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Soil water content in soils Rafael Mu ñ oz-Carpena Outline Soil Hydrology A soil and water “refresher” Capillarity theory Field capacity Atmosphere Soil Aquifer Hydrological Methods This refers to water balance methods. RO: Runoff P: Precipitation F: Soil Infiltration

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Soil water content in soils l.jpg

Soil water content in soils

Rafael Muñoz-Carpena


Outline l.jpg
Outline

  • Soil Hydrology

  • A soil and water “refresher”

  • Capillarity theory

  • Field capacity


Hydrological methods l.jpg

Atmosphere

Soil

Aquifer

Hydrological Methods

This refers to water balance methods.

RO: Runoff

P: Precipitation

F: Soil Infiltration

D: Deep percolation

Dq= Soil moisture

If RO=0 and all but

ET are measured we

can Estimate ET


Soil is made of three components l.jpg

SOIL

Volume

Mass

Air

Water

Solids

Soil is made of three components

  • Pore space=Va+Vg

  • Porosity=Pore space/total volume= (Va+Vg)/V

  • Water content (in volume) = Volume of water/total volume =Va/V

    (in weight)=Ma/Ms

  • Bulk density= Mass of solids/total volume = Ms/V

Water is held in the soil pores


Soil particle size have an effect on soil water holding capacity l.jpg

Sand

Silt

Clay

Soil particle size have an effect on soil water holding capacity

Texture is made out by the the relative content of each of the soil particles

Pores are spaces between particles


As does soil structure l.jpg

Block

Prismatic

…as does soil structure…

  • Structure is the association of particles in larger lumps.


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A paradox?

  • The coarser the soil the less water it contains

  • - The coarser the particles the larger the pores but the total amount of pores is small

  • On the other hand…

  • -The finer the particles the smaller the pores but the total amount of pores is large.

Also water flows slower in fine soils…


Does love make the world go around l.jpg
Does love make the world go around?

  • Energy, or rather differences in energy do…

  • The universe tends spontaneously to lower energy stages: “chaos” or “disorder”

  • Soil water movement follows the same pattern


Water in soil is related to energy l.jpg

Air water soil root

Water in soil is related to energy

  • Water does not move freely as it does above the surface, but is held in the grasp of the soil which determines how it will move and how much energy (work) the plant roots have to invest to withdraw it .

(Drawing source: SoilMoisture, Inc.)


Potential energy in the soil l.jpg
Potential: Energy in the soil root

  • t = g +p +o

    t: total

    g: gravitational

    p: pressure

    o: osmotic


As soil dries more energy is needed l.jpg

Wet soil Dry soil root

As soil dries more energy is needed

Increasing work is required to remove the water from the small sized pores compared to the large pores, as the soil dries out. Because of this, plants find it increasingly difficult to get adequate water as the soil dries. When remaining water is held only in extremely small pore spaces, the plants cannot exert enough force to withdraw it, and the plants wilt and die

(even when there is still water in the soil).

(Drawing: SoilMoisture, Inc.)


Pressure capillary potential l.jpg
Pressure (capillary) potential root

  • P=g |hc|

  • Weight-unit volume

    units p= hc

    |hc| = 2 cos  / (gr)


Moisture is related to suction l.jpg

Clay root

Sand

Water content (in3H2O/in3Soil)

Suction,

Moisture is related to suction

  • “Soil Suction”(negative pressure potential) is the work that plants have to do to get needed water, and the energy that determines which way moisture will move in the soil.

  • Water content in the soil is related to suction (energy)



Moisture holding is related to texture l.jpg

Clay root

Sand

Water content (in3H2O/in3Soil)

Suction,

Moisture holding is related to texture

  • Coarse soil releases moisture rapidly with less energy required.

  • Fine soils hold moisture longer, even at high energy (suction)

  • Water content in the soil is related to texture


Texture vs structure l.jpg

Clay root

Sand

Water content (cm3H2O/cm3Soil)

Structure

Suction,

Texture vs. Structure

Texture


Field capacity hydrology or agronomy l.jpg
Field capacity: Hydrology or Agronomy? root

  • In 1949 Veihmeyer and Hendrickson “in 2-3 days after rain or irrigation in soils of uniform texture and structure soils”

  • When gravitational and capillary forces equilibrate after a water application event, the soil stops draining freely.


Slide19 l.jpg


Slide20 l.jpg

Field capacity (redistribution does not stop after FC). In sandy soils the concept is closer to reality (why?)

(w/ organic matter)

(w/o organic matter)

(w/ organic matter)

Water content

(w/o organic matter)

Wilting point

Clay


Slide23 l.jpg

Questions? (redistribution does not stop after FC). In sandy soils the concept is closer to reality (why?)


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