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BASIC HORTICULTURE – NOTES WEEK #9 THE AMBIENT ENVIRONMENT –TEMPERATURE THE ROOT ENVIRONMENT - WATER and SOILS HAND BACK LAB SHEETS – ASSIGNMENTS PASS BACK EXAM and REVIEW THE AMBIENT ENVIRONMENT - TEMPERATURE Plants EVOLVED with the EARTH’S various TEMPERATURE regimes Limited to 0 – 50 degrees C (32 – 122 degrees F) BEST GROWTH @ 10 - 30 degrees C (50 – 85 degrees F) o @ 0 degrees C (32 F) - biological ACTIVITY SLOWS or STOPS o @ > 122 degrees F - PROTEINS destroyed, PLANT INJURY or DEATH As TEMPERATURE RISES every 10 degrees GROWTH can INCREASE 1.3 – 5 X’s (2 X’s average) Growers use this fact to INCREASE or DECREASE GROWTH by increasing or decreasing TEMPERATURE THERMOPERIODICITY Is the FLUCTUATION of DAY and NIGHT TEMPERATURES Most plant GROWTH occurs at NIGHT o STOMATA are closed, decrease in TRANSPIRATION o ROOTS still take in water, increase of TURGOR pressure in cells, o CELLS swell and ENLARGE for GROWTH Plants from GROW BETTER with THERMOPERIODICITY o Important to TEMPERATE CLIMATE plants because they have ADAPTED to FLUCTUATION o Not so important to tropical plants VERNALIZATION The INITIATION of FLOWERING in plants by exposure to EXTENDED COLD PERIODS o Most BIENNIALS – only FLOWER after first season of COLD WINTER TEMPERATURES First year – VEGETATIVE GROWTH Second year – FLOWERING after a COLD PERIOD Example: Foxgloves, Cabbage, Dill, Onion, Celery, Hollyhocks Some plants have specific CHILLING REQUIREMENTS o ABSOLUTE – a certain number of DAYS BELOW a certain TEMPERATURE to flower in spring Example: beets, celery, and cabbage o QUANTITATIVE – flower EARLIER and MORE with exposure to COLD Stimulus for this VERNALIZATION is perceived in the APICAL MERISTEM o Not fully understood o APPLICATION of GIBBERELINS can substitute for LOW TEMPS HIGH TEMPS can REVERSE vernalization or DEVERNALIZE plants Example: Onion sets are stored at HIGHER TEMPS so they will keep in a VEGETATIVE STATE otherwise at lower temps they would go to flower too early DORMANCY and HARDINESS DORMANCY is state of INACTIVE GROWTH due to INTERNAL and EXTERNAL FACTORS o ADAPTIVE MECHANISM that SLOWS DOWN plant PROCESSES during winter months o Only allows a plant to BREAK DORMANCY when ENVIRONMENTAL CONDITIONS are FAVORABLE for GROWTH and DEVELOPMENT o Ensures SPECIES SURVIVAL BUD BREAK in deciduous plants SEED GERMINATION PLANT and BUD DORMANCY o DORMANCY is key for SURVIVAL of PERENNIAL plants growing in TEMPERATE or COLD CLIMATES o GRADUAL PROCESS that STARTS as GROWTH TAPERS in SUMMER TRIGGERED by: SHORTENING DAYS LOWER TEMPS DROUGHT STEPS to PLANT DORMANCY: PHOTOSYNTHESIS SLOWS or STOPS o DECIDUOUS plant STOPS o EVERGREEN SLOWS GROWTH STOPS TRANSLOCATION of FLUIDS reduced Decreased ENERGY REQUIREMENTS PROGRESSION through plant AXILLARY BUDS first o summer pruning TERMINAL BUDS >>> BRANCHES >>> TRUNK >>> BARK last ROOTS never become truly dormant, they CONTINUE to GROW as long as SOIL TEMPS > 40 degrees o ROOTS can never attain cold HARDINESS o Can attain some COLD TOLERANCE but it can be LOST in 24 HRS o MULCHING for ROOTS is important to MODERATE EXTREME TEMPS HARDINESS and ACCLIMATION o HARDINESS - The ABILITY of a DORMANT plant to withstand COLD TEMPS without severe TISSUE DAMAGE DORMANCY must be achieved FIRST before HARDINESS o ACCLIMATION - the ability to DEVELOP HARDINESS Plants gain HARDINESS through a CONSTANT EXPOSURE to COLDER TEMPS or ACCLIMATION o DEGREE of HARDINESS changes in RESPONSE to the ENVIRONMENT, and the responsiveness of the plant DEPENDS on the GROWTH STAGE of the plant (Show overhead) BUD BREAK to LEAF MATURITY – not hardy Initiation of HARDINESS begins as DAY LENGTH DROPS below a CDL TRIGGERS DORMANCY HORMONE in leaves AUXIN lessens breaks down ETHYLENE GAS & ABSCISSIC ACID (ABA) By LEAF ABSCISSION - DORMANCY COMPLETE ACCLIMATION occurs with continued COLD TEMPS EARLY FALL FREEZES may be a problem as tissues not acclimatized yet But NON-KILLING FROSTS actually can INCREASE RATE of acclimation “What doesn’t kill you - makes you strong!” WINTER reaches MAXIMUM HARDINESS (November - December) Plants can be DEACCLIMATIZED by WARM PERIODS If followed by LATE SPRING FROSTS (January – February – March) we can have TISSUE DAMAGE “INDIAN SPRINGS are far more DANGEROUS to plants than “INDIAN SUMMERS” as plants can QUICKLY DEACCLIMATIZE o MAXIMUM DEGREE of COLD HARDINESS DEPENDS on: GENETICS of the plant and the HABITAT and CLIMATE it originally ADAPTED to Example: TROPICAL plants, such as Freesias, can never reach cold hardiness to survive our CLIMATE. But plants that are nearby such as Oleander (California plant) can be BRED for cold hardiness GROWTH STAGE (already covered) FOOD STORED in the plant LOW RESERVES in the plant will LOWER COLD HARDINESS o Poor nutrition o Heavy foliage, flower, fruit production o Shortened growing period o Excessive forced growth from high N fertilization PHYSIOLOGY of ACCLIMATION o The FORMATION of ICE CRYSTALS in CELLS is what PHYSICALLY INJURES them Expansion of ICE bursts CYTOPLASMIC MEMBRANE and CELL DIES o Plant have a variety of WAYS to KEEP SAP from FREEZING CONVERSION of STARCH to SUGARS in CELL As temps cool INSOLUBLE STARCH is CONVERTED into SOLUBLE SUGARS ACTS like ANTIFREEZE – lets the sap get colder than freezing without freezing VISCOSITY or THICKNESS of SOLUTION in CELLS increases and LOWERS FREEZING POINT ICE CRYSTALS form in the INTERCELLULAR SPACES DEHYDRATES CELL - draws more water out of cell due to osmosis Makes content of cell MORE VISCOUS “SUPERCOOLING” sap Some plants have the ability to “SUPERCOOL” fluids below the freezing point without freezing their tissues Not known how this is done Example: one rhododendron was capable of maintaining a LIQUID CELL SOLUTION of - 40 degrees C WINTER INJURIES (cold stress) DESICCATION – DRYING out of TISSUES o TRANSPIRATION is less but EXCEEDS SOIL MOISTURE and dries out plant o PREVENTION: WATER when ground thawed MULCHING to retain moisture WINDBREAKS to decrease transpiration ANTI – DESICCANTS sprays reduce transpiration for a few days, good for transplanting FREEZE INJURY o SUDDEN DROP in TEMP or EXTREME TEMP CHANGE o PREVENTION: MULCH WHOLE plant SPRAYING ORCHARDS with WATER As water freezes HEAT is released, continually freezing water protects tissues @ 32 degrees F ROOT INJURY o FROST HEAVING FREEZING HEAVES plants out of ground DAMAGE to shallow ROOTED or CROWNED plants PREVENTION: MULCHING Better DRAINAGE ONCE HAPPENS - PRESS plants DOWN into ground o FREEZING of CONTAINER PLANTS PREVENTION: GROUP together HEAL into MULCH ICE DAMAGE o FREEZING RAIN in Gorge and E. Multnomah Co. o PREVENTION: STAKE or PROP small trees and shrubs Proper PRUNING and THINNING SLOW GROWING TREES BARK SPLITTING or FROST SPLITTING o SUDDEN FREEZE before the tree attains HARDINESS causes the BARK to SPLIT along the CAMBIUM LAYER o PREVENTION: NONE o ONCE HAPPENS – WRAP TRUNK or TACK BARK BACK to protect as much cambium and phloem tissue from drying out WINTER INJURY or WINTER SUNSCALD o TRUNK absorbs HEAT on a clear sunny day during the WINTER, which DEACCLIMATIZES BARK o Followed by a rapid DROP in nighttime TEMPS o Causes BARK to DIE BACK on S or SW side (also called S or SW injury) o PREVENTION: Protect by WRAPPING with burlap, tree guards, white paint Plant more RESISTANT, THICKER BARK SPECIES SUMMER INJURIES – Heat Stress SUMMER SUNSCALD o Too much HEAT and TRANSPIRATION LOSS for the plant to cool itself o LEAVES, FRUIT and BARK can be BURNED o PREVENTION: Adequate WATER in SOIL SPRAYING WATER on plant THICKER BARKED TREES THE ROOT ENVIRONMENT - WATER and SOILS SOILS Provides plants with PHYSICAL SUPPORT, WATER, NUTRIENTS and O2 SOIL PROFILE (show overhead / handout) o o o o o O Horizon – litter layer A Horizon – Topsoil – darker, higher OM B Horizon – Subsoil – lighter, lower OM C Horizon – Parent material R Horizon - Bedrock SOIL COMPOSITION – Ideal o SOIL TEXTURE – Mineral portion (Show overhead) PROPORTION or % of SAND, SILT, and CLAY in the SOIL SOIL TEXTURE difficult to CHANGE o ORGANIC MATTER (OM) – HUMUS Decaying plant and animal matter Break down of OM provides CO2, H2O, and NUTRIENTS for plant use Improves WATER holding capacity and NUTRIENT holding capacity You can always IMPROVE soils by adding OM o PORE SPACE – Ideally 50% of SOIL 25% WATER, 25% AIR SIZE of PORE SPACE and how they CONNECT determines how well WATER and AIR MOVES in soils and how ROOTS grow in it CONTRAST SANDY and CLAY soils SOIL ORGANISMS o Whole ECOSYSTEM full of SOIL ORGANISMS o MICRO – bacteria, fungi, algae, actinomycetes, protozoans o MACRO – nematodes, earthworms, arthropods, rodents o IMPORTANT for: Breakdown of OM NITROGEN CYCLE MYCORRHIZAL Associations MIXING, AERATING and DRAINAGE SOIL STRUCTURE o Few are harmful, MOST are BENEFICIAL SOIL STRUCTURE o ARRANGEMENT or grouping of soil particles into AGGREGATES or “CLUMPS” o PORE SPACE and SOIL STRUCTURE determine DRAINAGE, AERATION, and ROOT PENETRATION o SOIL STRUCTURE is CHANGEABLE MICROBES, HUMUS, and CLAY can cement soil particles together to make AGGREGATES Poor CULTURAL PRACTICES can DESTROY soil structure Example: tilling in wet soil PLANT NUTRITION (Show overhead) o 17 ESSENTIAL NUTRIENTS - used by ALL plants MAIN elements – from water and air C, H, O MACRO NUTRIENTS – used most by plants, nutrients in poor supply in the soil PRIMARY – N, P, K SECONDARY – Ca, Mg, S MICRO NUTRIENTS – Trace elements Used in small amounts B, Cu, Cl, Fe, Mn, Mo, Ni, Zn BENEFICIAL NUTRIENTS Used by only SOME plants Na, Si, Co o IN TERMS of SOILS: The PRESENCE of an NUTRIENT in the SOIL does not guarantee UPTAKE by ROOTS Ions ADSORB differently to SOIL Ions DISSOLVED differently in the SOIL SOLUTION ROOTS take in IONS SELECTIVELY CORRECTING a NUTRIENT DEFICIENCY in a PLANT is not always a matter of ADDING it to the SOIL This is why we LEARN about SOILS and TESTING SOILS o