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Abiotic factors of Grasslands

   Each abiotic component influences the number
    and variety of plants that grow in an ecosystem,
    which in turn has an influence on the variety of
    animals that live there. The four major abiotic
    components are: climate, parent material and
    soil, topography, and natural disturbances.
1) Climate

 includes the rainfall, temperature and wind
  patterns that occur in an area, and is the most
  important abiotic component of a grassland
  ecosystem.
 The climate in our grassland ecosystems is
  usually hot and dry in the spring and summer
  growing season, and cool or cold in winter
  dormant season.
Temperature, in tandem with Precipitation
   The amount and distribution of the rainfall an area
    receives in a year influences the types and
    productivity of grassland plants

Temperature
 Grasslands     occur in both high-temperature
    areas near the Equator and mid-to-low-
    temperature areas nearing subarctic regions.
    Grasslands that are near the Equator are
    generally either tropical grasslands or
    temperate. Grasslands that are further from the
    Equator are mostly temperate grasslands and
    montane grasslands.
Precipitation

   Tropical grasslands receive the most rain out of all
    the grassland biomes, up to 60 inches a year.
    Temperate grasslands receive much less annual
    rainfall on average (no more than 40 inches a
    year). Flooded grasslands, though they are very
    wet, also receive less annual rainfall than tropical
    grasslands, around 30 to 40 inches per year.
    Montane grasslands receive the lowest amount of
    precipitation, no more than 30 inches per
    year, and often, that precipitation is in the form of
    snow.
Humidity

 Tropical grasslands and flooded grasslands are
  very humid, meaning there is a very high
  percentage of moisture in the air. Temperate
  grasslands are somewhat humid, but can also be
  arid, meaning dry or little moisture in the air.
  Montane grasslands are typically very arid;
  however, some are mildly humid.
 During the hottest months of the year (the height
  of summer) more water evaporates from parts of
  the grasslands than falls as rain, creating
  a moisture deficit.
2.) Parent Material and Soil
Parent Material

   Much of the parent material underlying BC's
    grasslands was deposited as the last ice sheets
    melted away. In the Rocky Mountain Trench, for
    example, some material was deposited under a
    moving glacier, while on the Chilcotin plateau
    some was deposited under a stationary ice sheet;
    in many places throughout the grasslands material
    was carried and deposited by water on, in, or
    under the ice.
Soil
   The type of parent material in a particular area
    influences the texture of the soil, how well water flows
    through it, and hence the chemistry and nutrients of
    the soil.

   The fine silt soils found on the terraces of the
    Okanogan, Kootenay and Thompson valleys hold
    water near to the surface where it either evaporates
    or is soaked up by the dense fine roots of grasses;
    trees are not common in these areas. By contrast, in
    areas with gravel soils water moves quickly down to
    depths below the grass roots to levels where tree
    roots grow. As such, more trees are likely to be found
    in these areas.
glacial till (C) deposited
by the ice as it melted
12,000 to 10,000 years
ago. These soils have
a deep organic-rich
layer (A) that results
from the breakdown of
the roots and plant
material each year.
The organic layer
increases in depth with
increases in elevation
and moisture.
3.) Topography

   They generally occur in very hilly, uneven
    landscapes. Temperate grasslands are usually
    more flat and occur in areas of mid-to-low
    elevation. Flooded grasslands are almost all flat
    and in areas of low elevation. Montane grasslands
    are very mountainous and usually in areas of high
    elevation.
Aspect
 refers to the direction in which a piece of land is
  facing.
slope
 is the angle at which the land lies. Slope is
  important in our grasslands as water may run
  downhill rather than soak into the ground where it
  is available for plants
Elevation
 describes the height of land above sea level.
  Temperatures are generally cooler and rainfall is
  higher as elevation is gained.
4.) Natural Disturbances


   change grasslands in many ways, adding to the
    diversity of these ecosystems. Some types of
    disturbance, such as annual flooding of riparian
    areas along rivers and streams, can be predicted
    while others, such as a fire after a lightning
    storm, happen unexpectedly.
Flooding
   The flooding waters can alter stream and river
    banks and move soil, broken trees and shrubs
    downstream.

Lightning Storms
   Since grassland plants burn readily, fire spreads
    very quickly, and is thought to have been an
    important factor in maintaining the grasslands
    ecosystem. Fires are important for returning
    nutrients to the soil.
Biotic factors of Grasslands

   The biotic factors of the grassland ecosystem
    includes the autotrophs, and the heterotrophs, that
    is the producers, primary consumers, secondary
    consumers and the tertiary consumers.

   Primary producers: The primary producers
    include the autotrophs that can photosynthesize
    and includes the grasses, sedged, rushes,
    cyanobacteria. lichens, mosses, trees etc.
   The primary and the secondary consumers
    includes the rabbits, moles , hares, elks,
    small dears in some places along with the
    phytophagous insects , snakes, preying
    birds, insect feeders and in some
    grassland ecosystems like in Africa where
    there are carnivores like the panthers. lions,
    foxes, wild dogs, etc
     The bacteria , fungi and other micro-
    organisms form the detritus food chain that
    is involved in the nutrient cycling of the
    grassland.

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Eudece grasslands

  • 1.
  • 2. Abiotic factors of Grasslands  Each abiotic component influences the number and variety of plants that grow in an ecosystem, which in turn has an influence on the variety of animals that live there. The four major abiotic components are: climate, parent material and soil, topography, and natural disturbances.
  • 3. 1) Climate  includes the rainfall, temperature and wind patterns that occur in an area, and is the most important abiotic component of a grassland ecosystem.  The climate in our grassland ecosystems is usually hot and dry in the spring and summer growing season, and cool or cold in winter dormant season.
  • 4. Temperature, in tandem with Precipitation  The amount and distribution of the rainfall an area receives in a year influences the types and productivity of grassland plants Temperature  Grasslands occur in both high-temperature areas near the Equator and mid-to-low- temperature areas nearing subarctic regions. Grasslands that are near the Equator are generally either tropical grasslands or temperate. Grasslands that are further from the Equator are mostly temperate grasslands and montane grasslands.
  • 5.
  • 6. Precipitation  Tropical grasslands receive the most rain out of all the grassland biomes, up to 60 inches a year. Temperate grasslands receive much less annual rainfall on average (no more than 40 inches a year). Flooded grasslands, though they are very wet, also receive less annual rainfall than tropical grasslands, around 30 to 40 inches per year. Montane grasslands receive the lowest amount of precipitation, no more than 30 inches per year, and often, that precipitation is in the form of snow.
  • 7. Humidity  Tropical grasslands and flooded grasslands are very humid, meaning there is a very high percentage of moisture in the air. Temperate grasslands are somewhat humid, but can also be arid, meaning dry or little moisture in the air. Montane grasslands are typically very arid; however, some are mildly humid.  During the hottest months of the year (the height of summer) more water evaporates from parts of the grasslands than falls as rain, creating a moisture deficit.
  • 8.
  • 9. 2.) Parent Material and Soil Parent Material  Much of the parent material underlying BC's grasslands was deposited as the last ice sheets melted away. In the Rocky Mountain Trench, for example, some material was deposited under a moving glacier, while on the Chilcotin plateau some was deposited under a stationary ice sheet; in many places throughout the grasslands material was carried and deposited by water on, in, or under the ice.
  • 10.
  • 11.
  • 12. Soil  The type of parent material in a particular area influences the texture of the soil, how well water flows through it, and hence the chemistry and nutrients of the soil.  The fine silt soils found on the terraces of the Okanogan, Kootenay and Thompson valleys hold water near to the surface where it either evaporates or is soaked up by the dense fine roots of grasses; trees are not common in these areas. By contrast, in areas with gravel soils water moves quickly down to depths below the grass roots to levels where tree roots grow. As such, more trees are likely to be found in these areas.
  • 13. glacial till (C) deposited by the ice as it melted 12,000 to 10,000 years ago. These soils have a deep organic-rich layer (A) that results from the breakdown of the roots and plant material each year. The organic layer increases in depth with increases in elevation and moisture.
  • 14. 3.) Topography  They generally occur in very hilly, uneven landscapes. Temperate grasslands are usually more flat and occur in areas of mid-to-low elevation. Flooded grasslands are almost all flat and in areas of low elevation. Montane grasslands are very mountainous and usually in areas of high elevation.
  • 15. Aspect  refers to the direction in which a piece of land is facing. slope  is the angle at which the land lies. Slope is important in our grasslands as water may run downhill rather than soak into the ground where it is available for plants Elevation  describes the height of land above sea level. Temperatures are generally cooler and rainfall is higher as elevation is gained.
  • 16. 4.) Natural Disturbances  change grasslands in many ways, adding to the diversity of these ecosystems. Some types of disturbance, such as annual flooding of riparian areas along rivers and streams, can be predicted while others, such as a fire after a lightning storm, happen unexpectedly.
  • 17. Flooding  The flooding waters can alter stream and river banks and move soil, broken trees and shrubs downstream. Lightning Storms  Since grassland plants burn readily, fire spreads very quickly, and is thought to have been an important factor in maintaining the grasslands ecosystem. Fires are important for returning nutrients to the soil.
  • 18. Biotic factors of Grasslands  The biotic factors of the grassland ecosystem includes the autotrophs, and the heterotrophs, that is the producers, primary consumers, secondary consumers and the tertiary consumers.  Primary producers: The primary producers include the autotrophs that can photosynthesize and includes the grasses, sedged, rushes, cyanobacteria. lichens, mosses, trees etc.
  • 19. The primary and the secondary consumers includes the rabbits, moles , hares, elks, small dears in some places along with the phytophagous insects , snakes, preying birds, insect feeders and in some grassland ecosystems like in Africa where there are carnivores like the panthers. lions, foxes, wild dogs, etc The bacteria , fungi and other micro- organisms form the detritus food chain that is involved in the nutrient cycling of the grassland.