Impact of Weather Variability and Soil Moisture Deficit ...

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maximum soil moisture deficit on WU and WUE of sweet corn. Impact of Weather Variability and Soil Moisture Deficit on. Water Use and Water Use Efficiency of ...
Impact of Weather Variability and Soil Moisture Deficit on Water Use and Water Use Efficiency of Sweet Corn Axel Garcia y Garcia*, Larry C. Guerra, and Gerrit Hoogenboom *[email protected] Department of Biological and Agricultural Engineering, The University of Georgia

Introduction

Materials and Methods

Rainfall (mm)

450 40

Maximum Air Temperature Average Air Temperature Minimum Air Temperature

0 Rainfall Cumulative Rainfall Cumulative Evapotranspiration

500 375

20

250 10

125 0 Apr

May

Jun

Jul

Aug

0 450

April 10 Irrigated

300 Anthesis

150

Water Use

10

-3

Anthesis

150

Mar

12

March 27 Irrigated

250

Y = -0.078 + 0.023*X; r2 = 0.84

9

300

April 25 Irrigated

Cumulative Rainfall or Cumulative Rainfall + Irrigation Cumulative Evapotranspiration

0

2006

03/15

100

3

Anthesis

150

50 100

0 04/05

04/26

05/17

2006

06/07

06/28

0

50

100

150

200

130

250

160

190

220

250

Maximum Soil Moisture Deficit

Maximum Soil Moisture Deficit

¾ The soil moisture was monitored in each replicate twice per week using a PR2 at six fixed depths (10, 20, 30, 40, 60, and 100 cm). The PR2 uses electromagnetic signals to measure the permittivity of the soil (dominated by the water)

¾ A marked difference was observed between cumulative rainfall and cumulative potential evapotranspiration (ET0) during the growing season. The cumulative rainfall / ET0 were 86/330, 75/300, 130/279 for March 27, April 10, and April25 growing seasons, respectively.

¾ Rainfall and irrigation were recorded with rain gauges installed in the experimental area; other weather variables were recorded with an automatic weather station located near the experiment.

¾Water use was reduced from 268 mm to 119 mm, while the maximum soil moisture deficit varied from 117 mm to 205 mm.

Acknowledgements

Orthogonal contrasts for WUE of sweet corn total aboveground biomass and fresh and dry matter ears Water Use Efficiency Mean comparison for aboveground biomass, fresh and dry matter of ears, and WUE Yield (t ha-1) Treatment

WUE (kg m-3)

Ears

Aboveground biomass

Fresh

March 27 rainfed

5.5a

March 27 irrigated

7.4b

April 10 irrigated

7.6b

April 25 irrigated LSD

Ears

Contrast

Ears

Total Aboveground biomass

Fresh

Dry matter

March 27 irrigated vs. March 27 rainfed

< 0.0001*

< 0.0001*

< 0.0001*

April 10 vs. March 27 rainfed

< 0.0001*

< 0.0001*

< 0.0001*

0.26ns

0.18ns

0.55ns

Dry matter

Aboveground biomass

Fresh

13.1a

3.8a

4.70a

11.40a

19.1b

4.7b

2.83b

7.30b

1.7b

March 27 irrigated vs. April 10 irrigated

0.32ns

0.20ns

0.76ns

20.4c

4.4b

2.85b

7.60b

1.65b

March 27 irrigated vs. April 25 irrigated

< 0.0001*

< 0.0001*

< 0.0001*

5.7a

14.5d

3.3a

4.2c

10.60a

2.44c

April 10 irrigated vs. April 25 irrigated

< 0.0001*

< 0.0001*

< 0.0001*

0.70

0.43

0.32

0.36

0.47

0.27

Irrigated vs. Rainfed

< 0.0001*

< 0.0001*

0.0002*

Within columns, means with the same letter are not significantly different at p < 0.05. LSD = Least Significant Difference

Dry matter 2.8a

April 25 irrigated vs. March 27 rainfed

¾ Biomass of fresh ears was more sensitive to soil moisture deficit than for both total aboveground biomass and ears, as the relationship WUE of fresh ears and soil moisture deficit had a higher slope. ¾ Further work will study the potential impact of timing of soil moisture deficit on yield of sweet corn.

¾ A significant difference was found between WUE of irrigated and rainfed conditions for both, total aboveground biomass and ears. However, no significant differences were found for WUE of the sweet corn plant on April 25 under irrigated conditions and the rainfed experiment.

¾ A water balance equation was used to determine the crop’s daily evapotranspiration using the PR2’s soil moisture readings. Water use was calculated as the sum of the crop’s daily evapotranspiration (ETa). WUE was determined for aboveground biomass and fresh and dry matter as their ration with ETa.

¾ An analysis of variance was conducted for aboveground biomass, fresh and dry matter ears yield as well as for WUE. Orthogonal contrasts were also performed for WUE between treatments.

¾ The higher the soil moisture deficit, the higher the WUE for total aboveground biomass and for yield of fresh and dry matter ears.

0 450

¾ The growing season was dry and hot. March was exceptionally warm and early April was exceptionally cool. These conditions resulted in temporary stress of the crop from the March 27 planting date for irrigated conditions and in an early stressed crop for the rainfed conditions.

¾ As a measure of the crop’s moisture stress, potential soil moisture deficit was calculated as the accumulated difference between daily PET and irrigation amount for each treatment. The maximum soil moisture deficit reached during the crop’s growth was used.

200

150

6

¾ Sweet corn (sh2 type) was planted using a simple one-way randomized complete block design and four replicates of three planting dates; including March 27 (one rainfed and one irrigated) and April 10 and April 25, both irrigated. Irrigation was applied with a linear sprinkler irrigation system.

¾ Growth analysis data were collected every two weeks. At harvest, yield and yield components were obtained in 3-m row length from each replicate.

¾ Water use efficiency of sweet corn differed significantly between planting dates and between both rainfed and irrigated conditions.

300

0

¾ An experiment was conducted in 2006 at the Bledsoe Research Farm of The University of Georgia in Pike County, Georgia, USA, in a Cecil sandy clay loam soil.

March 27, rainfed Y = 506 - 1.94*X; r2 = 0.84

Aboveground biomass (dry matter)

450

Solar Radiation

20

30

April 25, irrigated

Y = -0.126 + 0.014*X; r2 = 0.85

WUE (kg m )

0 30

April 10, irrigated

Ears (dry matter)

¾ Sweet corn water use was markedly affected by the soil moisture deficit. ¾ The higher the soil moisture deficit, the smaller the amount of water used by the sweet corn.

March 27, irrigated

300

Y = 1.67 + 0.047*X; r2 = 0.74

15

0

10

Water use of sweet corn as a function of the maximum soil moisture deficit

Ears (fresh)

March 27 Rainfed

Anthesis

150

20

Conclusions

Water use efficiency of sweet corn as a function of the maximum soil moisture deficit

300

30

mm

¾The objectives of this study were to determine the impact of weather variability and maximum soil moisture deficit on WU and WUE of sweet corn.

Cumulative rainfall and irrigation for each treatment

Cumulative Rainfall and Cumulative ET 0 (mm)

Air Temperature (oC)

¾ASW is depleted due to the crop’s uptake at a rate determined by PET (Stone et al., 2001) until the soil reaches a state of moisture deficit and growth stops. Beyond that point, crops are exposed to stresses that have cumulative effects and ultimately can reduce final biomass (Jamieson et al., 1995).

Results Weather conditions during the 2006 cropping season at Bledsoe Research Farm, Pike County, GA.

Solar Radiation (MJ m-2 d-1)

¾Water use (WU) and water use efficiency (WUE) of crops are affected by weather conditions and available soil water (ASW) (Tanner and Sinclair, 1987). Weather conditions determine the extent of the potential evapotranspiration (PET), whereas ASW acts as the reservoir to respond to that demand.

* Contrasts are significantly different at p < 0.05; ns = no significant difference between contrasts

This work was conducted under the auspices of the Southeast Climate Consortium (SECC; secc.coaps.fsu.edu) and supported by a partnership with the United States Department of Agriculture-Risk Management Agency (USDA-RMA), by grants from the US National Oceanic and Atmospheric Administration-Climate Program Office (NOAACPO) and USDA Cooperative State Research, Education and Extension Services (USDA-CSREES) and by State and Federal funds allocated to Georgia Agricultural Experiment Stations Georgia Agricultural Experiment Stations Hatch project GEO01654

References Jamieson, P.D., R.J. Martin, G.S. Francis, and D.R. Wilson. 1995. Drought effects on biomass production and radiation-use efficiency in barley. Field Crop Research 43:77-86. Stone, P.J., D.R. Wilson, J.B. Reid, and R.N. Gillespie. 2001. Water deficit effects on sweet corn. I. Water use, radiation use efficiency, growth, and yield. Aust. J. Agric. Res. 52:103-113. Tanner, C.B., and T.R. Sinclair. 1983. Efficient water use in crop production: Research or research? p. 1-27. In H.M. Taylor et al. (ed.) Limitations to efficient water use in crop production. ASA-CSSA-SSSA, Madison, WI.