Physical Features of inland Water Environment.pdf

Physical Features of inland Water Environment

1. Md. EftekharulAlam
(Emon)
Roll: 19103413
Session: 2018-19
Department of
Environmental Science
and Engineering

2. Introduction
❑Inland Water: Water of the interior that does not border upon marginal or high seas or is
above the rise and fall of the tides. The study of inland water is also known as Limnology.
Rivers, streams, reservoir, wetlands, lakes( both freshwater and saline), and groundwater.
❑Freshwater Environment:
►Pond
►Swamp
►River
►Lake
►Marsh
►Bog
►Fen

3. Physical Characteristics
❑Characteristicswould differ depending on the type of the water body
❑Physical properties of water in any aquatic system are largely regulated by the existing
meteorological conditions and chemical properties.
❑The study of Freshwater ecology are divided into two groups:
►Lenticsystemsare diverse, ranging from a small, temporary rainwater pool a few
inches deep to Lake.
►Loticis nothing but the running water series are included all forms of inland waters in
which the entire water moves continuously in a definite direction.

4. Density, Viscosity and Surface Film
❑Density: Density of water varies inversely proportional to temperature. Water is most dense
at 4°C and become less dense as its above and below. Salts dissolved in water directly
increased its density. Density of most inland water bodies in much less than that of the
ocean.
❑Viscosity: Viscosity of water increases as densityincreases. It doubles as temperature
decreases from 25°C to 0°C. It effects on movements of microscopic plants, animals, and
sinking of particles in lakes
❑Surface Film: When water is exposed to air, it acts like an extremely thin elastic, surface
membrane. This is also known as Surface Film. Surface tension is maximum in pure water
than in any other liquid except mercury. Surface film provides support for organisms

5. Surface Tension, Surface Radiation, Turbidity
❑Surface Tension : Surface tension is responsible for the ability of some solid objects to float
on the surface of a liquid. As temperature increases, molecules of water become more
active and they move more rapidly; therefore, the intermolecular forces are more
instable. Surface tension decreases with increasing temperature.
❑Surface Radiation : Solar radiation heats the surface layers of water in lakes, reservoirs, and
ponds more quickly than it warms deeper water. Water bodies often experience thermal
stratification in which warmer, lighter water of the surface layer does mix with cooler,
heavier deeper water
❑Turbidity : Suspended material in water produces turbidity and reduces light penetration.
Turbidity when caused by clay and silt particles in often important as a limiting factor
and it is diversely proportional to the photosynthesis of aquatic phytoplankton and
submerged macrophysics, not only retards the photosynthetic rate but clogs the gill
systems of lamellibranches thereby increasing the rate of mortality

6. Effect of Light on Organisms
❑Lightplays an important role in lake ecology and determines the potential rate of
photosynthesis
❑The daily alternation of light and darkness establishes a rhythm in the activities of
many aquatic organisms. Light is essential for photosynthesis. Some fish require light to
feed
❑Many organisms orient to light and some are sensitive to UV light. Small, soft bodied
bottom dwelling organisms are particularly sensitive to light. It is thought the evolution of
pigmentation, chitinous exoskeleton, shells, cases and similar other structure have helped
certain photo sensitive species to survive in shallow, well lighted area

7. Effect of Temperature on Organisms
❑Temperaturechanges produce characteristic patterns of circulation which greatly
influence the aquatic life.
❑Temperaturevariation in a fresh water habitat is smaller and the changes takes place very
slowly this is due to unique thermal properties of water i.e.
❑During the hot months of summer, the organism from the top layer migrate to the lower
layers to avoid high temperature of epilimnion. With the onset of winter, as the surface
water cool below the 4°C, it expands and become lighter, remain on the surface and
freezes. Immediately below the ice, the temperature of water is very close to 0°C but
further below of one / two meters it usually raises rapidly to 4°C.

8. Thermal Stratification
❑In tropical lake, heat intake at the surface to the formation of a vertical temperature
gradient within which the thermal resistance become too great for the existing winds to
continue mixing the whole water masses. The upper warmer layer is called epilimnion and
the lower cooler layer is called hypolimnion. In between the two distinct portions, a layer
called thermocline

9. Thermal Circulation
❑The inland water layers undergoes
stratification in the summer and
complete overturn in the autumn
and spring. During winter, surface
ice prevents further mixing by the
wind. Small differences in density
and temperature exist, with cooler
water (0 °C [32 °F]) staying near the
surface and warmer, denser water
(4 °C [39.2 °F]) extending to the
bottom.

10. THE END