IRRIGATION_2 - PowerPoint PPT Presentation

About This Presentation
Title:

IRRIGATION_2

Description:

adhesion force (attractive force betweenthe solid particle and the water) ... KS is the Darcy coefficient of proportionality. Soil-water-plant relationship ... – PowerPoint PPT presentation

Number of Views:30
Avg rating:3.0/5.0
Slides: 24
Provided by: ormos1
Category:

less

Transcript and Presenter's Notes

Title: IRRIGATION_2


1
IRRIGATION_2
  • Design of Irrigation Systems
  • by
  • László Ormos

2
Soil properties
  • Soil texture(water holding capacity)
  • Clay lt0.002 mm
  • Silt 0.002-0.02mm
  • Fine sand 0.02-0.2mm
  • Coarse sand 0.2-2mm
  • Gravel gt2mm

3
Soil properties
  • Soil structure (infiltration rate)

4
Soil-water-plant relationship
  • Soil moisture
  • Total water potential acting is as following
  • where
  • Pt is the total water potential,
  • Pm is matric potential due to capillary forces,
  • adhesion force (attractive force betweenthe
    solid particle and the water)
  • cohesion force (attraction between water
    molecules)
  • Pg is gravitational potential due to the
    gravity,
  • Po is osmotic potential due to the dissolved
    salts in the water,
  • Pp is pressure potential due to the position with
    respect to a fixed
  • datum level.

5
Soil-water-plant relationship
  • Classes and availabilities of soil water

Available moisture
Unavailable moisture
6
Soil-water-plant relationship
  • Hysteresis effect

Suction
Moisture content
7
Soil-water-plant relationship
  • The movement of water in the soil
  • Hydraulic conductivity (or flow velocity)
  • where
  • Q is the amount of water which moves through the
    soil,
  • A is the cross section area of the tested soil
    sample,
  • H is the difference in water pressure head
    between two points,
  • L is the distance between the two points,
  • KS is the Darcy coefficient of proportionality.

8
Soil-water-plant relationship
  • KS in saturated soil is the following
  • KnS in unsaturated soil is the following
  • where hG is the hydraulic gradient computed as
    follows
  • H1 and H2 are pressure head values.

9
Soil-water-plant relationship
  • Infiltration under various methods of irrigation
  • Furrow irrigation gravitational influence,
  • Flood irrigation gravitational influence,
  • Sprinkler irrigation water distribution is more
    or less symmetrical,
  • Micro-sprinkler the distribution pattern is
    trapezoid, and wets the area only partially
    (50-70),
  • Drip irrigation cone-shaped volume of moistured
    soil surrounding the plant root-zone, size
    and shape depend on the type of soil, the
    discharge of dripper, and the duration of
    water application.

10
Soil-water-plant relationship
Water distribution in the soil
Root distribution in the various soil layers
40
D/4
Root zone extraction Depth D
30
D/4
20
D/4
10
D/4
11
Soil-water-plant relationship
  • Storage in soil
  • Small pores are required to store the water.
  • Medium-sized pores help the movement of water in
    the soil.
  • Large-sized pores are required for aeration of
    soil.
  • The saturation
  • Saturation capacity means the pores of soil are
    full filled with water.
  • Gravity occurs the water drains quickly from the
    root zone.

12
Soil-water-plant relationship
  • Field capacity Fc
  • The moisture content of soil means the remained
    water quantity after the gravitational water has
    been removed.
  • Field capacity depends on the texture of soil.
  • Permanent wilting point Pw
  • It is the minimum of the available moisture of
    soil.
  • When water content is at the wilting point or it
    is lower then plants permanently wilt and they
    might not be recovered after being placed in
    moisturized environment.
  • Wilting point is influenced by soil texture.
  • Temporary wilting point
  • It is occurred in any hot windy days but plants
    will recover in cooler portion of days.

13
Soil-water-plant relationship
  • Available soil water AW
  • where AW is in percent of moisture volume, ?S is
    the specific density of soil and ?W is the
    specific water density.
  • The depth of available soil water for a 1m layer
    AWDm

14
Soil-water-plant relationship
  • The depth of available water in the soil layer of
    depth Z AWDZ
  • where Z means the soil layer of depth.
  • The available water volume in the soil layer of
    depth Z AWVZ

15
Soil-water-plant relationship
  • The depth of available water in the main root
    zone Zr of the
  • crop AWDZr
  • where Zr is the depth of main root zone.
  • After replacement in this equation, calculation
    directly the
  • depth of available water in the main root zone is
    as follows

16
Soil-water-plant relationship
  • The available water volume in the main root zone
    Zr of the
  • crop in a hectare AWZr
  • The net water application NWA
  • where PWD is the permitted water deficit.
  • The available net water application in the main
    root zone Zr
  • of the crop in a hectare AWZr

17
Soil-water-plant relationship
  • The gross water application GWA
  • where ?irr is the efficiency of irrigation.
  • The irrigation interval IrI
  • where CU may be either the consumptive use, or
    evapotranspiration.

18
Soil-water-plant relationship
  • Calculate the available water volume per hectare
    in a soil
  • with a homogeneous profile according to the
    following data
  • Field capacity Fc17
  • Wilting point Pw7
  • Soil density ?S1.3g/cm3
  • Water density ?W1.0g/cm3
  • Main root zone Zr0.4m

19
Soil-water-plant relationship
  • Available water by volume
  • The depth of available water for a 1m layer
  • The depth of available water in the effective
    root zone Zr

20
Soil-water-plant relationship
  • 4. The available water in a hectare, in the
    effective root zone Zr

21
Soil-water-plant relationship
  • Calculate the available water volume per hectare
    in a soil with different
  • texture layer according to the following data

Layer Layer Depth Layer thickness Soil texture Fc Pw ?S
cm m w w g/cm3
1 0-20 0.2 Sandy-loam 13 5 1.5
2 20-35 0.15 loam 20 8 1.4
3 35-65 0.30 Clay-loam 27 13 1.4
4 65-110 0.45 clay 32 16 1.3
22
Soil-water-plant relationship
  • The applied equation is

Fc-Pw ?S g/cm3 Zr m AWDZr mm/layer
13-5 1.5 0.2
20-8 1.4 0.15
27-13 1.4 0.3
32-16 1.3 0.1
AWDZr (Zr0.75m)
24.0
25.2
58.8
20.8
128.8
23
References
Azenkot, A.(1998)Design Irrigation System.
Ministry of Agricul- ture Extension Service
(Irrigation Field service), MASHAV Israel Dr.
Avidan, A.(1995)Soil-Water-Plant Relationship.
Ministry of Agriculture Extension Service
(Irrigation Field service), CINADCO, Ministry of
Foreign Affairs, MASHAV, Israel Sapir, E.-Dr. E.
Yagev (1995)Drip Irrigation. Ministry of
Agricul- ture and Rural Development, CINADCO,
Ministry of Foreign Affairs, MASHAV,
Israel Sapir, E.-Dr. E. Yagev (2001)Sprinkler
Irrigation. Ministry of - culture and Rural
Development, CINADCO,Ministry of Foreign
Affairs, MASHAV, Israel Eng. Nathan, R.
(2002)Fertilization Combined with Irrigation
(Fertigation). Ministry of Agriculture and Rural
Development, CINADCO,Ministry of Foreign Affairs,
MASHAV, Israel
Write a Comment
User Comments (0)
About PowerShow.com