2011
DOI: 10.1016/j.agwat.2011.09.010
|View full text |Cite
|
Sign up to set email alerts
|

Components of the water balance in soil with sugarcane crops

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
19
2
7

Year Published

2014
2014
2022
2022

Publication Types

Select...
10

Relationship

1
9

Authors

Journals

citations
Cited by 36 publications
(29 citation statements)
references
References 19 publications
1
19
2
7
Order By: Relevance
“…By the criteria of Warrick and Nielsen (1980), this variability can be classified as medium in the first three crop stages and high for the end of the cycle. In addition, data variation was much higher in the last period, when rainfalls were recorded, confirming that the greatest variations in the internal drainage process occur in the periods of greatest rainfall (Ghiberto et al, 2011b).…”
Section: Internal Drainage (D) and Capillary Rise (Cr)supporting
confidence: 48%
“…By the criteria of Warrick and Nielsen (1980), this variability can be classified as medium in the first three crop stages and high for the end of the cycle. In addition, data variation was much higher in the last period, when rainfalls were recorded, confirming that the greatest variations in the internal drainage process occur in the periods of greatest rainfall (Ghiberto et al, 2011b).…”
Section: Internal Drainage (D) and Capillary Rise (Cr)supporting
confidence: 48%
“…The K(θ) and at 0.2 and 0.9 m soil depth were calculated from weekly readings of tensiometers installed at depths of 0.15, 0.25, 0.85 and 0.95 m. The tensiometer readings were monitored for 36 months (Feb 2009to Jan 2012. To calculate the soil water flux density, we determined the soil water retention curve to obtain the soil water content from tensiometer readings and then the soil hydraulic conductivity K from the equation of K as a function of volumetric water content obtained at both depths (0.2 and 0.9 m) by the instantaneous profile method (Ghiberto et al, 2011).…”
Section: Native Vegetationmentioning
confidence: 99%
“…Soil water dynamics provides essential knowledge for agricultural management practices during different phenological stages for crop yield improvement (Zougmoré et al, 2004;Ghiberto et al, 2011), whereas ET provides important information for water management both in irrigated and dry soil conditions. However, records on ET data for forage cactus are few around the world and practically non-existent in the Brazilian semiarid region, where this crop is of great economic importance (Oliveira et al, 2010).…”
Section: Introductionmentioning
confidence: 99%