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Journal of Stress Physiology & Biochemistry, Vol. 10 No. 3 2014, pp. 197-217 ISSN 1997-0838 Original Text Copyright © 2014 by Sawan
ORIGINAL ARTICLE
Nature Relation Between Climatic Variables and Cotton Production
Zakaria M. Sawan
Cotton Research Institute, Agricultural Research Center, Ministry of Agriculture & Land Reclamation, 9 Gamaa Street, 12619, Giza, Egypt
*E-Mail: zmsawan@hotmail.com
Received April 15, 2014
This study investigated the effect of climatic variables on flower and boll production and retention in cotton (Gossypium barbadense). Also, this study investigated the relationship between climatic factors and production of flowers and bolls obtained during the development periods of the flowering and boll stage, and to determine the most representative period corresponding to the overall crop pattern. Evaporation, sunshine duration, relative humidity, surface soil temperature at 1800 h, and maximum air temperature, are the important climatic factors that significantly affect flower and boll production. The least important variables were found to be surface soil temperature at 0600 h and minimum temperature. There was a negative correlation between flower and boll production and either evaporation or sunshine duration, while that correlation with minimum relative humidity was positive. Higher minimum relative humidity, short period of sunshine duration, and low temperatures enhanced flower and boll formation.
Key words: evaporation, relative humidity, sunshine duration, temperature
ORIGINAL ARTICLE
Nature Relation Between Climatic Variables and Cotton Production
Zakaria M. Sawan
Cotton Research Institute, Agricultural Research Center, Ministry of Agriculture & Land Reclamation, 9 Gamaa Street, 12619, Giza, Egypt
*E-Mail: zmsawan@hotmail.com
Received April 15, 2014
This study investigated the effect of climatic variables on flower and boll production and retention in cotton (Gossypium barbadense). Also, this study investigated the relationship between climatic factors and production of flowers and bolls obtained during the development periods of the flowering and boll stage, and to determine the most representative period corresponding to the overall crop pattern. Evaporation, sunshine duration, relative humidity, surface soil temperature at 1800 h, and maximum air temperature, are the important climatic factors that significantly affect flower and boll production. The least important variables were found to be surface soil temperature at 0600 h and minimum temperature. There was a negative correlation between flower and boll production and either evaporation or sunshine duration, while that correlation with minimum relative humidity was positive. Higher minimum relative humidity, short period of sunshine duration, and low temperatures enhanced flower and boll formation.
Key words: evaporation, relative humidity, sunshine duration, temperature
Abbreviations: ET, Evapotranspiration; ETmax, Maximum Evapotranspiration; PGR, plant growth regulator; TKW, thermal kinetic window
The balance between vegetative and reproductive development can be influenced by soil fertility, soil moisture, cloudy weather, spacing and perhaps other factors such as temperature and relative humidity (Guinn 1982). Weather, soil, cultivars, and cultural practices affect crop growth interactively, sometimes
resulting in plants responding in unexpected ways to their conditions.
Water is a primary factor controlling plant growth. Xiao et al. (2000) stated that, when water was applied at 0.85, 0.70, 0.55 or 0.40 ET (evapotranspiration) to cotton plants grown in pots, there was a close
relationship between plant development and water supply. The fruit-bearing branches, square and boll numbers and boll size were increased with increased water supply. Barbour and Farquhar (2000) reported on greenhouse pot trials where cotton cv. CS50 plants were grown at 43 or 76% relative humidity (RH) and sprayed daily with abscisic acid (ABA) or distilled water. Plants grown at lower RH had higher transpiration rates, lower leaf temperatures and lower stomatal conductance. Plant biomass was also reduced at the lower RH. Within each RH environment, increasing ABA concentration generally reduced stomatal conductance, evaporation rates, superficial leaf density and plant biomass, and increased leaf temperature and specific leaf area.
Temperature is also a primary factor controlling rates of plant growth and development. Burke et al. (1988) has defined the optimum temperature range for biochemical and metabolic activities of plants as the thermal kinetic window (TKW). Plant temperatures above or below the TKW result in stress that limits growth and yield. The TKW for cotton growth is 23.5 to 32°C, with an optimum temperature of 28°C. Biomass production is directly related to the amount of time that foliage temperature is within the TKW.
Reddy et al. (1995) in growth chamber
experiments found that Pima cotton cv. S-6 produced lower total biomass at 35.5°C than at 26.9° C and no bolls were produced at the higher temperature of 40°C. Schrader et al. (2004) stated that high temperatures that plants are likely to experience inhibit photosynthesis. Zhou et al. (2000) indicated that light duration is the key meteorological factor
influencing the wheat-cotton cropping pattern and position of the bolls, while temperature had an important function on upper (node 7 to 9) and top (node 10) bolls, especially for double cropping patterns with early maturing varieties.
In Texas, Guo et al. (1994) found that plant growth and yield of the cotton cv. DPL-50 (Upland cotton) were less in a humid area than in an arid area with low humidity. Under arid conditions, high vapor pressure deficit resulted in a high transpiration rates, low leaf water potential and lower leaf temperatures. Gipson and Joham (1968) mentioned that cool temperatures (< 20°C) at night slowed boll development. Fisher (1975) found that high temperatures can cause male sterility in cotton flowers, and could have caused increased boll shedding in the late fruiting season. Zhao (1981) indicated that temperature was the main climatic factor affecting cotton production and 20-30°C was the optimum temperature for cotton growth.
Hodges et al. (1993) found that the optimum temperature for cotton stem and leaf growth, seedling development, and fruiting was almost 30°C, with fruit retention decreasing rapidly as the time of exposure to 40°C increased. Reddy et al. (1998) found that when Upland cotton (G. hirsutum) cv. DPL-51 was grown in naturally lit plant growth chambers at 30/22°C day/night temperatures from sowing until flower bud production, and at 20/12, 25/17, 30/22, 35/27 and 40/32°C for 42 days after flower bud production, fruit retention was severely curtailed at the two higher temperatures compared with 30/22° C. Species/cultivars that retain fruits at high temperatures would be more productive both in the
present-day cotton production environments and even more in future warmer world.
The objectives of this investigation were to study: A- The effect of climatic factors (namely, evaporation, sunshine duration, relative humidity, soil temperature, and air temperature) on the overall flower and boll production in Egyptian cotton. It would be useful to minimize the deleterious effects of the factors through utilizing proper cultural practices which would limit and control their negative effects, and this will lead to an increase in cotton yield. B- Also, investigated the relationship between climatic factors and production of flowers and bolls obtained during the periods of the flowering and boll stage.
MATERIALS AND METHODS
Two uniform field trials were conducted at the experimental farm of the Agricultural Research Center, Ministry of Agriculture, Giza, Egypt (30oN, 31o: 28'E at an altitude of 19 m), using the cotton cultivar Giza 75 (Gossypium barbadense L.) in 2 successive seasons (I and II). The soil texture was a clay loam, with an alluvial substratum (pH = 8.07, 42.13% clay, 27.35% silt, 22.54% fine sand, 3.22% coarse sand, 2.94% calcium carbonate and 1.70% organic matter) (Sawan et al. 2010).
Total water consumed during each of two growing seasons supplied by surface irrigation was about 6,000-m3 h-1. The criteria used to determine amount of water applied to the crop depended on soil water status. Irrigation was applied when soil water content reached about 35% of field capacity (0-60 cm). In season I, the field was irrigated on 15 March (at planting), 8 April (first irrigation), 29 April, 17 May, 31
May, 14 June, 1 July, 16 July, and 12 August. In season II, the field was irrigated on 23 March (planting date), 20 April (first irrigation), 8 May, 22 May, 1 June, 18 June, 3 July, 20 July, 7 August and 28 August. Techniques normally used for growing cotton in Egypt were followed. Each experimental plot contained 13 to 15 ridges to facilitate proper surface irrigation. Ridge width was 60 cm and length was 4 m. Seeds were sown in hills 20 cm apart on one side of the ridge. Seedlings were thinned to 2 plants per hill 6 weeks after planting, resulting in a plant density of about 166,000 plants ha-1. Phosphorus fertilizer was applied at a rate of 54 kg P2O5 ha-1 as calcium super phosphate during land preparation. Potassium fertilizer was applied at a rate of 57 kg K2O ha-1 as potassium sulfate before the first irrigation (as a concentrated band close to the seed ridge). Nitrogen fertilizer was applied at a rate of 144 kg N ha-1 as ammonium nitrate in two equal doses: the first was applied after thinning just before the second irrigation and the second was applied before the third irrigation. Rates of phosphorus, potassium, and nitrogen fertilizer were the same in both seasons. These amounts were determined based on the use of soil tests.
After thinning, 261 and 358 plants were randomly selected (precaution of border effect was taken into consideration by discarding the cotton plants in the first and last two hills of each ridge) from 9 and 11 inner ridges of the plot in seasons I, and II respectively. Pest control management was carried out on an-as-needed basis, according to the local practices performed at the experimental.
Flowers on all selected plants were tagged in order to count and record the number of open flowers, and set bolls on a daily basis. The flowering season commenced on the date of the first flower appearance and continued until the end of flowering season (31 August). The period of whole September (30 days) until the 20th of October (harvest date) allowed a minimum of 50 days to develop mature bolls. In season I, the flowering period extended from 17 June to 31 August, whereas in season II, the flowering period was from 21 June to 31 August. Flowers produced after 31 August were not expected to form sound harvestable bolls, and therefore were not taken into account.
For statistical analysis, the following data of the dependent variables were collected: number of tagged flowers separately counted each day on all selected plants (Y1), number of retained bolls obtained from the total daily tagged flowers on all selected plants at harvest (Y2), and (Y3) percentage of boll retention ([number of retained bolls obtained from the total number of daily tagged flowers in all selected plants at harvest]/[daily number of tagged flowers on each day in all selected plants] x 100).
As a rule, observations were recorded when the number of flowers on a given day was at least 5 flowers found in a population of 100 plants and this continued for at least five consecutive days. This rule omitted eight observations in the first season and ten observations in the second season. The number of observations (n) was 68 (23 June through 29 August) and 62 (29 June through 29 August) for the two seasons, respectively.
The climatic factors (independent variables) considered were daily data of: maximum air temperature (°C, X1); minimum air temperature (°C, X2); maximum-minimum air temperature (diurnal temperature range) (°C, X3); evaporation (expressed as Piche evaporation) (mm day-1, X4); surface soil temperature, grass temperature or green cover temperature at 0600 h (°C, X5) and 1800 h (°C, X6); sunshine duration (h day-1, X7); maximum relative humidity (maxRH) (%, Xe), minimum relative humidity (minRH) (%, X9) and wind speed (m s-1, X10) in season II only. The source of the climatic data was the Agricultural Meteorological Station of the Agricultural Research Station, Agricultural Research Center, Giza, Egypt. No rainfall occurred during the two growing seasons.
Daily records of the climatic factors (independent variables) were taken for each day during production stage in any season. Range and mean values of the climatic parameters recorded during the production stage for both seasons and overall data are listed in Table 1. Daily number of flowers and number of bolls per plant which survived till maturity (dependent variables) during the production stage in the two seasons are graphically illustrated in Figures 1 and 2.
RESULTS AND DISCUSSION A. Response of flower and boll development to climatic factors on the anthesis day
Daily number of flowers and number of bolls per plant which survived to maturity (dependent variables) during the production stage of the two seasons (68 days and 62 days in the first and the second seasons, respectively) are graphically illustrated in Figures 1
and 2. The flower- and boll-curves reached their peaks during the middle two weeks of August, and then descended steadily till the end of the season. Specific differences in the shape of these curves in the two seasons may be due to the growth-reactions of environment, where climatic factors (Table 1) represent an important part of the environmental effects (Miller et al. 1996).
A.1. Correlation estimates:
Results of correlation coefficients [correlation and regression analyses were computed, according to Draper and Smith (1966) by means of the computer program SAS package (1985). between the initial group of independent variables and each of flower and boll production in the first and second seasons and the combined data of the two seasons are shown in Table 2.
The correlation values indicate that evaporation is the most important climatic factor affecting flower and boll production as it showed the highest correlation value. This factor had a significant negative relationship with flower and boll production. Sunshine duration showed a significant negative relation with fruit production except for boll production in the first season, which was not significant. Maximum air temperature, temperature magnitude, and surface soil temperature at 1800 h, were also negatively correlated with flower and boll production in the second season and the combined data of the two seasons. Minimum humidity in the second season, the combined data of the two seasons, and maximum humidity in the first season were positively and highly correlated with flower and boll production. Minimum
air temperature and soil surface temperature at 0600 h showed low and insignificant correlation to flower and boll production.
The negative relationship between evaporation with flower and boll production, means that high evaporation rate significantly reduces cotton flower and boll production. This may be due to greater plant water deficits when evaporation increases. Also, the negative relation between each of maximum temperature, temperature magnitude, surface soil temperature at 1800 h, or sunshine duration, with flower and boll production revealed that the increase in the values of these factors had a detrimental effect upon fruit production in Egyptian cotton. On the other hand, there was a positive correlation between each of maximum or minimum humidity with flower and boll production (Sawan et al. 2002).
Results obtained from the production stage of each season individually, and the combined data of the two seasons, indicate that relationships of some climatic variables with the dependent variables varied markedly from one season to another. This may be due to the differences between climatic factors in the two seasons as illustrated by the ranges and means shown in Table 1. For example, maximum temperature, minimum humidity and soil surface temperature at 1800 h did not show significant relations in the first season, while that trend differed in the second season. The effect of maximum humidity varied markedly from the first season to the second one. Where it was significantly correlated with the dependent variables in the first season, while the inverse pattern was true in the second season. This
diverse effect may be due to the differences in the mean values of this factor in the two seasons; where it was, on average, about 86% in the first season, and about 72% on average in the second season, as shown in Table 1.
Boll retention ratio [(The number of retained bolls obtained from the total number of each daily tagged flowers in all selected plants at harvest/Total number of daily tagged flowers of all selected plants) x 100] curves for both of the two seasons are shown in Figures 3 and 4.. Also, these curves describe why the shapes and patterns associated with the flower and boll curves for I and II seasons were different. It seems reasonable that the climatic data that were collected in these two experiments (I and II seasons) could provide adequate information for describing how these two seasons differed and how the crop responded accordingly.
These results indicate that evaporation is the most effective and consistent climatic factor affecting boll production. As the sign of the relationship was negative, this means that an increase in evaporation would cause a significant reduction in boll number. Thus, applying specific treatments such as an additional irrigation, and use of plant growth regulators, would decrease the deleterious effect of evaporation after boll formation and hence contribute to an increase in cotton boll production and retention, and the consequence is an increase in cotton yield (Sawan et al. 2002). In this connection, Moseley et al.
(1994) stated that methanol has been reported to increase water use efficiency, growth and development of C3 plants in arid conditions, under
intense sunlight. In field trials cotton cv. DPL-50 (Gossypium hirsutum), was sprayed with a nutrient solution (1.33 lb N + 0.27 lb Fe + 0.27 lb Zn acre-1) or 30% methanol solution at a rate of 20 gallons acre-1, or sprayed with both the nutrient solution and methanol under two soil moisture regimes (irrigated and dry land). The foliar spray treatments were applied 6 times during the growing season beginning at first bloom. They found that irrigation (a total of 4.5 inches applied in July) increased lint yield across foliar spray treatments by 18%. Zhao and Oosterhuis (1997) reported that in a growth chamber when cotton (Gossypium hirsutum cv. Stoneville 506) plants were treated with the plant growth regulator PGR-IV (gibberellic acid, IBA and a proprietary fermentation broth) under water deficit stress and found significantly higher dry weights of roots and floral buds than the untreated water-stressed plants. They concluded that PGR-IV can partially alleviate the detrimental effects of water stress on photosynthesis and dry matter accumulation and improves the growth and nutrient absorption of growth chamber-grown cotton plants. Meek et al. (1999) in a field experiment in Arkansas found that application of 3 or 6 kg glycine betaine (PGR) ha-1, to cotton plants had the potential for increasing yield in cotton exposed to mild water stress.
A.2. Multiple linear regression equation:
By means of the multiple linear regression analysis, fitting predictive equations (having good fit) were computed for flower and boll production per plant using selected significant factors from the nine climatic variables studied in this investigation. Wind
speed evaluated during the second season had no influence on the dependent variables. The equations obtained for each of the two dependent variables, i.e. number of flowers (Y1) and bolls per plant (Y2) in each season and for combined data from the two seasons (Table 2) (Sawan et al. 2002) are as follows:
First Season: (n = 68)
Y1 = 21.691 - 1.968 X4 - 0.241 X7 + 0.216 X8, R = 0.608** and R2 = 0.3697,
While R2 for all studied variables was 0.4022.
Y2 = 15.434 - 1.633 X4 + 0.159 X8, R = 0.589** and R2 = 0.3469 and R2 for all studied variables was 0.3843.
Second Season: (n = 62)
Y1 = 77.436 - 0.163 X1 - 2.861 X4 - 1.178 X7 + 0.269 X9, R = 0.644**, R2 = 0.4147.
Y2 = 66.281 - 0.227X1 - 3.315X4 - 2.897X7 + 0.196X9, R = 0.629**, R2 = 0.3956.
In addition, R2 for all studied variables was 0.4503 and 0.4287 for Y1 and Y2 equations respectively.
Combined data for the two seasons: (n = 130)
Y1 = 68.143 - 0.827 X4 - 1.190 X6 - 2.718 X7 + 0.512 X9, R = 0.613**, R2 = 0.3758
Y2 = 52.785 - 0.997 X4 - 0.836 X6 - 1.675 X7 +
0.426 X9, R = 0.569**, R2 = 0.3552
While R2 for all studied variables was 0.4073 for
Y1 and 0.3790 for Y2.
Three climatic factors, i.e. minimum air temperature, surface soil temperature at 0600 h, and wind speed were not included in the equations since they had very little effect on production of cotton
flowers and bolls. The sign of the partial regression
coefficient for an independent variable (climatic
factor) indicates its effect on the production value of
the dependent variable (flowers or bolls). This means
that high rates of humidity and/or low values of
evaporation will increase fruit production.
A.3. Contribution of selected climatic factors to variations in the dependent variable:
Relative contributions (RC %) for each of the selected climatic factors to variation in flower and boll production is summarized in Table 3. Results in this table indicate that evaporation was the most important climatic factor affecting flower and boll production in Egyptian cotton. Sunshine duration is the second climatic factor of importance. Relative humidity and temperature at 1800 h were factors of lower contribution than evaporation and sunshine duration/day. Maximum temperature made a contribution less than the other affecting factors.
The highest contribution of evaporation to the variation in both flower and boll production (Sawan et al. 2002) can, however, be explained in the light of results found by Ward and Bunce (1986) in sunflower (Helianthus annuus). They stated that decreases of humidity at both leaf surfaces reduced photosynthetic rate of the whole leaf for plants grown under a moderate temperature and medium light level. Kaur and Singh (1992) found in cotton that flower number was decreased by water stress, particularly when applied at flowering. Seed cotton yield was about halved by water stress at flowering, slightly decreased by stress at boll formation, and not significantly affected by stress in the vegetative stage (6-7 weeks
after sowing). Orgaz et al. (1992) in field experiments at Cordoba, SW Spain, grew cotton cultivars Acala SJ-C1, GC-510, Coker-310 and Jean cultivar at evapotranspiration (ET) levels ranging from 40 to 100% of maximum ET (ETmax) which were generated with sprinkler line irrigation. The water production function of Jean cultivar was linear; seed yield was 5.30 t ha-1 at ETmax (820 mm). In contrast, the production function of the three other cultivars was linear up to 85% of ETmax, but leveled off as ET approached ETmax (830 mm) because a fraction of the set bolls did not open by harvest at high ET levels. These authors concluded that it is possible to define an optimum ET deficit for cotton based on cultivar earliness, growing-season length, and availability of irrigation water.
The negative relationship between sunshine duration and cotton production (Sawan et al. 2002) may be due to the fact that the species of Gossypium used is known to be a short day plant (Hearn and Constable 1984), so, an increase of sunshine duration above that needed for cotton plant growth will decrease flower and boll production. Oosterhuis (1997) studied the reasons for low and variable cotton yields in Arkansas, with unusually high insect pressures and the development of the boll load during an exceptionally hot and dry August. Solutions to the problems are suggested i.e. selection of tolerant cultivars, effective and timely insect and weed control, adequate irrigation regime, use of proper crop monitoring techniques and application of plant growth regulators.
B. Effect of climatic factors during the development periods of flowering and boll formation on the production of cotton
Daily number of flowers and number of bolls per plant that survived to maturity (dependent variables) during the production stage of the two growing seasons are graphically illustrated in Figures 5 and 6. Observations used in the statistical analysis were obtained during the flowering and boll stage (60 days for each season), which represent the entire production stage. The entire production stage was divided into four equivalent quarter's periods (15 days each) and used for correlation and regression analyses.
Independent variables, their range and mean values for the two seasons and during the periods of flower and boll production are listed in Table 4. Both flower number and boll production show the higher value in the third and fourth quarters of production stage, accounting for about 70% of total production during the first season and about 80% of the total in the second season.
Linear correlation between the climatic factors and the studied characteristics, i.e. flower, boll production and boll retention ratio, were calculated based on quarters of the production stage for each season. Significant relationships (< 0.15) are shown in Tables
5 and 6 (Sawan et al. 1999). Examining these tables, it is clear that the fourth quarter of production stage consistently exhibited the highest R2 values regardless of the second quarter for boll retention ratio; however, less data pairs were used (n = 30 for combined data of the fourth quarter “n = 15 for each
quarter of each season”) to calculate the relations.
Results obtained from the four quarters of the production period for each season separately and for the combined data of the two seasons, indicated that relationships varied markedly from one season to another. This may be due to the differences between the climatic factors in the two seasons; as illustrated by its ranges and means shown in Table 4. For example, maximum temperature and surface soil temperature at 1800 h did not show significant effects in the first season, while this trend differed in the second season.
Multiple linear regression equations obtained from data of the fourth quarter, for:
1. Flower production,
Y = 160.0 + 11.28X1 - 4.45X3 - 2.93X4 - 5.05X5 -11.3X6 - 0.962X8 + 2.36X9
And R2= 0.672**
2. Boll production,
Y = 125.4 + 13.74X1 - 6.76X3 - 4.34X4 - 6.59X5 -10.3X6 - 1.25X8 + 2.16X9
With an R2 = 0.747**
3. Boll retention ratio,
Y = 81.93 - 0.272X3 - 2.98X4 + 3.80X7 - 0.210X8 -0.153X9
And its R2 = 0.615**
The equation obtained from data of the second quarter of production stage for boll retention ratio,
Y= 92.81 - 0.107X3 - 0.453X4 + o.298X7 - 0.194X8 + 0.239X9
And R2 = 0.737**
R2 values for these equations ranged from 0.615
to 0.747. It could be concluded that these equations may predict flower and boll production and boll retention ratio from the fourth quarter period within about 62 to 75% of its actual means. Therefore, these equations seem to have practical value. Comparing Tables 6 and 7 (Sawan et al. 1999), it can be seen that differences in R2 between the fourth quarter and the entire production period of the two seasons for each of flower, boll production, and boll retention ratio were large (0.266, 0.325, and 0.279 respectively). These differences are sufficiently large to make a wide gap under a typical field sampling situation. This could be due to the high percentage of flower and boll production for the fourth quarter.
Equations obtained from data of the fourth quarter explained more variations of flower, boll production and boll retention ratio. Evaporation, humidity and temperature are the principal climatic factors that govern cotton flower and boll production during the fourth quarter; since they were most strongly
correlated with the dependent variables studied
(Table 6).
Evaporation, that seems to be the most important climatic factor, had negative significant relationship which means that high evaporation ratio reduces significantly flower and boll production. Maximum temperature, temperature-differentiates and
maximum humidity also showed negative significant link with fruiting production (Sawan et al. 1999), which indicates that these climatic variables have
determinable effect upon Egyptian cotton fruiting production. Minimum humidity was positively high correlated in most quarter periods for flower, boll
production and boll retention ratio (Sawan et al. 1999). This means that an increase of this factor will increase both flower and boll production. Maximum temperature is sometime positively and sometime negatively linked to boll production (Table 6) (Sawan et al. 1999). These erratic correlations may be due to the variations in the values of this factor between the quarters of the production stages, as shown from its range and mean values (Table 4) (Sawan et al. 1999).
Burke et al. (1990) pointed out that the usefulness of the 27.5°C midpoint temperature of the TKW of cotton as a baseline temperature for a thermal stress index (TSI) was investigated in field trials on cotton cv. Paymaster 104. This biochemical baseline and measurements of foliage temperature were used to compare the TSI response with the cotton field performance. Foliage temperature was measured with hand-held 4°C field of view IR thermometer while plant biomass was measured by destructive harvesting. The biochemical based TSI and the physically based crop water stress index were highly correlated (r2 = 0.92) for cotton across a range of environmental conditions. Reddy et al. (1995) in controlled environmental chambers pima cotton cv. S-
6 produced less total biomass at 35.5°C than at 26.9°C and no bolls were produced at the higher temperature 40°C. This confirms the results of this study as maximum temperature showed negative significant relationship with production variables in the fourth quarter period of the production stage. Zhen
(1995) found that the most important factors decreasing cotton yields in Huangchuan County,
Henan, were low temperatures in spring, high temperatures and pressure during summer and the sudden fall in temperature at the beginning of autumn. Measures to increase yields included the use of the more suitable high-oil cotton cultivars, which mature early, and choosing sowing dates and spacing so that the best use was made of the light and temperature resources available.
It may appear that the grower would have no control over boll shedding induced by high temperature, but this is not necessarily the case. If he can irrigate, he can exert some control over temperature since transpiring plants have the ability to cool themselves by evaporation. The leaf and canopy temperatures of drought-stressed plants can exceed those of plants with adequate quantity of water by several degrees when air humidity is low (Ehrler 1973). The grower can partially overcome the adverse effects of high temperature on net photosynthesis by spacing plants to adequately expose the leaves. Irrigation may also increase photosynthesis by preventing stomata closure during the day. Adequate fertilization is necessary for maximum rates of photosynthesis. Finally, cultivars appear to differ in their heat tolerance (Fisher 1975). Therefore, the grower can minimize boll abscission where high temperatures occur by selecting a heat-tolerant cultivar, planting date management, applying an adequate fertilizer, planting or thinning for optimal plant spacing, and irrigating as needed to prevent drought stress.
—•— Flowers — — Bolls
0 4 S 12 16 20 24 2S 32 36 40 44 4S 52 56 60 64 6S
Days after begining of flowering
Figure 1. Daily number of flowers and bolls during the production stage (68 days) in the first season (I) for the
Egyptian cotton cultivar Giza 75 (Gossypium barbadense L.) grown in uniform field trial at the
experimental farm of the Agricultural Research Centre, Giza (30oN, 3^:28'E), Egypt. The soil texture was a clay loam, with an alluvial substratum, (pH = 8.07). Total water consumptive use during the growing season supplied by surface irrigation was about 6000 m3ha-1. No rainfall occurred during the
growing season. The sampling size was 261 plants (Sawan et al. 2005).
Days after begining of flowering
Figure 2. Daily number of flowers and bolls during the production stage (62 days) in the second season (II) for the Egyptian cotton cultivar Giza 75 (Gossypium barbadense L.) grown in uniform field trial at the experimental farm of the Agricultural Research Centre, Giza (30°N, 31°:28'E), Egypt. The soil texture was a clay loam, with an alluvial substratum, (pH = 8.07). Total water consumptive use during the growing season supplied by surface irrigation was about 6000 m3ha-1. No rainfall occurred during the growing season. The sampling size was 358 plants (Sawan et al. 2005).
100 — 90
~ SO
I 70 = 60 a
I 50 a)
tS 40
£ 30
? 20 GO
10 0
0 4 8 12 16 20 24 28 32 36 40 44 48 52 56 60 64 68
Days after begining of flowering
Figure 3. Daily boll retention ratio during the production stage (68 days) in the first season (I) for the Egyptian cotton cultivar Giza 75 (Gossypium barbadense L.) grown in uniform field trial at the experimental farm of the Agricultural Research Centre, Giza (30°N, 31°:28'E at an altitude 19 m), Egypt. The soil texture was a clay loam, with an alluvial substratum, (pH = 8.07). Total water consumptive use during the growing season supplied by surface irrigation was about 6000 m3 ha-1. No rainfall occurred during the growing season. The sampling size was 261 plants (Sawan et al. 2002).
Days after begining of flowering
Figure 4. Daily boll retention ratio during the production stage (62 days) in the second (II) for the Egyptian cotton cultivar Giza 75 (Gossypium barbadense L.) grown in uniform field trial at the experimental farm of the Agricultural Research Centre, Giza (30°N, 31°:28'E at an altitude 19 m), Egypt. The soil texture was a clay loam, with an alluvial substratum, (pH = 8.07). Total water consumptive use during the growing season supplied by surface irrigation was about 6000 m3 ha-1. No rainfall occurred during the growing season. The sampling size was 358 plants (Sawan et al. 2002).
Figure 5. Daily number of flowers and bolls during the production stage (60 days) in the first season (I) for the Egyptian cotton cultivar Giza 75 (Gossypium barbadense L.) grown in uniform field trial at the experimental farm of the Agricultural Research Centre, Giza (30°N, 31°:28'E), Egypt. The soil texture was a clay loam, with an alluvial substratum, (pH = 8.07). Total water consumptive use during the growing season supplied by surface irrigation was about 6000 m3ha-1. No rainfall occurred during the growing season. The sampling size was 261 plants (Sawan et al. 1999).
0 5 10 15 20 25 30 35 40 45 50 55 60
Days after begnmgof flowering
Figure 6. Daily number of flowers and bolls during the production stage (60 days) in the first season (I) for the Egyptian cotton cultivar Giza 75 (Gossypium barbadense L.) grown in uniform field trial at the experimental farm of the Agricultural Research Centre, Giza (30°N, 31°:28'E), Egypt. The soil texture was a clay loam, with an alluvial substratum, (pH = 8.07). Total water consumptive use during the growing season supplied by surface irrigation was about 6000 m3ha-1. No rainfall occurred during the growing season. The sampling size was 261 plants (Sawan et al. 1999).
Table 1: Range and mean values of the independent variables for the two seasons and over all data.
Climatic factor's First season* Second season** Over all data (Two seasons)
Range Mean Range Mean Range Mean
Max Temp (°C), (X,) 31.0-44.0 34.3 30.6-38.8 34.1 30.6-44.0 34.2
Min Temp (°C), (X2) 18.6-24.5 21.9 18.4-23.9 21.8 18.4-24.5 21.8
Max-Min Temp (°C), (X3) * 9.4-20.9 12.4 8.5-17.6 12.2 8.5-20.9 12.3
Evap (mm d-1), (X4) 7.6-15.2 10.0 4.1-9.8 6.0 4.1-15.2 8.0
0600 h Temp (°C), (X5) 14.0-21.5 17.8 13.3-22.4 18.0 13.3-22.4 17.9
1800 h Temp (°C), (X6) 19.6-27.0 24.0 20.6-27.4 24.2 19.6-27.4 24.1
Sunshine (h d"’), (X7) 10.3-12.9 11.7 9.7-13.0 11.9 9.7-13.0 11.8
Max RH (%), (X8) 62-96 85.4 51-84 73.2 51-96 79.6
Min RH (%), (X9) 11-45 30.8 23-52 39.8 11-52 35.1
Wind speed (m s-1), (X10) ND ND 2.2-7.8 4.6 ND ND
(Sawan et al. 2006).
♦Diurnal temperature range. ND not determined.
*Flower and boll stage (68 days, from 23 June through 29 August). **Flower and boll stage (62 days, from 29 June through 29
August).
Table 2: Simple correlation values for the relationships between the independent variables and the
studied dependent variable.
Independent variables (Climatic factors) Dependent variable
First season Second season Combined data
Flower Boll Flower Boll Flower Boll
Max Temp [°C] (Xt) -0.07 -0.03 -0.42** -0.42** -0.27** -0.26**
Min Temp [°C] (X2) -0.06 -0.07 0.00 0.02 -0.03 -0.02
Max-Min Temp [°C] (X3) -0.03 -0.01 -0.36** -0.37** -0.25** -0.24**
Evapor [mm d-1] (X4) -0.56** -0.53** -0.61** -0.59** -0.40** -0.48**
0600 h Temp [°C] (X5) -0.01 -0.06 -0.14 -0.13 -0.09 -0.09
1800 h Temp [°C] (X6) -0.02 -0.16 -0.37** -0.36** -0.27** -0.25**
Sunshine [h d-1] (X7) -0.25* -0.14 -0.37** -0.36** -0,31** -0.25**
Max RH [%] (X8) 0.40** 0.37** 0.01 0.01 0.04 -0.06
Min RH [%] (X9) 0.14 0.10 0.45** 0.46** 0.33** 0.39**
Wind speed [m s-1] (X10) ND ND -0.06 -0.04 ND ND
(Sawan et al. 2002).
ND not determined P < 0.05; ** P < 0.01.
Table 3. Selected factors and their relative contribution to variations of flower and boll production.
Flower production____________________________________Boll production
Selected climatic factors * R.C. (%) R.C. (%)
First season Second season Combined data First season Second season Combined data
Max Temp [°C] (Xt) - 5.92 - - 5.03 -
Evapor [mm d-1] (X4) 19.08 23.45 16.06 23.04 22.39 22.89
1800 h Temp [°C] (X6) - - 5.83 - - 2.52
Sunshine [h d-1] (X7) 9.43 7.77 8.31 11.65 7.88 5.47
Max RH [%] (Xs) 8.46 - - - - -
Min RH [%] (X9) - 4.37 7.38 - 4.26 4.64
** R2 % for selected factors 36.97 41.47 37.58 34.69 39.56 35.52
R2 % for factors studied 40.22 45.03 40.73 38.43 42.87 37.90
R2 % for factors deleted 3.25 3.56 3.15 3.74 3.31 2.38
(Sawan et al. 2002).
* R.C. % = Relative contribution of each of the selected independent variables to variations of the dependent variable.
** R2 % = Coefficient of determination in percentage form.
Table 4. Range and mean value of the independent variables (climatic factors) during the four periods of flower and boll production stage.
Climatic First priod Second period Third period Fourth period
factors Range Mean Range Mean Range Mean Range Mean
First season
Max Temp °C, (Xi) 31.0-37.333.7 33.0-37.334.7 32.4-37.234.5 32.0-38.433.8
Min Temp °C, (X2) 18.6-23.521.4 20.6-23.522.3 18.9-24.421.6 19.6-23.821.8
Max-Min °C, (X3) 9.4-14.8 12.3 9.8-15.6 12.4 9.7-18.3 12.9 9.5-14.6 12.0
Evapor. mm/d, (X4) 10.2-15.211.7 8.0-13.2 '10.1 7.6-11.2 9.1 7.7-11.1 9.2
0600 h Temp. ' °C,(X5) 14.2-19.916.8 15.8-21.518.9 13.9-21.1 17.4 15.4-20.818.0
8 O O h T CD 3 . o C,(X6) 22.0-25,223.8 22.2-27.024.2 19.6-25.624.1 21.8-26.023.9
Sunshine h/d, (X7) 11.4-12.912.4 10.4-12.411.5 10.5-12.411.6 9.9-12.2 11.4
Max Hum %, (X>) 62-88 80.7 84-94 88.4 85-96 89.9 76-96 87.4
Min Hum %, (X>) 21-37 28.2 22-43 31.4 Second Season 17-42 29.9 24-45 34.0
Max Temp °C, (Xi) 31.4-38.835.5 31.4-35.533.4 32.6-37.934.4 30.6-34.632.8
Min Temp °C, (X2) 20.1-23.421.3 19.6-23.121.7 18.4-24.322.3 18.6-23.921.7
Max-Min °c, (X3) 9.4-17.6 14.2 10.1-15.011.7 9.6-17.0 12.1 8.5-12.6 11.0
Evapor. mm/d, (X4) 5.9-9.8 7.5 5.0-7.0 6.0 4.3-7.1 5.6 4.1-6.1 4.9
0600 h Temp. °C,(X5) 15.5-20.417.5 15.2-21.418.4 12.9-22.418.7 13.3-21.017.5
1800 h Temp. °C,(X6) 22.8-26.524.4 22.2-26.524.2 22.9-27.424.4 20.6-25.823.6
Sunshine h/d, (X7) 11.2-13.012.4 10.9-12.611.9 10.6-12.411.6 10.3-12.311.5
Max-Hum %, (X8) 62-83 71.7 51-82 72.8 59-81 74.7 64-84 73.3
Min Hum %, (X9) 23-44 33.1 32-50 41.3 29-51 39.9 37-52 44.7
Windspeed m/s, (X10) 2.8-6.8 5.1 3.4-6.6 4.5 2.2-7.8 4.4 3.4-5.8 4.5
(Sawan et al. 1999)
Table 5. Significant simple correlation values between the climatic factors and flower, boll production and boll retention ratio due to quarters of production stage.
Climatic factors Flower Boll Ratio:Bolls/Flowers (100)
1st 2nd 3rd 4th 1st 2nd 3rd 4th 1st 2nd 3rd 4th
First season (n by quarter = 1 5)
MaxTemp °C, (X,) n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s..
Min Temp °C, (X) 0.516' 0.607' n.s. n.s. 0.561' 0.638” n.s. n.s. n.s. 0.680'' n.s. n.s.
Max-Min °C, (X3) n.s. n.s. C 1.538 n.s. n.s. n.s. 0 i.494' n.s. 0.515 n.s. n.s. n.s.
Evapor. mm/d, (X) 0.512' 0-.598' n.s. 1 0.424** 0.397' '-0.500' -.0321 *n.s. n.s. -0.387*- -0.287*n.s.
0600 h Temp. °C,(X5) -0.352 *0.534' -0.358*0.301* 0.402' '0.516'- 0.44- I**n.s. n.s. 0.440** n.s. -.292*
1800 h Temp. °C,(X6) n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s. n.s.
Sunshine h/d, (X7) n.s. n.s. 0 1.346' * n.s. n.s. n.s. n.s. 0.430** n.s. n.s. n.s. 0.480'
Max Hum %, (X) -0.316 *-0.260 *0.461**0.283* n.s. n.s. 0. 410** n.s. .389* n.s. n.s. -0.322*
Min Hum %, (X9) n.s. 0.309*- 0.436**n.s. n.s. 1 0.436**- ■0.311 3**n.s. -0.473 **0.527' n.s. n.s.
Second season (n by quarter = : 15)
MaxTemp °C, (X.) n.s. n.s. n.s. ■ -0.730'' n.s. n.s. n.s. - 0.654'' n.s. n.s. 0 .407* * n.s.
Min Temp °C, (X) n.s. n.s. n.s. - 0.451** n.s. n.s. n.s. - 0.343* n.s. n.s. n.s. n.s.
Max-Min °C, (X3) n.s. n.s. 0.598 n.s. n.s. n.s. 0 i.536' n.s. 0.456H '*-0.416 **n.s. . n.s.
Evapor. mm/d, (X) n.s. n.s. 0 i.640' n.s. n.s. n.s. 0 i.580' n.s. n.s. -0.318* n.s. n.s.
0600 h Temp. °C,(X5) 0.397+ '-0.301 *-0.407** 0.506' -0.380 *-0.323 *-0.332* -0.426**n.s. n.s. 0 .283 * n.s.
1800 h Temp. °C,(X6) n.s. - .0440** n.s. ■ -0.656'' n.s.- 0.410** n.s. - ■0.582' -.0626 ' n.s. n.s. n.s.
Sunshine h/d, (X7) 0.362+ ' n.s. n.s. n.s. 0.340' '0.308*. 354* n.s. n.s. 0.409** n.s. n.s.
Max Hum %, (X) -0.523 *0.424++-0.587*n.s. -0530 '0.431** -0.586 n.s. n.s. n.s. n.s. n.s.
Min Hum %, (X9) n.s. n.s. -0.585 i'0.639" n.s. n.s. -0.517 '0.652'' n.s. n.s. n.s. 1 0.420**
n.s. Means simple correlation coefficient is not significant at the 0.15 alpha level of significance.
Significant at 1 % probability level, Significant at 5% probability level.
** Significant at 10% probability level, + Significant at 15% probability level. n Number of data pairs used in calculation.
Wind speed did not show significant effect upon the studied production variables.
(Sawan et al. 1999)
Table 6. Significant simple correlation values between the climatic factors and flower, boll production, and boll retention ratio due to quarters periods of production stage for the combined data of the two seasons. (n =30)
Climatic factors Flower Boll Ratio:Bolls/Flowers (100)
1st 2nd 3rd 4th 1st 2nd 3rd 4th 1st 2nd 3rd 4th
MaxTemp °C, (X) n.s. n.s. 0.29* -0.48'' n.s. n.s. 0.38** -0.47” 0.27* n.s. n.s. n.s.
Min Temp °C, (X2) n.s. n.s. -0.35** ' n.s. n.s. n.s. -0.28* n.s. n.s. n.s. n.s. n.s.
Max-Min °C, (X3) -0.40 -0.30* '0.59''' -0.36** n.s. -0.48 0.52 -0.38** -0.40 -0.47 n.s. -0.28*
Evapor. mm/d, (X4) 0.78 n.s. 0.32** -0.67 0.67 -0.51 n.s. -0.74 n.s. -0.82 -0.49 -0.72
0600 h Temp. °C, (X) n.s. 0.27* -0.43' -0.31* n.s. n.s. -0.37** -0.37** n.s. n.s. n.s. n.s.
1800 h Temp. °C, (X6) n.s. n.s. n.s. -0.42 n.s. n.s. n.s. -0.37** n.s. n.s. n.s. n.s.
Sunshine h/d, (X7) n.s. n.s. 0.38** n.s. n.s. n.s. 0.32** n.s. n.s. 0.30* n.s. 0.27*
Max Hum %, (X) n.s. n.s. n.s. -0.64 n.s. n.s. n.s. -0.71 n.s. -0.60 -0.44 -0.70
Min Hum %, (X) n.s. n.s. -0.54 0.69 -0.32** 0.42 -0.37** 0.72 n.s. 0.72 0.40 0.56
R2 0.667 0.116 0.496 0.672 0.446 0.335 0.389 0.747 0.219 0.737 0.269 0.615
(Sawan et al. 1999)
Climatic factors Flower Boll Ratio
Table 7. Significant simple correlation values between the climatic factors and flower, boll ratio for combined data of the two seasons (n = 120).production and boll retention
MaxTemp “C, (X,) -0.152++ n.s. n.s.
Min Temp “C, (X2) n.s. n.s. n.s.
Max-Min “C, (Хз) -0.259" -0.254" n.s.
Evapor.mm/d, (X4) -0.327" -0.429" -0.562"
0600 h Temp. “C, (X5) n.s. n.s. n.s.
1800 h Temp. “C, (X6) -0.204^ -0.190++ n.s.
Sunshine h/d, (X7) -0.227^ -0.180++ n.s.
Max Hum %, (X8) n.s. n.s -0.344".
Min Hum %, (X9) 0.303" 0.364" 0.335"
R2 0.406''
(Sawan et al. 1999)
CONCLUSION
Evaporation, sunshine duration, relative humidity, surface soil temperature at 1800 h, and maximum temperature, were the most significant climatic factors affecting flower and boll production of Egyptian cotton. Also, it could be concluded that the fourth quarter period of the production stage is the most appropriate and usable production time to collect data for determining efficient prediction equations for cotton flower and boll production in Egypt, and making valuable recommendations. Further, it could be concluded that evaporation, minimum relative humidity and sunshine duration, were the most significant climatic factors affecting cotton flower and boll production and retention in Egyptian cotton. The negative correlation between each of evaporation and sunshine duration with flower and boll formation along with the positive correlation between minimum relative humidity value and flower and boll production, indicate
0.422" 0.336^
that low evaporation rate, short period of sunshine duration and high value of minimum humidity would enhance flower and boll formation. Temperature appeared to be less important in the reproduction growth stage of cotton in Egypt than evaporation (water stress), sunshine duration and minimum relative humidity. These findings concur with those of other researchers except for the importance of temperature. A possible reason for that contradiction is that the effects of evaporation rate and relative humidity were not taken into consideration in the research studies conducted by other researchers in other countries. The matter of fact is that temperature and evaporation are closely related to each other to such an extent that the higher evaporation rate could possibly mask the effect of temperature. Water stress is in fact the main player and other authors have suggested means for overcoming its adverse effect which could be utilized in the Egyptian cotton. It must
be kept in mind that although the reliable prediction of the effects of the aforementioned climatic factors could lead to higher yields of cotton, yet only 50% of the variation in yield could be statistically explained by these factors and hence consideration should also be given to the management practices presently in use. Evaporation and sunshine duration appeared to be important climatic factors affecting boll production in Egyptian cotton. Our findings indicate that increasing evaporation rate and sunshine duration resulted in lower boll production. On the other hand, relative humidity, which had a positive correlation with boll production, was also an important climatic factor. In general, increased relative humidity would bring about better boll production.
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