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KETERSEDIAAN & SERAPAN HARA. Basic concepts of soil fertility. How plants absorb nutrients. movement to the root surface absorption into plant. Determining nutrient need. Essential plant nutrients. categories effect of soil characteristics. Liming. Sources of nutrients to plants.
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Basic concepts of soil fertility How plants absorb nutrients • movement to the root surface • absorption into plant Determining nutrient need Essential plant nutrients • categories • effect of soil characteristics Liming
Sources of nutrients to plants Soil solution - ionic form - low concentration - highly buffered Contributors to the soil solution - exchange sites on clay and organic matter - organic matter and microorganisms - soil rocks and minerals - atmosphere and precipitation - fertilizer and other additions
Movement of ions from soils to roots • Root interception • Mass flow • Diffusion
MASS FLOW – dissolved nutrients move to the root in soil water that is flowing towards the roots root tip Ca2+ NO3- NO3- Ca2+
DIFFUSION – nutrients move from higher concentration • in the bulk soil solution to lower concentration at the root; • In the time it takes NO3- to diffuse 1 cm, K+ diffuses 0.2 cm, • and H2PO4- diffuses 0.02 cm root tip NO3- NO3- NO3- NO3- NO3- NO3-
ROOT INTERCEPTION – roots obtain nutrients by physically contacting nutrients in soil solution or on soil surfaces; - roots contact ~1% of soil volume; - mycorrhizal infection of root increase root-soil contact root tip H2PO4- Mn2+ H2PO4- Zn2+ Zn2+ H2PO4- mycorrhizae
Ion absorption by plants: Passive uptake - diffusion - ion exchange Active ion uptake - ion carriers - selective / competitive
Overview Today I want to look at all aspects of plant nutrient uptake. This will cover the plants’ viewpoint, but also soil conditions and management. Topics to cover: The biology of nutrient uptake by roots The soil chemistry affecting this uptake.
Root uptake It has long been appreciated that roots in plants are like guts in animals – the site where nutrients are taken up. Because of this plant roots usually have an immense surface area caused by repeated divisions. Much of this area is due to root hairs, and it is these which are the main sites of entry into a plant for water and nutrients. Root hairs adhere tightly to soil particles, which is where soil water tends to be bound. Water enters through the epidermis of root hairs into the apoplast of the root (extra-cellular space). Here is is gradually taken up by cells and enters the symplast, from where it passes the casparian strips into the xylem vessels of the stele.
The flow of water into roots is controlled by a band of corky, water-impermeable cells lining the root cortex which force water to flow into the main vessels symplastically. This band of corky tissue (suberin + lignin) is the casparian strip, and is present in the endodermis of the root systems of most vascular plants. The casparian strip ensures that all water entering the stele of the root (thence up to the main stem) has passed through a plasma membrane so has been regulated by transport proteins. Casparian strip stele Cortex
Note that the tracheids and vessel elements of the xylem are dead and lack protoplasts, hence their lumen is apoplast, not symplast. Minerals and water enter the xylem proper by being actively pumped from the walls of the endodermal (and stele parenchymal) cells. This way the xylem contents have been filtered through the plasma membranes of many cells, and are highly purified (of bacteria, mineral debris etc).
The Supply and Availability of Plant Nutrients in Mineral Soils Factors Controlling the Growth of Higher Plants 1. Light 2. Mechanical Support 3. Heat 4. Air 5. Water 6. Nutrients
Principle of Limiting Factors • The factor which is least optimum will determine the level of crop production The Essential Elements • 16 - essential elements • Must be in farms usable by the plant • Optimum concentration for plant growth • Proper balance
Essential Elements Used in Relatively Large Amounts Mostly from Air and Water From Soil Solids Carbon Nitrogen Calcium Hydrogen Phosphorus Magnesium Oxygen Potassium Sulfur Essential Elements Used in Relatively Small Amounts From Soil Solids Iron Copper Manganese Zinc Boron Chlorine Molybdenum Essential Nutrients Elements and Their Sources
Transfer of Plant Nutrients to Available Forms Organic Nitrogen Ammonium Nitrite Nitrate (protein, amino acids) NH4+ NO2- NO3- Ca3(PO4) + 4H2O + 4CO2 Ca(H2PO4)2 + 2Ca(HCO3)2 Insoluble Phosphate Water Soluble Soluble Calcium (Tri Ca Phosphate) Phosphate Bicarbonate 2KAlSi3O8 + H2CO3 + H2O H4Al2Sl2O9 + K2CO3 + 4SlO2 Microcline Carbonic Hydrated Soluble feldspar Acid silicate carbonate 1. Taken up by plants 2. Leached 3. Adsorbed
Transfer of Plant Nutrients to Available Forms H Ca + 2H2CO3 + Ca(HCO3)2 H Sulfur Organic sulfur Sulfides Sulfites Sulfates Protein H2S SO3= SO4= Colloidal Surface Colloidal Surface
Forms of Elements Used by Plants Two general sources of readily available nutrients in the soil. 1. Nutrients adsorbed on the colloids -Ca NH4 - - Mg - K 2. Salt in the soil solution KCl K+ + Cl-
Essential element must be in the ionic form 1. Cationic- Positively charged ions 2. Anionic- Negatively charged ions
The more important ions present in the soil solution or on the soil colloids may be tabulated as follows ElementsSymbolForm Used by Plants Sulfur S SO3=, SO4= Carbon C++++ CO3=, HCO3-, CO2 Hydrogen H+ H2O Oxygen O= O2 Nitrogen N NH4+, NO2-, NO3- Phosphorus P+5 HPO4=, H2PO4 Potassium K+ K+ Calcium Ca++ Ca++ Magnesium Mg++ Mg++
Cont. ElementsSymbolForm Used by Plants Iron Fe Fe++, Fe+++ Molybdenum Mo+6 MoO4= Manganese Mn Mn++, Mn++++ Copper Cu Cu+, Cu++ Zinc Zn++ Zn++ Born B BO3= Chlorine Cl- Cl- Water H2O H+, OH- O2 and CO2 come from the soil air or the atmosphere
Inorganic Salts -Forms in which you buy fertilizer KCl K+ + Cl- NaNO3 Na+ + NO3- NH4NO3 NH4 + NO3-
Inorganic Salts -Forms in which you buy fertilizer KCl K+ + Cl- NaNO3 Na+ + NO3- NH4NO3 NH4 + NO3-
Other Elements K+, Ca++, Zn++, Mg++, Cl-, only one form present Fe, Mn and Cu - From depends on the oxidation reduction condition of the soil Fe+++ + e- Fe++ oxidation reduction ic ous
Other Elements Aerated soils Fe+++ (Ferric oxides) Mn++++ (Manganic oxide) Poor Drainage Fe++ (Ferrous oxides) Mn++ (Manganous oxide) Toxic
Micronutrients • Micronutrient elements • Iron (Fe) • Manganese (Mn) • Boron (B) • Zinc (Zn) • Molybdenum (Mo) Zinc (Zn) • Copper (Cu) • Chloride (Cl) • Usually supplied by irrigation water and soil • Deficiency and toxicity occur at pH extremes
Copper Manganese Nickel Iron Zinc Boron Chloride Molybdenum CationsAnions
Inputs Insoluble salts Plant uptake Micronutrients in solution Exchangeable cations Soil OM Losses
Recreational hydroponics • Home hydroponics systems
Transport in plants • Water and mineral nutrients must be absorbed by the roots and transported throughout the plant • Sugars must be transported from site of production, throughout the plant, and stored
Transport and water potential • Water potential (Ψ) of a cell: Ψcell = Ψp + Ψπ + Ψm p = pressure potential π = solute potential m = matrix potential
Ψp - Pressure potential (turgor) Low Ψp High Ψp
Ψπ- Solute potential • Pure water Ψπ = 0 • All solutions, Ψπ < 0 • As solute concentration increases, Ψcell …
Water movement in plants • Movement from high Ψcell to low Ψcell • Occurs in the xylem Early thoughts on water transport • Capillary action
higher ψ higher ψ Transpiration creates tension lower ψ lower ψ cohesion lower ψ higher ψ highest ψ Tension-cohesion theory • Water is drawn up the plant by transpiration of water from stomata higher ψ low ψ
Importance of stomata • Regulate transpiration rate • Controls rate of water uptake • Water required for photosynthesis • Water required to maintain turgor pressure • Controls nutrient uptake • Regulate gas exchange • CO2 required for photosynthesis
Ψ and transpiration rate • In terms of ψ, can you explain how transpiration rate is influenced by: • Atmospheric humidity? • Wind? • Air temperature? • Light intensity?
Transpiration and photosynthesis • The dilemma of a hot, sunny day? Good for photosynthesis, but… Bad for water loss
1M 10-50mM Phloem transport • Pressure-flow hypothesis