1986
DOI: 10.1061/(asce)0733-9437(1986)112:3(242)
|View full text |Cite
|
Sign up to set email alerts
|

Emitter Spacing and Geometry of Wetted Soil Volume

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
104
1
17

Year Published

2000
2000
2024
2024

Publication Types

Select...
10

Relationship

0
10

Authors

Journals

citations
Cited by 145 publications
(123 citation statements)
references
References 6 publications
1
104
1
17
Order By: Relevance
“…Soil water flow under trickle irrigation is described as line source, two-dimensional or point source, threedimensional depending on the distance between emitters along a lateral according to [5] [6]. In case of a line source, emitters are spaced in order to produce a continuous strip of wetted soil along the row.…”
Section: Introductionmentioning
confidence: 99%
“…Soil water flow under trickle irrigation is described as line source, two-dimensional or point source, threedimensional depending on the distance between emitters along a lateral according to [5] [6]. In case of a line source, emitters are spaced in order to produce a continuous strip of wetted soil along the row.…”
Section: Introductionmentioning
confidence: 99%
“…Equations 1 and 2 express the relationship of wetted depth and width to emitter discharge. 2 (Schwartzmass and Zur 1985), where z vertical distance to wetting front (m); w wetted width or diameter of water pattern (m); K 1 29.2 (empirical coe cient); V w volume of water applied (l); C s saturated hydraulic conductivity of the soil (m/s); q point-source emitter discharge (l/h); and K 2 0.031 (empirical coef®cient). Equations 1 and 2 illustrate that the wetted width is large while the vertical distance to wetting front is short if emitter discharge is large when the volume of water applied is the same.…”
Section: Introductionmentioning
confidence: 99%
“…According to [27,28], ECa mapping is one of the most valuable methods in agriculture for measuring the spatial variability of soil properties at field and landscape scales. We also conducted field measurements of the unsaturated soil hydraulic conductivity within each mapped soil zone using a retention disk infiltrometer (Soil Measurement Systems, LLC, Tucson, AZ, USA), and then estimated the maximum vertical and horizontal dimensions of wetted area for different drip emitter flow rates with irrigation durations from 1 h to 24 h according to the method proposed by Schwartzman and Zur [29] for determining the geometry of a wetted soil zone under point-source water application. Based on these measurements and calculations, for treatment number 2 we selected an optimal soil-specific SDI setup, among those commercially available, consisting of driplines spaced 0.…”
Section: Field Research Experiments At Uc Facilitiesmentioning
confidence: 99%