 in 007-08 and 008-09, respectively). Non-significant increase in HTU was observed with variety PBW-343 than WH-54 at all the phenological stages of the crop during both the years (Table ). Treatmen ts Nov. 0 81 Table : Helio-thermal unit (HTU) required for various phenophases of wheat as affected by different treatments. Helio-thermal unit (HTU) for various phenophases of wheat 007-08 008-09 I II III IV V VI VII I II III IV V VI VII Dates of sowing 165 187 98 473 607 791 54 186 47 39 550 736 9934 0 1 1 1 6 6 4 8 8 9 115 14 05 488 66 8353 37 83 116 193 56 774 1018 Dec. 15 46 8 3 9 4 8 0 1 7 4 1 3 5 Jan. 09 36 756 901 10 60 805 1093 49 97 110 66 767 980 7 5 5 8 4 3 5 SEm± 31 85 16 9 6 46 6 11 1 18 1 3 50 1 CD at 5% 1 33 64 11 43 179 44 43 81 74 45 9 194 65 1 156 6 Varieties PBW-343 54 3 117 9 140 0 39 7 56 8 69 977 46 9 1 8 160 63 6 69 8 833 WH-54 55 119 140 36 516 666 8865 47 11 156 6 63 87 4 4 1 4 8 0 1 4 7 9 SEm± 14 69 17 30 5 78 17 15 18 16 45 40 65 CD at 5% 48 4 60 103 180 70 440 51 61 54 77 154 139 6 1094 7 1084

Agro-meteorological Indices to Predict Plant Stages and Yield of Wheat for Foot 913 3.3 Yield response of wheat Timely sown wheat crop (0 th November) with an average seasonal air temperature of 16.3 O C produced highest yield of 4580.3 kg ha -1 in 007-08, while, it was 4080.3 kg ha -1 in 008-09 with an average seasonal air temperature of 17.9 O C (Pal et al., 01b) With every 5 days delay in sowings with an increase in average seasonal air temperature (17 to 18.6 O C) caused reduction in yield (Khichar and Niwas, 007) by 13 to 6.1 percent in the year 007-08, whereas, 14.6 to 9.3 percent in 008-09 (due to increase in average seasonal air temperature from 18.8 to 0.4 O C) (Fig. 1 and ). Genotype PBW-343 recorded highest grain yield followed by the genotype WH-54 in both the years (Table 3). Pal et al. (01) reported that the significantly highest straw & biological yield was also recorded with crop sown on 0 th November with the genotype PBW-343. Hundal (004) observed that a 0 C increase in temperature in wheat or rice resulted in 15-17 percent decrease in grain yield of both crops but beyond that the decrease was very high in wheat. 3.4 Prediction of a crop stage using agro-meteorological indices After germination of seed with sufficient moisture record the seeding date and coinciding degree day value by running the degree day accumulation using the base temperature of 5 C for the wheat crop. Watch for that corresponding crop stage to occur in the field until the difference between the beginning and the current accumulation value approaches the table 1 and values. Thereafter, validate the table 1 and values for study area by recording when the crop stage actually occurs in the field. With the time, doing this adjustment to the table values will increase the accurateness of the agro-meteorological indices. 4. Conclusion It is therefore, concluded that wheat crop sown on 0 th November (normal) need to be less photothermal unit as well as heliothermal unit, while, 09 th January (late) sowing required higher PTU and HTU during crop growth period. In the year 007-08, 0 th November sowing recorded maximum grain yield to the extent of 13.0 % higher over 15 th December and 6.1 % over 09 th January sowing indicating optimum thermal regime. Grain yield accounted more in 008-09 with the crop sown on 0 th November sowing which was 14.6 % and 9.3 % higher than 15 th December and 09 th January sowings, respectively. Overall, the performance of genotype PBW-343 was accredited to better followed by the genotype WH-54 in both the years. Temperature is one of the most important elements of the climate which determines the potential productivity level particularly for winter crops. The response of wheat crop to different thermal regimes, suggests that under the foot hills of Western Himalayas, the wheat crop sown on 0 th November proved to be beneficial as the farmers can keep good harvest.

914 R.K. Pal et al References [1] D J Major, D R Johanson, J W Tanner and I C Anderson (1975), Effect of day length and temperature on soybean development, Crop Sci., 15: 174-179. [] Jonghan Ko, L Ahujab, B Kimballc, S Anapallib, L Mab, T R Greenb, A C Ruaned, G W Wallc, P Pinterc and D A Badere (010), Simulation of free air CO enriched wheat growth and interactions with water, nitrogen, and temperature, Agr. Forest Meteorol., 150: 1331-1346. [3] M L Khichar and R Niwas (007), Thermal effect on growth and yield of wheat under different sowing environments and planting systems, Ind. J. Agr. Res., 41(): 9-96. [4] N Kalra (008), Effect of increasing temperature on yield of some winter crops in north west India, Cur. Sci., 94 (1): 8-88. [5] R K Pal, N S Murty and M M N Rao (01), The response of wheat to temperatures as simulated with CERES-wheat model in Tarai region, J. Agrometeorol., 14 (): 163-166. [6] R P Rajput (1980), Response of Soybean crop to climatic and soil environments. Ph.D. Thesis, IARI, New Delhi, India. [7] S D Ramteke, M B Chetti and P M Salimath (1996), Heat unit requirement of chickpea genotypes for various phenological stages during kharif and rabi seasons, Annals of Plant Physiology, 10 (): 176-181. [8] S S Hundal (004), Climatic changes and their impact on crop productivity vis-à-vis mitigation and adaptation strategies, In proc. of workshop Sustainable Agricultural Problems and Prospects. Punjab Agril. Uni., Ludhiana. pp 148-153. [9] U Shanker, K K Agrawal and V K Gupta (1996), Heat unit requirements of rainfed soybean, Ind. J. Agr. Sci., 66: 401-404. [10] V U M Rao, Diwan Singh and Raj Singh (1999), Heat use efficiency of winter crops in Haryana, J. Agrometeorol., 1(): 143-148.