PROPERTIES OF WATER RELATED WITH PLANT

PROPERTIES OF WATER  During KSS WONDERFUL DISCUSSION WITH ShriJKP SIR

PLANT CONTENT herbaceous plants - 85-95% water  woody plants - 75-85% water  FUNCTIONS OF WATER 1) solvent - dissolves solutes;                      - the cytosol of the cytoplasm is a water solution of dissolved solutes.  2) reagent - water is used in biochemical reactions, such as photosynthesis.  3) translocation medium - water translocates solutes in xylem and phloem.  4) temperature relations - water is very important in regulating temperature.      a) stabilizes plants and environment (due to high specific heat)      b) evaporative cooling (due to heat of vaporization)      c) releases heat when freezes (due to heat of fusion)      d) constant temperature during phase change - freezing/melting  water/ice stays at 32 oF.  5) turgor pressure and growth     turgor pressure - the positive pressure inside of cells due to water uptake.      a) turgor pressure is due to osmosis.      b) turgor pressure keeps cells expanded      c) turgor pressure keeps herbaceous plants and plant parts erect     d) turgor pressure is the driving force for growth in size by causing cell expansion    growth - an irreversible increase in size or mass.    plasmolysis - shrinkage of individual cells due to loss of turgor pressure that causes a cell to                            become flaccid.     wilting - excessive water loss that causes loss of plant rigidity.                   - caused by plasmolysis of enough individual cells to cause the organ to be limp.

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ATMOSPHERIC WATER

UNITS FOR EXPRESSING HUMIDITY humidity - amount of water vapor in air; can be expressed as: a)absolute humidity - amount of water vapor in air expressed as grams water per cubic meter                                      of air (g/m3)  b) specific humidity - amount of water vapor in air expressed as grams water per kilogram of                                    air (g/kg)  c) relative humidity - amount of water vapor in air expressed as a percentage of the amount of                                    water vapor that could be held at saturation.  d) vapor pressure - amount of water vapor in air expressed as the downward pressure exerted                                 by the water vapor present in the atmosphere. (1-55 mm Hg).  RELATIONSHIP BETWEEN HUMIDITY AND TEMPERATURE dew point - the temperature where relative humidity equals 100%.  condensation - conversion of water vapor to liquid or ice; condensation occurs when the                           temperature drops below the current dew point.  precipitation - loss of atmospheric water; occurs when condensation is extensive enough that                         the water or ice coalesce to form droplets/crystals that fall from the atmosphere                         due to the force of gravity.  Cold air can hold less water vapor than warm air, so as temperature decreases the absolute humidity or specific humidity that can be held at saturation decreases.  Relative humidity is a percent of saturation.  So as temperature decreases the absolute or specific humidity at saturation decreases, but the amount of water vapor present stays the same, thus relative humidity increases (conversely, as temperature increases relative humidity decreases). If the temperature continues to decrease (such as cooling over night or as air rises in the atmosphere),  a temperature is reached where the relative humidity reaches 100% - this temperature is the dew point.  If the temperature drops below the current dew point, the air becomes over saturated and condensation will occur.  If this occurs in the upper atmosphere, a cloudforms or precipitation occurs. If this occurs close to the earth's surface, fog or dew forms  TYPES OF CONDENSATION 1) dew - condensation of water onto solid surfaces  2) fog - condensation of water into small droplets that stay suspended in air close to the              earth's surface.  3) cloud - condensation of water into small droplets that stay suspended in air high in the                 atmosphere.  TYPES OF PRECIPITATION I) condensation occurs above freezing (when dew point is above 32 oF)      a)drizzle - water droplets less than 0.5 mm      b)rain - water droplets greater than 0.5 mm.  2) condensation occurs below freezing (when dew point is below 32 oF)      a) snow - water condenses below freezing directly into small, loose ice crystals.  3) condensation occurs above freezing, followed by freezing     a)sleet - liquid rain droplets fall through a layer of freezing air and then freeze.      b)hail - liquid rain droplets fall through a layer of freezing air and then freeze; air currents                   carry the frozen droplets back up into the upper atmosphere; they pick-up more water,                   then freeze upon falling through the layer of freezing air; each time the ice crystal                   circulates through the warm and freezing layer it gets larger until it finally falls to earth.

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PRECIPITATION OR HYDROLOGIC CYCLE

. Aquifers An aquifer is an underground  layer of porous rock, sand, or gravel, through which water can seep or be held in natural storage. Aquifers generally hold sufficient water to be used as a water supply.  Many aquifers are enormous, with one of the largest being the Ogallala, which stretches from southern South Dakota to the panhandle of Texas.  One of the largest within Texas is the Edwards Aquifer, which stretches from the Hill Country to the San Antonio area.

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PATHWAY OF WATER THROUGH PLANTS

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ABSORPTION, TRANSLOCATION AND TRANSPIRATION OF WATER

TERMINOLOGY absorption - uptake of water by roots.  translocation - movement of water through plants, mainly through xylem.  transpiration - loss of water vapor from leaves and other above ground plant parts;                          - mainly occurs through the stomata.  guttation - loss of liquid water from leaves;                    - occurs through hydathodes (similar to stomata, but they do not close).  SITE OF WATER ABSORPTION 1) young roots - most absorption, mainly through root hairs due to:      a) very numerous - 14 billion on a typical rye plant.      b) large surface area -14,000 ft2 (1310 m2) on a typical rye plant      c) rapidly and constantly produced - 975 linear ft (300 m) per day on a squash plant  2) older roots - little absorption due to:      a) suberization of endodermis      b) periderm (bark) formation  COHESION THEORY OF TRANSLOCATION IN THE XYLEM 1) Transpiration occurs and is driving force  2) Causes negative pressure in leaves  3) Column of water is pulled up in the xylem and translocated due to:     a) H-bonding (hydrogen-bonding)     b) small size of xylem pores     c) negative charges on xylem walls  FUNCTIONS OF TRANSLOCATION 1) driving force for translocation: transpiration causes a negative pressure in leaves, which      "pulls" the water up the xylem.  2) evaporative cooling of leaves:  540 cal of heat energy is dissipated for every gram of water      that evaporates from leaves, which is a major contributor to the cooling of leaves.  Transpiration is usually much greater than is needed to satisfy these two functions. Thus, many horticultural practices attempt to minimize excessive transpiration.

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FACTORS THAT AFFECT TRANSPIRATION

PLANT FACTORS 1) leaf area - smaller leaf area decreases transpiration  2) leaf orientation - vertically orientated leaves decrease transpiration  3) leaf surface - waxy, hairy or shiny leaf surfaces decrease transpiration  4) stomata - when stomata are closed, transpiration decreases  ENVIRONMENTAL FACTORS 1) humidity- high humidity decreases transpiration  2) temperature     a) low temperature decreases transpiration.      b) high temperature increases transpiration, but when it gets too hot the stomata close, then          transpiration may decrease  3)light intensity     a) darkness decreases, because stomata close, (except for CAM plants open at night)      b) high light intensity increases temperature which increases transpiration, until stomata close          then transpiration may decrease; occurs midday during heat of summer  4) wind     a) as wind increases transpiration increases      b) if wind gets too high, then stomata close and transpiration may decrease  5) soil water     a) when soil is moist, transpiration occurs according to the above factors      b) when soil is too dry, stomata close causing transpiration to decrease           (over rides above factors)  TECHNIQUES TO DECREASE TRANSPIRATION 1) mistor spray foliage      a) in propagation an intermittent mist system is used      b) mid-afternoon sprinkler irrigate plants in greenhouses/nurseries  2) decrease light intensity - grow plants under shade  3) harden-off seedlings     a) decrease watering,      b) decrease temperature, or      c) decrease fertilizer, especially N.  4) antitranspirants - chemicals that close or clog stomata.      Two Types     a) physiologically cause stomatal closure      b) wax, resin or latex that clogs stomata

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METHODS OF IRRIGATION

Types Uses Advantages Disadvantages  OUTDOOR SYSTEMS 1)Surface Irrigation      a) flood rice, orchards,  cranberry 1) good wetting  2) frost protection 1) need level land  2) uses lots of water  3) some plants sensitive      b) basin rice, orchards,  cranberry 1 & 2) same as flood  3) irrigate sections 1 & 2) same as flood  3) upkeep of levees  4) slightly unleveled land      c) furrow row crops 1) less water used  2) ideal for rows 1) uneven distribution  2) supervise for erosion 2)Sprinkler      Irrigation container plants,  turf,  high value fruits  and vegetables 1) irrigate section  2) can be automated  3) evaporative cooling  4) frost protection 1) high cost  2) wind disrupts  3) nozzles clog  3)Drip or Trickle      Irrigation fruit (2.5 gal/hr/tree)  row crops (300-400  gal/acre/day) 1) most water efficient  2) less plant stress  3) low pressure equip 1) high cost  2) emitters clog  GREENHOUSE SYSTEMS 1) Manual anything 1) personal monitoring 1) high labor costs  2) Chapin Tube or      Spaghetti Tube  container plants 1) keeps foliage dry  2) can be automated 1) must use fine medium  2) gets tangled  3) high costs  3) Capillary Mat container plants 1) constant moisture,      maximum growth 2) keeps foliage dry 3) can be automated 1) need fine medium  2) 6" or less pots  3) too wet for some  4) algae growth on mat  4) Subirrigation     or Ebb & Flow container plants 1) keeps foliage dry 2) can be automated  1) high cost  2) disease may spread  5) Spray Nozzles  bench crops 1) can be automated 1) moderate cost  6) Sprinkler container plants,  bench crops 1) can be automated  2) evaporative cooling 1) high cost  2) nozzles clog