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LH1  WaterPlant and Soil Water Relationships<br />
Many Plants are 90% Water<br /><ul><li>Water is essential for chemical reactions of plants, especially the process of phot...
Water keeps cells rigid so that they don’t collapse
Water is the primary vehicle for transporting plant nutrients, sugars, hormones and all other biochemical molecules within...
Areas of High Water Potential include very wet or moist soils or where the molecules of water are greater than molecules o...
Areas of Low Water Potential include leaf tips where water is actively evaporating, also any tissue such as roots which ha...
Roots and other plant parts contain high concentrations of solutes:  molecules dissolved in water necessary for all bioche...
Water moves into roots from an area of high water potential to low water potential in an attempt to equalize the contents ...
Water Travels Upwards in Plants through the Xylem Through Cohesion and Adhesion<br />Cohesion is the attraction water mole...
Xylem is formed by sections of long ultrathin segments known as vessel elements or tracheids<br />
Water lost through Stomatal Pores when they are open for gas exchange is known as TRANSPIRATION<br /><ul><li>In temperate ...
Stomata close if a dark cloud passes overhead during the day and they close at night.</li></li></ul><li>Stomates are prima...
Transpiration of Water into the Atmosphere is fueled by the Sun’s Radiant Energy and the process of the movement of water ...
Temperatures are high
 Under warm and windy conditions
If there is full sun, as opposed to cloudy conditions or plants growing in shade</li></li></ul><li>Plants Have Adapted Man...
Needle-like Leaves Reduce Surface Area Loss of Water<br />
Summer Dormancy in Mediterranean Climates<br />Babianacorms grow during wet winters and …<br />Are dormant in the summer<b...
Water Movement in Soil<br />Gravitational Water:  water that moves down through the soil due to the effect of gravity<br /...
A Totally Saturated SoilOccurs During a Rainstorm<br />
<ul><li>Water is held is small pores between soil particles
This water is held against the pull of gravity by the forces of adhesion, the attraction of water molecules to other parti...
This water is known as Capillary water. It is the available water in the soil which plants can suck off of soil particles
Capillary forces can move water laterally or upward through the small soil pores through the cohesion of water molecules f...
When all available water is removed by plants or has evaporated there remains Hydroscopic Water<br /><ul><li>Hydroscopic W...
Plant root hairs cannot obtain this water from the soil particles</li></li></ul><li><ul><li>Sandy soils have the lowest fi...
Adding organic matter to sandy soils can significantly increase its field capacity
Clay soils hold more capillary water and also hydroscopic water
At the point where plants cannot obtain water from a soil they will wilt
If they are not quickly watered they may reach their PWP (Permanent Wilting Percentage) and die!</li></ul> Soils differ in...
With Clay soils, water must be applied more slowly and more water must be applied to water at the same depth as a sandy or...
More water must be applied to a clay soil to reach the same depth as sandy or loamy soil<br />
Movement of Water into Soil is known as Infiltration<br />*When the application of water is higher than infiltration then ...
How to Determine the Water Content of the Soil?<br />Tensiometer is an airtight, hollow tube filled with water with a poro...
Hand-Feel Test<br />
Practical Hand-Feel Test<br />
Water Quality<br />
Misc. Water Quality Parameters<br />
Hard  vs. Soft Water<br />Hard Water is due to high levels of dissolved minerals, commonly calcium and magnesium<br />Caus...
Guidelines for Using Grey Water in the Garden<br />Mix washwater with rinse-cycle water before using on plants<br />Some p...
Chlorine in Bleach will damage plants, let water stand overnight before using to let chlorine dissipate<br />Boron will bu...
Watering and Irrigation<br />
Hunter Sprayers used for some Large Landscape Installations but wasteful<br />
Underground Watering Systems(E.g. Netafim)<br />
Micro-Sprayers<br />
Microsprayer Set-up<br />
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Lh1 water

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Introductory Lecture for Landscape Horticulture on Water: Plant and Soil Relationships

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Transcript of "Lh1 water"

  1. 1. LH1 WaterPlant and Soil Water Relationships<br />
  2. 2. Many Plants are 90% Water<br /><ul><li>Water is essential for chemical reactions of plants, especially the process of photosynthesis
  3. 3. Water keeps cells rigid so that they don’t collapse
  4. 4. Water is the primary vehicle for transporting plant nutrients, sugars, hormones and all other biochemical molecules within the plant</li></li></ul><li>Water Moves Through Plants From Areas of High Water Potential to Low Water Potential<br /><ul><li>Water Potential is essentially the same as Water Concentration
  5. 5. Areas of High Water Potential include very wet or moist soils or where the molecules of water are greater than molecules of dissolved minerals
  6. 6. Areas of Low Water Potential include leaf tips where water is actively evaporating, also any tissue such as roots which have high concentrations of dissolved minerals and molecules</li></li></ul><li><ul><li>Water is absorbed by the roots through the process of osmosis, which is the diffusion of fluid through a semi-permeable membrane until there is an equal concentration on both sides of the membrane
  7. 7. Roots and other plant parts contain high concentrations of solutes: molecules dissolved in water necessary for all biochemical reactions.
  8. 8. Water moves into roots from an area of high water potential to low water potential in an attempt to equalize the contents of the plant cells</li></ul>OsmosisThe process which water enters the Root System<br />
  9. 9. Water Travels Upwards in Plants through the Xylem Through Cohesion and Adhesion<br />Cohesion is the attraction water molecules have for other water molecules. <br />Adhesion is the attraction between water molecules on mineral particles<br />
  10. 10. Xylem is formed by sections of long ultrathin segments known as vessel elements or tracheids<br />
  11. 11. Water lost through Stomatal Pores when they are open for gas exchange is known as TRANSPIRATION<br /><ul><li>In temperate climates, due to extreme water loss, at 92-94 deg F, stomata start to close, at 100 degrees all stomata close and the plant “shuts down” and photosynthesis cannot occur
  12. 12. Stomata close if a dark cloud passes overhead during the day and they close at night.</li></li></ul><li>Stomates are primarily located on the underside of leaves<br />
  13. 13. Transpiration of Water into the Atmosphere is fueled by the Sun’s Radiant Energy and the process of the movement of water through a plant is known as Transpirational Pull<br />Each water molecule is “connected” to other water molecules due to attraction of Hydrogen and Oxygen of different molecules <br />Transpirationincreases if:<br /><ul><li>Air has low humidity
  14. 14. Temperatures are high
  15. 15. Under warm and windy conditions
  16. 16. If there is full sun, as opposed to cloudy conditions or plants growing in shade</li></li></ul><li>Plants Have Adapted Many Mechanisms to prevent water loss and survive periods of drought<br />Waxy coating to prevent loss of water<br />Specialized water storage stems<br />
  17. 17. Needle-like Leaves Reduce Surface Area Loss of Water<br />
  18. 18. Summer Dormancy in Mediterranean Climates<br />Babianacorms grow during wet winters and …<br />Are dormant in the summer<br />
  19. 19. Water Movement in Soil<br />Gravitational Water: water that moves down through the soil due to the effect of gravity<br />Capillary Water: Water that is held on soil particles and aggregates which can be used by plants<br />Hydroscopic Water: Water that is bound tightly to soil particles and not available to plants<br />
  20. 20. A Totally Saturated SoilOccurs During a Rainstorm<br />
  21. 21. <ul><li>Water is held is small pores between soil particles
  22. 22. This water is held against the pull of gravity by the forces of adhesion, the attraction of water molecules to other particles
  23. 23. This water is known as Capillary water. It is the available water in the soil which plants can suck off of soil particles
  24. 24. Capillary forces can move water laterally or upward through the small soil pores through the cohesion of water molecules from areas of high water potential to low water potential</li></ul>Field CapacityA measure of the amount of water a soil retains after gravitational water drains<br />
  25. 25. When all available water is removed by plants or has evaporated there remains Hydroscopic Water<br /><ul><li>Hydroscopic Water is held tightly by the soil particle through adhesion
  26. 26. Plant root hairs cannot obtain this water from the soil particles</li></li></ul><li><ul><li>Sandy soils have the lowest field capacity
  27. 27. Adding organic matter to sandy soils can significantly increase its field capacity
  28. 28. Clay soils hold more capillary water and also hydroscopic water
  29. 29. At the point where plants cannot obtain water from a soil they will wilt
  30. 30. If they are not quickly watered they may reach their PWP (Permanent Wilting Percentage) and die!</li></ul> Soils differ in their ability to retain water, both capillary and hydroscopic water<br />
  31. 31. With Clay soils, water must be applied more slowly and more water must be applied to water at the same depth as a sandy or loamy soil<br /><ul><li>A clay soil will hold more water in a smaller volume of soil, closer to the surface</li></ul>*Clay soils take longer to saturate due to its small pore spaces. But when it is saturated it holds onto the water more tightly and water drains less well<br />
  32. 32. More water must be applied to a clay soil to reach the same depth as sandy or loamy soil<br />
  33. 33.
  34. 34. Movement of Water into Soil is known as Infiltration<br />*When the application of water is higher than infiltration then run-off will occur<br />*Infiltrometer gauges how fast water will penetrate soil. Will give you an idea of soil texture.<br />
  35. 35. How to Determine the Water Content of the Soil?<br />Tensiometer is an airtight, hollow tube filled with water with a porous end inserted into the soil<br />A vacuum gauge at the other end measures the pull exerted by the soil on the water. The greater the pressure the drier the soil<br />
  36. 36. Hand-Feel Test<br />
  37. 37. Practical Hand-Feel Test<br />
  38. 38. Water Quality<br />
  39. 39. Misc. Water Quality Parameters<br />
  40. 40. Hard vs. Soft Water<br />Hard Water is due to high levels of dissolved minerals, commonly calcium and magnesium<br />Causes spots on dishes, scale on shower heads, and can clog drip irrigation emmiters<br />Hard Water is worse in S. California <br />Soft Water has <br />
  41. 41. Guidelines for Using Grey Water in the Garden<br />Mix washwater with rinse-cycle water before using on plants<br />Some plants are more sensitive, eg. Azaleas and strawberries<br />Do not use wash water for potted plants with restricted root zones<br />Do not pour directly onto base of plants which may cause crown rot<br />Use of black water not allowed by law<br />
  42. 42. Chlorine in Bleach will damage plants, let water stand overnight before using to let chlorine dissipate<br />Boron will burn leaf edges. Fabric softeners contain either boron or metaphosphates containing sodium. Use natural detergents.<br />Phosphates will generally not hurt plants, usually acts as a fertilizer, but can cause algae blooms in lakes and streams.<br />
  43. 43. Watering and Irrigation<br />
  44. 44. Hunter Sprayers used for some Large Landscape Installations but wasteful<br />
  45. 45. Underground Watering Systems(E.g. Netafim)<br />
  46. 46. Micro-Sprayers<br />
  47. 47. Microsprayer Set-up<br />
  48. 48. My Microsprayer Set Up!<br /><ul><li>Independent Irrigation Timer run by batteries
  49. 49. Filter
  50. 50. Pressure Reducer</li></li></ul><li>
  51. 51. Many Different Types of Sprayers are Available<br />
  52. 52.
  53. 53. Swale Gardens<br />
  54. 54. How Deep to Water?<br />LEAFY VEGETABLES AND ANNUALS<br />6 inches – 1 foot<br />SMALL SHRUBS, COOL SEASON TURFGRASS, CORN, TOMATOES<br />1 feet – 2 feet<br />LARGE SHRUBS, TREES, WARM-SEASON TURFGRASS<br />1.5 feet – 5 feet<br />
  55. 55. Soil Auger to test how deep you are actually watering<br />
  56. 56. How Much Water Do Plants Require?<br />Water is loss from plants through TRANSPIRATION<br />Water is also lost from the soil surface through EVAPORATION<br />Total water loss from plants and soil is known as EVAPOTRANSPIRATION<br />WATER LOSS THROUGH EVAPOTRANSPIRATION MUST BE REPLACED FOR HEALTHY PLANTS <br />
  57. 57. AVERAGE SEASONAL EVAPOTRANSPIRATION RATES VARY BY LOCATION IN CALIFORNIA<br /><ul><li>Evapotranspiration rates are established for different regions of the state
  58. 58. Coastal Areas have lower evapo-transpiration rate
  59. 59. Northern California generally has lower evapotranspiration rates than S. California</li></li></ul><li>How Much to Water and How Long to Water?<br />It all depends on: <br /><ul><li>Soil texture
  60. 60. Type of plant and root depth
  61. 61. Evapotranspiration Coefficient,
  62. 62. Wind, heat, rainfall
  63. 63. Topography: slopes usually require more water, also Southern exposures
  64. 64. You type of irrigation system</li></li></ul><li>Measure Water Application Rate and Depth of Penetration<br /><ul><li>Put tuna cans out in various locations
  65. 65. Turn on irrigation system for 20 min., measure inches of water & multiply by 3 to determine inches of water per hour
  66. 66. If the amounts vary by more than 15-20% your irrigation system needs adjusting
  67. 67. Run normal irrigation time or until run-off starts. Check to see how deep the water has penetrated
  68. 68. Adjust water time to allow water to penetrate proper depth</li></li></ul><li>What time of Day to Water?<br />Morning is best<br /><ul><li>Less evaporation, better water pressure
  69. 69. Plants begin using water as soon as sunrise
  70. 70. Fewer disease Problems, no children</li></ul>Midday is worst<br /><ul><li>High evaporation,
  71. 71. Low water pressure
  72. 72. Wind, children</li></ul>Evening has problems<br /><ul><li>Low water pressure
  73. 73. Disease and rots
  74. 74. Wind, less water Pressure</li></li></ul><li>How to Conserve Water in a Drought?<br />Prune back large plants to reduce water need and loss<br />Move container plants to shade and out of wind<br />Mulch to reduce water evaporation<br />Water deeply and infrequently<br />Remove weeds, remove your lawn<br />Plant drought tolerant natives and Mediterranean Plants<br />Do not fertilize heavily to avoid lush growth<br />Create berms to localize water<br />
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