Categorieën: Alle - atmosphere - environment - spores - adaptation

door roslina mustapha 11 jaren geleden

252

ATMOSPHERIC HABITAT

Airborne particle dispersal in atmospheric habitats involves several processes such as rainwashing, electrostatic deposition, and impaction. These particles, including spores, viruses, and bacteria, exhibit differing levels of adaptation to airborne environments.

ATMOSPHERIC HABITAT

ATMOSPHERIC HABITAT

Dispersal of airborne particles

Deposition
methods

Rainwashing

Electrostatic deposition

Brownian movement

impaction with surfaces

sedimation due to gravity

Dispersion
depend on physical characteristics of particles

environment

convection

air humidity

turbulence

wind movement

spores

density

degree of surface roughness

shape

size

Liberation & take off into the air
features

fungi have many adaptation

virus&bacteria are poorly adapted

requires energy to overcome adhesive forces

Atmospheric habitat

spores (better adapted)
endospores

primarily adapted to resistance other than reproduction

limited to gram +ve bacteria

xenosphores

adaptation for survival & fecundity

primarily adapted to reproduction vs. resistance to environment

bacteria

protozoans

algae

fungi

small size & low density
produced in high numbers
low metabolic rates
Dispersal vs. growth
lower atmosphere can theoritically support growth cause

light intensity within appropriate limits

clouds---sufficient water

other extreme environment

Antartica
Environmental conditions

high radiation

high velocity of desiccating winds

low humidity

low temperature

Salt lakes
high concentration of sodium chloride

precipitation of intracellular proteins

dehydration

Hot springs
grow of m/os limited by

low concentration of dissolved oxygen

low concentration of organic matter

high acidity/alkalinity

high temperature

at volcanic areas

Physical features of aerial environment

precipitation
9 days average of water vapour in air
water vapour--- continually recycled
radiation
mostly absorbed or reflected back
from the sun
air movement in troposhere
principle

displacement of air occur

sun heats up the ground, create gradient

temperature decreases with altitude

main agent of dipersal

Regions in Atmosphere

Lonosphere
extreme UV and ionizing radiation levels
extreme low temperature
Exosphere
Helium and H2 predominant
extending into outer space
Thermosphere
Temperature increases with altitude
Mesosphere
temperature decreasing with height
stratosphere
extreme low temperatures
increasing temperature with height
location of good enzyme
Trophosphere
location of the bad ozone
most highly populated area
nearest to Earth