Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table

Salloom B. Salim; Luma S. Khudhair

doi:doi:10.11648/j.ijaas.20150103.17

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Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table

Salloom B. Salim, Luma S. Khudhair

Published in International Journal of Applied Agricultural Sciences (Volume 1, Issue 3)

Received: 24 August 2015 Accepted: 6 September 2015 Published: 14 September 2015

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Abstract

To determine the elements of soil water balance equation during the growing season detailed description for calculating daily contribution rates to evapotranspiration of wheat (ET) from applied irrigation water (ET_r) and upward flux capillarity (ET_c), depth of applied irrigation water (DAIW), change in water storage (Λ_s) and cumulative evapotranspiration (ET_cum) were algorithmed in this study. Irrigation water was applied to three different depths 30, 30-60 and 60 cm at three different depletion rates 50, 70 and 90% from plant available water. Wheat ET ranged from 428.49 to 522.12 mm. Contributions to ET from applied irrigation water ranged from 334.20 to 496.50 mm and increased with increasing irrigation depth. Contributions to ET from upward flux capillarity ranged from 25.61 to 96.59 mm and decreased with increasing irrigation depth. Contributions to ET from applied irrigation water decreased with increasing depletion rate whilst contributions to ET from upward flux capillarity increased with increasing depletion rates. Daily rate contribution to evapotranspiration from irrigation water ranged from 2.15 to 3.20 mm.d-1 and from capillary flux ranged from 0.16 to 0.61 mm.d-1.

Published in	International Journal of Applied Agricultural Sciences (Volume 1, Issue 3)
DOI	10.11648/j.ijaas.20150103.17
Page(s)	84-90
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2015. Published by Science Publishing Group

Keywords

Shallow Water Table, Water Balance, Depletion Rate, Capillary Flux, Cumulative Evapotranspiration

References

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APA Style

Salloom B. Salim, Luma S. Khudhair. (2015). Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table. International Journal of Applied Agricultural Sciences, 1(3), 84-90. https://doi.org/10.11648/j.ijaas.20150103.17

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ACS Style

Salloom B. Salim; Luma S. Khudhair. Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table. Int. J. Appl. Agric. Sci. 2015, 1(3), 84-90. doi: 10.11648/j.ijaas.20150103.17

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AMA Style

Salloom B. Salim, Luma S. Khudhair. Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table. Int J Appl Agric Sci. 2015;1(3):84-90. doi: 10.11648/j.ijaas.20150103.17

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@article{10.11648/j.ijaas.20150103.17,
  author = {Salloom B. Salim and Luma S. Khudhair},
  title = {Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table},
  journal = {International Journal of Applied Agricultural Sciences},
  volume = {1},
  number = {3},
  pages = {84-90},
  doi = {10.11648/j.ijaas.20150103.17},
  url = {https://doi.org/10.11648/j.ijaas.20150103.17},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijaas.20150103.17},
  abstract = {To determine the elements of soil water balance equation during the growing season detailed description for calculating daily contribution rates to evapotranspiration of wheat (ET) from applied irrigation water (ETr) and upward flux capillarity (ETc), depth of applied irrigation water (DAIW), change in water storage (Λs) and cumulative evapotranspiration (ETcum) were algorithmed in this study. Irrigation water was applied to three different depths 30, 30-60 and 60 cm at three different depletion rates 50, 70 and 90% from plant available water. Wheat ET ranged from 428.49 to 522.12 mm. Contributions to ET from applied irrigation water ranged from 334.20 to 496.50 mm and increased with increasing irrigation depth. Contributions to ET from upward flux capillarity ranged from 25.61 to 96.59 mm and decreased with increasing irrigation depth. Contributions to ET from applied irrigation water decreased with increasing depletion rate whilst contributions to ET from upward flux capillarity increased with increasing depletion rates. Daily rate contribution to evapotranspiration from irrigation water ranged from 2.15 to 3.20 mm.d-1 and from capillary flux ranged from 0.16 to 0.61 mm.d-1.},
 year = {2015}
}

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TY  - JOUR
T1  - Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table
AU  - Salloom B. Salim
AU  - Luma S. Khudhair
Y1  - 2015/09/14
PY  - 2015
N1  - https://doi.org/10.11648/j.ijaas.20150103.17
DO  - 10.11648/j.ijaas.20150103.17
T2  - International Journal of Applied Agricultural Sciences
JF  - International Journal of Applied Agricultural Sciences
JO  - International Journal of Applied Agricultural Sciences
SP  - 84
EP  - 90
PB  - Science Publishing Group
SN  - 2469-7885
UR  - https://doi.org/10.11648/j.ijaas.20150103.17
AB  - To determine the elements of soil water balance equation during the growing season detailed description for calculating daily contribution rates to evapotranspiration of wheat (ET) from applied irrigation water (ETr) and upward flux capillarity (ETc), depth of applied irrigation water (DAIW), change in water storage (Λs) and cumulative evapotranspiration (ETcum) were algorithmed in this study. Irrigation water was applied to three different depths 30, 30-60 and 60 cm at three different depletion rates 50, 70 and 90% from plant available water. Wheat ET ranged from 428.49 to 522.12 mm. Contributions to ET from applied irrigation water ranged from 334.20 to 496.50 mm and increased with increasing irrigation depth. Contributions to ET from upward flux capillarity ranged from 25.61 to 96.59 mm and decreased with increasing irrigation depth. Contributions to ET from applied irrigation water decreased with increasing depletion rate whilst contributions to ET from upward flux capillarity increased with increasing depletion rates. Daily rate contribution to evapotranspiration from irrigation water ranged from 2.15 to 3.20 mm.d-1 and from capillary flux ranged from 0.16 to 0.61 mm.d-1.
VL  - 1
IS  - 3
ER  -

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Author Information

Salloom B. Salim

Department of Soil Sciences and Water Resources, College of Agriculture, Baghdad University, Baghdad, Iraq
Luma S. Khudhair

Extension Specialists, Ministry of Agriculture, Baghdad, Iraq

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Plain Text BibTeX RIS

APA Style

Salloom B. Salim, Luma S. Khudhair. (2015). Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table. International Journal of Applied Agricultural Sciences, 1(3), 84-90. https://doi.org/10.11648/j.ijaas.20150103.17

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ACS Style

Salloom B. Salim; Luma S. Khudhair. Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table. Int. J. Appl. Agric. Sci. 2015, 1(3), 84-90. doi: 10.11648/j.ijaas.20150103.17

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AMA Style

Salloom B. Salim, Luma S. Khudhair. Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table. Int J Appl Agric Sci. 2015;1(3):84-90. doi: 10.11648/j.ijaas.20150103.17

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@article{10.11648/j.ijaas.20150103.17,
  author = {Salloom B. Salim and Luma S. Khudhair},
  title = {Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table},
  journal = {International Journal of Applied Agricultural Sciences},
  volume = {1},
  number = {3},
  pages = {84-90},
  doi = {10.11648/j.ijaas.20150103.17},
  url = {https://doi.org/10.11648/j.ijaas.20150103.17},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijaas.20150103.17},
  abstract = {To determine the elements of soil water balance equation during the growing season detailed description for calculating daily contribution rates to evapotranspiration of wheat (ET) from applied irrigation water (ETr) and upward flux capillarity (ETc), depth of applied irrigation water (DAIW), change in water storage (Λs) and cumulative evapotranspiration (ETcum) were algorithmed in this study. Irrigation water was applied to three different depths 30, 30-60 and 60 cm at three different depletion rates 50, 70 and 90% from plant available water. Wheat ET ranged from 428.49 to 522.12 mm. Contributions to ET from applied irrigation water ranged from 334.20 to 496.50 mm and increased with increasing irrigation depth. Contributions to ET from upward flux capillarity ranged from 25.61 to 96.59 mm and decreased with increasing irrigation depth. Contributions to ET from applied irrigation water decreased with increasing depletion rate whilst contributions to ET from upward flux capillarity increased with increasing depletion rates. Daily rate contribution to evapotranspiration from irrigation water ranged from 2.15 to 3.20 mm.d-1 and from capillary flux ranged from 0.16 to 0.61 mm.d-1.},
 year = {2015}
}

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TY  - JOUR
T1  - Determination of the Elements of Soil Water Balance for Wheat (Triticum aestivum L.) Under Shallow Water Table
AU  - Salloom B. Salim
AU  - Luma S. Khudhair
Y1  - 2015/09/14
PY  - 2015
N1  - https://doi.org/10.11648/j.ijaas.20150103.17
DO  - 10.11648/j.ijaas.20150103.17
T2  - International Journal of Applied Agricultural Sciences
JF  - International Journal of Applied Agricultural Sciences
JO  - International Journal of Applied Agricultural Sciences
SP  - 84
EP  - 90
PB  - Science Publishing Group
SN  - 2469-7885
UR  - https://doi.org/10.11648/j.ijaas.20150103.17
AB  - To determine the elements of soil water balance equation during the growing season detailed description for calculating daily contribution rates to evapotranspiration of wheat (ET) from applied irrigation water (ETr) and upward flux capillarity (ETc), depth of applied irrigation water (DAIW), change in water storage (Λs) and cumulative evapotranspiration (ETcum) were algorithmed in this study. Irrigation water was applied to three different depths 30, 30-60 and 60 cm at three different depletion rates 50, 70 and 90% from plant available water. Wheat ET ranged from 428.49 to 522.12 mm. Contributions to ET from applied irrigation water ranged from 334.20 to 496.50 mm and increased with increasing irrigation depth. Contributions to ET from upward flux capillarity ranged from 25.61 to 96.59 mm and decreased with increasing irrigation depth. Contributions to ET from applied irrigation water decreased with increasing depletion rate whilst contributions to ET from upward flux capillarity increased with increasing depletion rates. Daily rate contribution to evapotranspiration from irrigation water ranged from 2.15 to 3.20 mm.d-1 and from capillary flux ranged from 0.16 to 0.61 mm.d-1.
VL  - 1
IS  - 3
ER  -

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