Performance Evaluation of Four Models for Estimating the Capillary Rise in Wheat Crop Root Zone Considering Shallow Water Table

Author(s):  
Arunava Poddar ◽  
Navsal Kumar ◽  
Vijay Shankar
2019 ◽  
Vol 213 ◽  
pp. 486-498 ◽  
Author(s):  
Guanfang Sun ◽  
Yan Zhu ◽  
Ming Ye ◽  
Jinzhong Yang ◽  
Zhongyi Qu ◽  
...  

1997 ◽  
Vol 77 (2) ◽  
pp. 249-251 ◽  
Author(s):  
J. W. Paul ◽  
V. Etches ◽  
B. J. Zebarth

Indirect measurements of denitrification to 120 cm depth in a coarse textured soil in October showed higher denitrification rates following a single spring application of dairy cattle slurry than following a spring application of fertilizer. The highest denitrification rates occurred immediately above and below the water table (90 cm depth) and resulted primarily from C applied in the manure moving down through the soil profile. Key words: Dairy cattle slurry, carbon, nitrate, shallow water table


2013 ◽  
Vol 3 ◽  
pp. 123-127
Author(s):  
M.H. Ali ◽  
I. Abustan ◽  
S. Islam

The upward movement of water by capillary rise from shallow water-table to the root zone is an important incoming flux. For determining exact amount of irrigation requirement, estimation of capillary flux or upward flux is essential. Simulation model can provide a reliable estimate of upward flux under variable soil and climatic conditions. In this study, the performance of model UPFLOW to estimate upward flux was evaluated. Evaluation of model performance was performed with both graphical display and statistical criteria. In distribution of simulated capillary rise values against observed field data, maximum data points lie around the 1:1 line, which means that the model output is reliable and reasonable. The coefficient of determination between observed and simulated values was 0.806 (r = 0.93), which indicates a good inter-relation between observed and simulated values. The relative error, model efficiency, and index of agreement were found as 27.91%, 85.93% and 0.96, respectively. Considering the graphical display of observed and simulated upward flux and statistical indicators, it can be concluded that the overall performance of the UPFLOW model in simulating actual upward flux from a crop field under variable water-table condition is satisfactory. Thus, the model can be used to estimate capillary rise from shallow water-table for proper estimation of irrigation requirement, which would save valuable water from over-irrigation.


2010 ◽  
Vol 136 (5) ◽  
pp. 289-299 ◽  
Author(s):  
Purnendu N. Singh ◽  
Wesley W. Wallender ◽  
Marco P. Maneta ◽  
Stephen L. Lee ◽  
Beatrice A. Olsen

1992 ◽  
Vol 13 (1) ◽  
Author(s):  
S.A. Prathapar ◽  
C.W. Robbins ◽  
W.S. Meyer ◽  
N.S. Jayawardane

Ground Water ◽  
2003 ◽  
Vol 41 (7) ◽  
pp. 964-972 ◽  
Author(s):  
James B. Shanley ◽  
K. Niclas Hjerdt ◽  
Jeffrey J. McDonnell ◽  
Carol Kendall

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