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Water & Solute Movement

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Presentation on theme: "Water & Solute Movement"— Presentation transcript:

1 Water & Solute Movement
A solid, liquid, or gas that is dissolved in a liquid to make a solution. When the solute has an electrical charge, the mobility of the solute is affected

2 Soil Properties & Water Movement
Infiltration The ability of water to move into the soil from the soil surface Permeability The ability of water to move through the soil horizon after it has penetrated the surface Is controlled by its least permeable horizon

3 Soil Properties & Water Movement
Solute movement is affected by pH OM CEC Soil texture Soil structure

4 Soil Properties & Water Movement
Soil pH influences the solubility and ionic state of a solute and thus influences its mobility OM can absorb and adsorb many times its own weight, tying up solutes with the notable exception of K, thus reducing their mobility CEC reflects the number of binding sites available for a positively charged solute to bind to

5 Soil Properties & Water Movement
Soil texture: Finer textured soils usually have a higher CEC and less movement of solutes Soil Structure: Well-structured soils allow for more movement of solutes down into the soil profile Reduces the risk of runoff Increases the chance of solute movement into a shallow water supply

6 Soil Properties & Water Movement
Other factors that affect solute movement: Timing Rate of application Tillage Conservation practices Irrigation

7 Soil Properties & Water Movement
Timing of a solute applied close to time of crop use has less time for excessive movement. Rates of application above what is needed for crop production can lead to excessive leaching, runoff, or residual. Tillage promotes good infiltration and reduces runoff potential

8 Soil Properties & Water Movement
Tillage (contd) Breaks up non-permeable zones Improves water use Conservation practices, like terracing, strip cropping, etc.. all trap water and soil particles and thus, the dissolved and retained solutes. Irrigation can increase solute leaching

9 Nutrient Movement in the Soil & Water
Non-Point Source Pollution: Cannot be traced to a specific location point or time of entry. Ag chemicals from field runoff Nitrate movement into ground water Point Source Pollution: Entry into the environment can be traced to a single event or sequence of events at an inclusive location Chemical spill at a well head Fertilizer spill into a storm sewer

10 Plant & Water Relationships
Evapotranspiration (ET): The loss of water from the soil by both surface evaporation and plant transpiration Is influenced by stage of crop growth, water status, and soil water potential As the crop grows, evaporation tends to decrease and transpiration increases As the soil water decreases, more energy is required to remove water from the soil

11 Plant & Water Relationships
Wind Increases evaporation losses Increases transpiration losses to a point…. Temperature works the same way wind does Warm air can hold more water (humidity) than cold air Solar radiation (sunlight) eventually becomes heat energy

12 Plant & Water Relationships
Relative humidity A measure of the concentration of water vapor in the air The higher the Relative Humidity the less likely there will be a need for supplemental water

13 Plant & Water Relationships
Plant canopy Reduces soil evaporation but increases transpiration Evapotranspiration is not proportional to the amount of size of plant canopy, but does trend higher as the plant canopy expands

14 Plant & Water Relationships
How plants lose water Stomata on leaf surfaces Stomata open and close according to temperature, humidity, wind, and soil water supply 98% of the water transpired is used to cool the plant

15 Plant & Water Relationships
Excessive soil moisture Reduces nutrient availability Reduces oxygen availability for root growth Roots can begin to die within 48 hours Denitrification in water-logged soils can account for major nitrogen losses

16 Plant & Water Relationships
Soil Moisture Deficiency Plant requires more energy to move water Affects nutrient movement & uptake N movement by mass flow K movement by mass flow & diffusion P movement by diffusion

17 Water Holding Capacity
Type Available Water (in/ft) Course sand to 0.75 Fine sand to 1.00 Loamy sand to 1.20 Sandy loam to 1.40 Fine sandy loam to 2.00 Silt loam to 2.50 Silty clay loam to 2.00 Silty clay to 1.70 Clay to 1.50

18 Available Water Handout

19 Permeability Classification System

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21 The Hydrologic Cycle

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23 Water Quality Concerns Ground water contamination
Surface water contamination Nitrate can contaminate both Nitrate reported in two ways Nitrate NO ppm (or mg/l) Nitrate-N NO3-N 10 ppm (or mg/l)

24 Water Quality Health affects of nitrate in drinking water
Methemoglobinemia (Blue Baby Syndrome) which is the result of poor O2 transport in the blood of very young babies Formation of nitrosamines, known carcinogens that form when nitrates react with organic compounds

25 Water Quality Water Contamination Occurs often at well heads
Considered a point-source pollutant Can enter through cracked casings, improper seals, or ponded contaminants near well head Sources of information about drinking water standards: US EPA, State Public Health and Environmental Agencies

26 Water Quality Prevention of water contamination
Use anti-backsiphoning devices Never fill or dump pesticides or fertilizers near a well head Fill depressional areas around a well head

27 Sediments & Surface Water Quality
Sediments settle out of the water stream As the flow of the water slows In reduced water temperature Sediments are considered pollutants The sediment itself Contaminants bound to the sediment Phosphorus contamination is primarily through sediment contamination (organic P exception)

28 P and N Effects on Surface Water Quality
Causes eutrophication where algae and weeds flourish Eutrophic waters have High nutrient levels Low species diversity Low dissolved oxygen Poor taste and odor Excessive vegetation (slows flow and….) Can be turbid and cause fish kills

29 Preventing Surface Water Contamination
Filter/buffer strips Plant along surface water shores Slows water movement and causes sediment to drop out before entering the main body of water Riparian Areas or Tree Plantings Serves the same purpose as above Both methods are effective in using up nitrates and phosphorus.


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