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Uptake and Movement of Water and Solutes. Water enters the plant through osmosis, ... Soil bacteria called nitrifiers oxidize NH3 to nitrite (NO2 ) and nitrate ions ... – PowerPoint PPT presentation

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Title: Table of Contents


1
Uptake and Movement of Water and Solutes
  • Water enters the plant through osmosis, but the
    uptake of minerals requires transport proteins
  • Why does water move into the root from the soil?
  • Moves into due to water potential difference.

2
Figure 36.1 The Pathways of Water and Solutes in
the Plant
3
Uptake and Movement of Water and Solutes
  • The force exerted by the rigid cell wall as water
    enters is called the pressure potential, or
    turgor pressure.
  • Water enters a plant cell until the pressure
    potential exactly balances the solute potential.
    The cell is then called turgid.
  • Keeps plant cells firm and plants dont wilt.

4
Uptake and Movement of Water and Solutes
  • Mineral ions generally require transport proteins
    in order to cross membranes.
  • Can be passive or active.
  • Proton pump helps get ions in by facilitated
    diffusion.

5
Transport of Water and Minerals in the Xylem
  • In the xylem, water and minerals constitute the
    xylem sap.
  • What causes the xylem sap to move upward?
  • transpirationcohesiontension

6
Transport of Water and Minerals in the Xylem
  • The transpirationcohesiontension mechanism
  • The concentration of water vapor is higher inside
    the leaf than outside, so water diffuses out of
    the leaf through the stomata. This process is
    called transpiration.
  • This creates a tension that draws water from the
    xylem.
  • The removal of water from the veins, in turn,
    establishes tension on the entire volume of water
    in the xylem, so the column is drawn up from the
    roots.

7
Figure 36.8 The TranspirationCohesionTension
Mechanism
8
Transport of Water and Minerals in the Xylem
  • Mineral ions in the xylem sap rise passively with
    the solution.
  • Transpiration also contributes to the plants
    temperature regulation, cooling plants in hot
    environments.

9
Transpiration and the Stomata
  • Guard cells control the opening and closing of
    the stomata.
  • Most plants open their stomata only when the
    light is intense enough to maintain
    photosynthesis.
  • Stomata also close if too much water is being
    lost.

10
Figure 36.11 Stomata (Part 1)
11
Transpiration and the Stomata
  • Opening closing and of the stomata are regulated
    by controlling K concentrations in the guard
    cells.
  • Light activates a proton pump gt K moves inside.
  • Water moves inside to lower water potential.
  • Guard cells open due to shape change.

12
Translocation of Substances in the Phloem
  • Sugars, amino acids, some minerals, and other
    solutes are transported in phloem and move from
    sources to sinks.
  • Transport often proceeds in both directions both
    up and down the stem simultaneously.

13
Translocation of Substances in the Phloem
  • Sieve tube cells at the source have a greater
    sucrose concentration that surrounding cells, so
    water enters by osmosis. This causes greater
    pressure potential at the source, so that the sap
    moves by bulk flow towards the sink.
  • At the sink, sucrose is unloaded by active
    transport, maintaining the solute and water
    potential gradients.
  • This is called the pressure flow model.

14
Figure 36.14 The Pressure Flow Model
15
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16
The Acquisition of Nutrients
  • Plants are sessile organisms. Nutrients and
    energy must be brought to them in some way.
  • A plant can extend itself by growing. The roots
    obtain most of the mineral nutrients needed.
  • The essential elements for plants were identified
    by growing plants hydroponically, or without
    soil.

17
Table 37.1 Mineral Elements Required by Plants
(Part 1)
18
Table 37.1 Mineral Elements Required by Plants
(Part 2)
19
Soils and Plants
  • Soils are complex mixtures of living and
    nonliving components, including bacteria, fungi,
    earthworms and other animals, particles of rock,
    clay, water, dissolved minerals, air spaces, and
    dead organic matter.
  • The type of soil in a given area depends on the
    type of rock from which it forms and how it is
    broken down.
  • Rocks are broken down by mechanical weathering,
    or physical breakdown and chemical weathering.

20
Soils and Plants
  • The availability of nutrient ions is influenced
    by soil pH. pH 6.5 is optimal for most crops.
  • In the process of liming, compounds such as
    calcium carbonate, calcium hydroxide, or
    magnesium carbonate are added to acidic soil to
    raise the pH.
  • The pH of soil can be lowered by adding sulfur,
    which soil bacteria convert to sulfuric acid.

21
Nitrogen Fixation
  • Most nitrogen fixation is done by bacteria.
  • Cyanobacteria are the principle nitrogen fixers
    in aquatic ecosystems.
  • Some nitrogen fixers live in close association
    with plant roots in a mutualistic relationship.
  • Rhizobium fix nitrogen only in close association
    with the roots of legumes.
  • These bacteria infect plant roots, causing the
    roots to develop nodules

22
Figure 37.5 Root Nodules
23
Nitrogen Fixation
  • Three things are required for fixation
  • A strong reducing agent to transfer the hydrogen
    atoms to N2.
  • Energy, supplied by ATP.
  • The enzyme nitrogenase.
  • Nitrogenase is strongly inhibited by O2.
  • Many nitrogen fixers are anaerobes. But others,
    such as Rhizobium, are not.

24
Nitrogen Fixation
  • Another type of symbiosis in which plants depend
    on another organism for their nutrition is that
    of mycorrhizae, the root-fungus association.

25
Nitrogen Fixation
  • The nitrogen cycle includes the process of
    nitrogen fixation, nitrification, nitrate
    reduction, and denitrification.
  • Soil bacteria called nitrifiers oxidize NH3 to
    nitrite (NO2) and nitrate ions (NO3) in a
    process called nitrification.

26
Nitrogen Fixation
  • Nitrate reduction is carried out by plants using
    their own enzymes, and reduces nitrate back to
    ammonia. The ammonia is used to produce amino
    acids.
  • Animals can not reduce nitrate, and depend on
    plants for reduced nitrogen compounds.
  • Bacteria called denitrifiers return the nitrogen
    from animal wastes and dead organisms back to N2
    gas in a process called denitrification.

27
Figure 37.8 The Nitrogen Cycle
28
Carnivorous and Heterotrophic Plants
  • Some plants that grow in acidic, nitrogen-poor
    environments trap and digest insects to help
    augment nitrogen and phosphorus supplies.
  • These carnivorous plants include sundews, Venus
    flytraps, and pitcher plants.
  • These plants have adaptations to capture small
    animals and digest the proteins.
  • Carnivorous plants can survive without feeding on
    insects, but they grow much faster in their
    natural habitats when they succeed in capturing
    insects.

29
Figure 37.9 Carnivorous Plants
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