roots and soils
DESCRIPTION
Roots and Soils. Chapter 5. Outline. Function of Roots Root Development Root Structure Specialized Roots Mycorrhizae Root Nodules Human Relevance of Roots Soils. Function of Roots. Anchor plants into soil Absorption of water and minerals Store food or water - PowerPoint PPT PresentationTRANSCRIPT
Roots and Soils
Chapter 5
Outline
Function of Roots
Root Development
Root Structure
Specialized Roots
Mycorrhizae
Root Nodules
Human Relevance of Roots
Soils
Function of Roots
Anchor plants into soil
Absorption of water and minerals
Store food or water
Other specialized functions
Root Development
Upon germination, embryo’s radicle grows out and develops into first root• May develop into thick
taproot with thinner branch roots
− Dicotyledonous plants (dicots)
Taproot system
Root Development
Or, after radicle formation, adventitious roots develop into fibrous root system• Adventitious Roots -
develop from stem or leaf• Fibrous Roots - large
number of fine roots of similar diameter
• Monocotyledonous plants (monocots) and some dicots
Fibrous root system
Root Structure 4 regions: • Root cap
• Region of cell division
• Region of cell elongation
• Region of maturation
Longitudinal section through root tip
Root Structure• Root Cap - thimble-
shaped mass of parenchyma cells covering each root tip
− Protects tissues from damage as root grows
o Secretes mucilage that acts as lubricant
o Functions in gravitropism (gravity perception)
Longitudinal section through root tip
Root Structure
• Region of Cell Division - composed of apical meristem in center of root tip– Subdivided into 3
meristematic areas:o Protoderm - gives rise to
epidermiso Ground meristem - gives
rise to cortex and pitho Procambium - gives rise
to 1° xylem and 1° phloem
Root tip showing primary meristems
Root Structure
• Region of Elongation - cells become several times original length– Vacuoles merge
• Region of Maturation - cells differentiate into various distinctive cell types– Root hairs
Root hair zone of radish seedling
Root Structure
• Root Hairs– Epidermal cell
extensions with thin cuticle
– Absorb water and minerals
– Adhere tightly to soil particles
– Increase total absorptive surface of root
Root hair zone of radish seedling
Root StructureRegion of Maturation
Cortex - parenchyma cells between epidermis and vascular cylinder• Mostly stores food
Cross section of dicot root
Root StructureRegion of Maturation
Endodermis - inner boundary of cortex, consisting of single-layered cylinder of compact cells• Cell walls with suberin bands called casparian strips
on radial and tangential walls– Forces water and dissolved substances entering and
leaving central core to pass through endodermis– Regulates types of minerals absorbed– Eventually inner cell walls become thickened with
suberin, except for passage cells
Root StructureRegion of Maturation
Enlargement of vascular cylinder of dicot root
Root StructureRegion of Maturation
Vascular Cylinder - core of tissues inside endodermis• Pericycle - outer boundary of vascular cylinder
– Continues to divide, even after mature
– Forms lateral (branch) roots and part of vascular cambium
Region of endodermis and pericycle in dicot root
Lateral root formation
Root StructureRegion of Maturation
Most cells of vascular cylinder 1° xylem or 1° phloem• In dicot or conifer roots - solid core of xylem, with
“arms” in cross section• In monocots - xylem
surrounds pith• Phloem in patches
between xylem arms• Vascular cambium forms 2°
phloem to outside and 2° xylem to inside
Vascular cylinder of dicot root
Root Structure Growth• Determinate Growth - growth that stops after
organ fully expanded or after plant has reached certain size
• Indeterminate Growth - new tissues added indefinitely, season after season
Specialized Roots
Food Storage Roots• Starch and other
carbohydrates• Sweet Potatoes
Water Storage Roots• Pumpkin family, especially
in arid regions
Propagative Roots• Adventitious buds on roots - develop into suckers
(aerial stems)• Fruit trees
Manroot, water storage root
Specialized Roots
Pneumatophores• Plants with roots
growing in water
• Spongy roots that extend above water’s surface and enhance gas exchange between atmosphere and subsurface roots
Mangrove pneumatophores
Specialized Roots
Aerial Roots• Orchids - velamen
roots, with epidermis several layers thick to reduce water loss
• Corn - prop roots support plants in high wind
• Ivies (English ivy, Virginia creeper) - aerial roots aid plants in climbing Orchid aerial (velamen) roots
Specialized Roots
Contractile Roots• Pull plant deeper into
soil− Lily bulbs, dandelions
Buttress Roots• Stability in shallow soil
− Tropical Trees
Parasitic Roots • No chlorophyll and dependent on chlorophyll-
bearing plants for nutrition
Buttress roots of tropical fig tree
Mycorrhizae
Mycorrhizae - fungi that form mutualistic association with plant roots• Mutualistic association: Both fungus and root benefit
and dependent upon association for normal development
− Fungi facilitate absorption of water and nutrients, especially phosphorus for roots
− Plant furnishes sugars and amino acids to fungus• Particularly susceptible to acid rain
Mycorrhizae
Root Nodules
A few species of bacteria produce enzymes that can convert nitrogen from atmosphere into nitrates and other nitrogenous substances readily absorbed by roots• Root nodules contain large
numbers of nitrogen-fixing bacteria
• Legume Family (Fabaceae)Root nodules on roots
Soils Soils divided into horizons: • Topsoil
− A Horizon - dark loam, more organic material than lower layers
− E Horizon - light loam• B Horizon - subsoil
− More clay, lighter in color
• C Horizon - parent material
Soil profile
SoilsParent Material
Parent Material - rock not broken down into smaller particles• Rock types:
− Igneous – volcanic
− Sedimentary - deposited by glaciers, water or wind
− Metamorphic - changes in igneous or sedimentary rocks from pressure or heat
SoilsClimate
Climate varies throughout globe, as does its role in weathering of rocks• Deserts - little weathering by rain, and soils poorly
developed
• Areas of moderate rainfall - well-developed soils
• Areas of high rainfall - excessive water flow through soil leaches out important minerals.
SoilsLiving Organisms and Organic Composition
Many kinds of organisms, roots and other plant parts in soil• Bacteria and fungi decompose organic material from
dead leaves, plants and animals• Roots and other living organisms produce carbon
dioxide, which combines with water and forms acid increasing rate at which minerals dissolve
• Small animals alter soil by activities and wastes• Humus - partially decomposed organic matter, gives
soil dark color
SoilsTopography
Topography - surface features• Steep areas:
− Soil may erode via wind, water or ice
• Flat, poorly drained areas:− Pools and ponds may appear− Development of soil arrested
• Ideal topography permits drainage without erosion
SoilsSoil Texture and Mineral Composition
Soil Texture - relative proportion of sand, silt and clay in soil• Sand - many small particles bound together chemically• Silt - particles too small to be seen without microscope• Clay - only seen with electron microscope
− Individual clay particles - micelleso Negatively charged and attract, exchange or
retain positively charged ions, such as Mg++ and K+
Soils
Best agricultural soils - loams composed of 40% silt, 40% sand and 20% clay• Coarse soils drain water too quickly• Clay soils allow little water to pass
Soil Structure - arrangement of soil particles into aggregates• Productive agricultural soils - granular with pore
spaces occupying between 40-60% of total soil volume
− Particle size more important than total volume
SoilsWater in the Soil
Hygroscopic Water - physically bound to soil particles and unavailable to plants
Gravitational Water - drains out of pore spaces after rain
Capillary Water - water held against force of gravity in soil pores• Determined by structure and organic matter, by
density and type of vegetation, and by location of underground water tables
• Plants mostly dependent upon this type
SoilsWater in the Soil
Field Capacity - water remaining in soil after water drains away by gravity• Determined by texture, structure and organic content of
soil
Permanent Wilting Point - rate of water absorption insufficient for plant needs• Plant permanently wilts
Available Water - soil water between field capacity and permanent wilting point
SoilsSoil pH
Affects nutrient availability
Alkalinity causes some minerals, such as copper, iron and manganese to become less available• Counteract by adding sulfur, which is converted to sulfuric
acid by bacteria, or by adding nitrogenous fertilizers
Acidity inhibits growth of nitrogen-fixing bacteria• Counteract by adding calcium or magnesium compounds
= liming
Review
Function of Roots
Root Development
Root Structure
Specialized Roots
Mycorrhizae
Root Nodules
Human Relevance of Roots
Soils