Wednesday, August 25, 2010

Plants in the Desert


1) Saguaro

















-The saguaro grows on the northern and southern slopes of the Sonoran Desert.
-It grows in gravel and rocky soils, usually between he heights of 610 to 1068 meters.

-extracts water from its environment every chance it gets

-Its roots are 2.5 centimeters deep in the soil, so it can soak up as much rain and dew before it evaporates. A giant saguaro can soak up to a ton of water during a heavy rain.

-has a spongy inside layer that helps distribute water in the plant. Its outside skin is pleated, so

when more water is absorbed its outside can expend to make room.

-Growth is very slow (can take thirty years or more before the saguaro can reach 1.5 meters high. After eighty years pass, the plant can be 6 meters tall and still not be full-grown. Two centuries may pass before the plant reaches its mature height)

-By growing slowly, the saguaro expends less energy, food, and water, making it fully adapted to the desert.

2) Living stones (Lithops)
-most of the plant’s leaf surface below the ground
-It is cooler; there is less exposure to drying winds, and less chance of being spotted by a grazing animal.
-Gas exchange occurs underground. The stomata open without any exposure to wind or sun, so water loss is minimized during this process.

-limited amount of leaf surface area exposed to the sun for photosynthesis to supply food for the plant.

-The clear tips of the leaves have a crude optical system that permits light striking the windows to be diffused by crystals of calcium oxalate onto the green photosynthetic area below

-seed capsules will not open to disperse their long-lived seeds until they experience rainfall or heavy dew

3) Joshua Tree
- grows in dry soils on plains, slopes and groves
-small knife like leaves that have a very small surface area
-has a waxy resin that prevents much water from evaporating
-
night flying Yucca moth helps pollination


References:
http://www.desertusa.com/jtree/jt_o2.jpg

Tuesday, August 24, 2010

How do desert plants survive?


Desert plants have adapted to the extreme conditions to survive in several ways.

Plants that have adapted by altering their physical structure are called xerophytes (such as cacti, usually have special means of storing and conserving water. They often have few or no leaves, which reduces transpiration.). Phreatophytes are plants that have adapted to arid environments by growing extremely long roots, allowing them to acquire moisture at or near the water table. Perennials are plants that live for several years and annuals are plants that live for only a season.

Plants need to conserve moisture and energy in the dry desert. Many plants slow down growth for half of the year to conserve moisture. Many others also lose their leaves when temperatures become too intense. When the short rain season comes, plants burst into color, sprouting leaves and flowers.

Water conservation is very important for all plants in the desert. Many plants achieve this by losing their leaves in one fashion or another. Some plants shed their leaves during long bouts of dryness. Shedding leaves not only prevents the loss of moisture from evaporation, but also slows the growth of the plant. Slowing growth helps plants use less water, food, and energy during hot seasons.

A large number of desert plants begin as seeds. Seeds can survive without water for indefinite periods of time. Seeds only begin to sprout when the rain washes away anti-sprouting chemicals on their shells. After the rains, the seeds will sprout when the temperatures become more moderate. After these plants sprout they may not live very long, because many desert plants sprout, mature, flower, and then die in a very short period of time.

Other plants have thin, knife-like leaves that prevent water loss by giving the sun a smaller area to evaporate water. Others, like the Joshua tree, have needle-like leaves with a waxy resin that prevents much water from evaporating. Another type of plant, called living stones, exposes only a few of its leaves to the sun. The rest of the plant remains underground, safe from the sun and heat. Other plants remain hydrated with their deep roots. The mesquite tree has roots that can extend 30.5 meters into the ground, tapping water from underground aquifers.

Many plants in the desert are located many feet meters away from one another. One reason may be that moisture is limited so plants must space out. Another concept is that some plants are poisonous to others. Roots of the creosote bush have chemicals on them just for the purpose of keeping other plants out of their way.

One problem to plants living in or near sand dunes was the constant changing and movement of the dunes. When dunes move, it can uproot plants. Thus, grasses and shrubs living in dune areas have developed long, tough roots to hold onto sand dunes.


References:
The Sahara and its people by Simon Scoones

Friday, May 14, 2010

Nuclear power station






















Nuclear energy in radioactive elements --> Heat --> Kinetic energy of steam --> Kinetic energy of turbines --> Electricity

Hydroelectric dams

















Gravitational potential energy of water--> Kinetic energy of the water --> Kinetic energy of turbine --> Electrical energy

Energy

Energy is the ability to do work

Potential Energy
  • stored energy due to a body's position or condition.

Chemical potential energy
  • the energy stored in fuels such as petrol and food
  • can be released through chemical reactions
Gravitational potential energy
  • the energy an object has because of its position or location
Elastic potential energy
  • the energy an object has when it is stretched or compressed
Kinetic energy
  • the energy that a body has due to its motion
Heat energy
  • the energy that flows from a region of higher temperature to one at lower temperature
Light energy
  • the energy that enables us to see
Sound energy
  • the energy produced when objects vibrate
  • allows us to communicate
Electrical energy
  • the energy that results from the flow of charged particles
  • can be transformed into many other forms of energy

Biomass

Biomass, a renewable energy source, is biological material derived from living, or recently living organisms, such as wood, waste, (hydrogen) gas, and alcohol fuels. Biomass is commonly plant matter grown to generate electricity or produce heat. In this sense, living biomass can also be included, as plants can also generate electricity while still alive. The most conventional way on how biomass is used however, still relies on direct incineration. Forest residues for example (such as dead trees, branches and tree stumps), yard clippings, wood chips and garbage are often used herefore. However, biomass also includes plant or animal matter used for production of fibers or chemicals. Biomass may also include biodegradable wastes that can be burnt as fuel. It excludes organic materials such as fossil fuels which have been transformed by geological processes into substances such as coal or petroleum.

Source: Wikipedia

Summary

I learnt lots of things during this term's Physics lessons, like S.I. units, mass, weight, density, work done, moments and energy. I have also learnt about many interesting things such as why face blotters and stiletto heels are not good. I have also learnt from Mr Lim that the weakest part of the school with the least stability is the toilet. Through the video of the airplane, I have learnt about conserving energy and I think that it demonstrated the law of conservation of energy. I really enjoyed Physic lessons this term.

Levers


Levers

First class levers
The fulcrum is between the load and the effort.
Examples: seesaw, scissors, crowbar

Second class levers
The load is between the fulcrum and the effort.
Examples: wheelbarrow, nutcracker

Third class levers
The effort is between the fulcrum and the load.
Examples: fishing rod, broom

The principle of moments

The principle of moments

The principle of moments states:
When a body is in equilibrium, the sum of clockwise moments about a pivot is equal to the sum of anticlockwise moments about the same pivot.

Tuesday, April 20, 2010

Stiletto Heels

Disadvantage of Stiletto Heels

Foot pain

Most of the women suffer from foot pain after walking with high heels. Because of high heels the entire pressure of body is concentrated on the feet. If this happens for a longer time it can cause foot and even hip pain.

Difficulty in walking

Many women find it difficult to walk with high heels. Walking long distance withhigh heels proves to be painful. It often causes heel pain due to walking or standing on high heels for longer time. The way of walking may also look wired. Difficulty in walking may also increase chances of losing balance and falling while walking.

Back pain

Wearing heals causes entire pressure of body fall on the lower back. This pressure falling on the lower back can cause back pain. However proper way of walking, exercise and yoga may help you avoid and get rid of such back pain.

Yellowing and misshapenness

Concentrated body weight on the foot heels may make them harder and develop yellow patches on it. It may also cause misshapenness of your feet. To avoid this you can massage your feet regularly with oil or cream and proper foot care.

Leg Sprain

Major cases of leg sprain in women are caused due to high heels. It may be caused if the person is not used to wearing high heels. Wearing heels regularly may cause serious leg and foot injuries in the future. Many of women are infatuated with high heels even if they are painful. It is a mentality of many women that high heels indicate higher status. However status is worthless if old age is full of leg and back pain.

Others

Stiletto heels concentrate a large amount of force into a small area. The great pressure transmitted through such a heel (allegedly greater than that exerted by an elephant standing on one foot) can cause damage to carpets andfloors. The stiletto heel will also sink into soft ground, making it impractical for outdoor wear on grass.

Wikipedia



Friday, April 16, 2010

High and low tides

High and Low Tides.

Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun, and the rotation of the Earth. Most coastal areas experience two daily high (and two low) tides. This is because at the point right "under" the Moon (the sub-lunar point), the water is at its closest to the Moon, so it experiences stronger gravity and rises. On the opposite side of the Earth (the antipodal point), the water is at its farthest from the moon, so it is pulled less; at this point the Earth moves more toward the Moon than the water does—causing that water to "rise" (relative to the Earth) as well. In between the sub-lunar and antipodal points, the force on the water is diagonal or transverse to the sub-lunar/antipodal axis (and always towards that axis), resulting in low tide.

Tuesday, April 13, 2010

Cartesian Diver

Cartesian Diver

A Cartesian diver or Cartesian devil is a classic science experiment, named for René Descartes, which demonstrates the principle of buoyancy and the ideal gas law.

Experiment Description

The Cartesian diver experiment is set up by placing a "diver"—a small, rigid tube, open at one end—in a much larger container with some flexible component; for example, a two litre soft drink bottle. The larger container is filled with water, and must be airtight when closed. The "diver" is partially filled with a small amount of water, but contains enough air so that it is nearly neutrally buoyant, but still buoyant enough that it floats at the top while being almost completely submerged.

The "diving" occurs when the flexible part of the larger container is pressed inward, causing the "diver" to sink to the bottom until the pressure is released, when it floats again.


Explanation

Air in the diver makes it neutrally buoyant and therefore float at the water's surface. As a result of Pascal's principle(pressure exerted anywhere in a confined fluid is transmitted equally in all directions throughout the fluid), when the pressure increases by squeezing the container, the least dense material, the air in the diver, is affected. Thus, the pressure on the water increases the pressure on the air bubble in the diver. The air compresses and reduces in volume, permitting more water to enter the diver. The diver now displaces a lesser weight of water than its own weight and becomes negatively buoyant (i.e. sinks), according to Archimedes principle. When the pressure on the container is released, the air expands again, increasing the weight of water displaced and the diver again becomes neutrally or positively buoyant and floats. If however, the buoyant force is equal to the compressed air force inside the diver, it will either float straight to the top or it will float in the middle of the container.




Friday, April 2, 2010

How to measure the volume of a cork?

How to measure the volume of a cork?


One way to measure the volume of a cork is:


1) Attach weights to the cork (so it doesn't float)
2) Place it in a measuring cylinder of water
3) Measure the change in height of the water level
4) Put the weights in another measuring cylinder
5) Measure the change in height of the water level
6) Subtract the height of the water level with the weights from the height of the water level of the cork and weights

Thursday, April 1, 2010

Why are we able to float in the Dead Sea?

The Dead Sea
The Dead Sea, also called the Salt Sea, is a salt lake bordering Israel and the West Bank to the west, and Jordan to the east.It is also one of the world's saltiest bodies of water, with 33.7% salinity. This salinity makes for a harsh environment where animals cannot flourish, hence its name. The Dead Sea is 67 kilometres (42 mi) long and 18 kilometres (11 mi) wide at its widest point.

Why is the Dead Sea so salty?

All roads lead to the Sea when it comes to the rivers in the area. The Dead Sea is continually fed water from the rivers and streams coming down off the mountains that surround it. However, no rivers drain out of the Dead Sea. The only way water gets out of the Sea is through evaporation. When the water evaporates, it leaves behind all the dissolved minerals in the Sea, just making it saltier. In fact, it's through the dual action of; 1) continuing evaporation and 2) minerals salts carried into the Sea from the local rivers, that makes the Sea so salty. The fact that the water doesn't escape the Sea just traps the salts within its shores.

Why are we able to float in the Dead Sea?

It is because of the extremely high concentration of dissolved mineral salts in the water its density is way more than that of fresh water. Thus, our bodies are more buoyant in the Dead Sea and its easier to float.

Archimedes


Archimedes of Syracuse was
Greek mathematician, physicist, engineer, inventor, and astronomer. He lived during the 3rd century BC. According to history he was in the bath one day when he discovered the principle of buoyancy. He noticed that as he lowered himself into the bath, the water displaced by his body overflowed the sides and he realized that there was a relationship between his weight and the volume of water displaced. It is said that he ran naked into the street yelling "eureka"(I found it).

Archimedes was on a mission to solve a question that was asked of him by King Hieron II of Syracuse, the home of Archimedes which was a Greek city at the time. The question that the king had asked was about his crown. Was it pure gold or partly silver? Archimedes reasoned that if the crown had any silver in it, it would take up more space than a pure gold crown of the same weight because silver is not as dense as gold. He compared the crown's volume (measured by the amount of water displaced) with the volume of equal weights of gold and then silver, he found the answer. He had to inform his king that the crown was not pure gold.

















Submarines

Kursk Submarine

K-141 Kursk was an Oscar-II class nuclear cruise missile submarine of the Russian Navy. Launched in 1994, it was commissioned in December of that year. At 154m long and four stories high it was the largest attack submarine ever built.

The Explosion

On the morning of 12 August 2000, as part of a naval exercise, Kursk was to fire two dummy torpedoes at a Kirov-class battle cruiser, Pyotr Velikiy, the flagship of the Northern Fleet. High test peroxide (HTP), a form of highly concentrated hydrogen peroxide used as propellant for the torpedo rocket engine, leaked through bad welds in the tubing into the torpedo and catalytically decomposed on the metals and oxides present there, yielding steam and oxygen. The resulting overpressure ruptured the kerosene tank, resulting in a chemical explosion, causing a weak seismic signature detected hundreds of kilometers away.

According to the maintenance records, the dummy torpedoes, manufactured in 1990s, never had their welds checked; it was considered unnecessary as they did not carry a warhead.

An emergency buoy, designed to release from a submarine automatically when emergency conditions such as rapidly changing pressure or fire are detected and intended to help rescuers locate the stricken vessel, did not deploy. The previous summer, in a Mediterranean mission, fears of the buoy accidentally deploying, and thereby revealing the submarine's position to the U.S. fleet, had led to the buoy being disabled.

Two minutes and fifteen seconds after the initial eruption, a much larger explosion ripped through the submarine. Seismic data from stations across Northern Europe show that the explosion occurred at the same depth as the sea bed, suggesting that the submarine had collided with the sea floor which, combined with rising temperatures due to the initial explosion, had caused other torpedoes to explode.

Twenty-three men working in the sixth through ninth compartments survived the two blasts. They gathered in the ninth compartment, which contained the secondary escape tunnel. Captain-lieutenant Dmitri Kolesnikov wrote down the names of those who were in the ninth compartment. The air pressure in the compartment following the second explosion was still normal surface pressure. It is not known with certainty how long the remaining men survived in the compartment. As the nuclear reactors had automatically shut down, emergency power soon ran out, plunging the crew into complete blackness and falling temperatures. Kolesnikov wrote two further messages, much less tidily than before. In the last, he wrote

"It's dark here to write, but I'll try by feel. It seems like there are no chances, 10-20%. Let's hope that at least someone will read this. Here's the list of personnel from the other sections, who are now in the ninth and will attempt to get out. Regards to everybody, no need to be desperate. Kolesnikov." There has been much debate over how long the sailors might have survived. Water is known to leak into a stationary Oscar-II craft through the propeller shafts, and at 100 metres depth it would have been impossible to plug these. Others point out that the many superoxide chemical cartridges, used to absorb carbon dioxide and chemically release oxygen to enable survival, were found used when the craft was recovered, suggesting that they had survived for several days. Ironically, the cartridges appear to have been the cause of death; a sailor appears to have accidentally brought a cartridge in contact with oily sea water, causing a chemical reaction and a flash fire. The official investigation into the disaster showed that some men appeared to have survived the fire by plunging under the water (the fire marks on the walls indicate the water was at waist level in the lower area at this time). However the fire rapidly used up the remaining oxygen in the air, causing death by asphyxiation.

Initially the other ships in the exercise, all of which had detected an explosion, did not report it. Each only knew about its own part in the exercise, and ostensibly assumed that the explosion was that of a depth charge, and part of the exercise. It was not until the evening that commanders stated that they became concerned that they had heard nothing from Kursk. Later in the evening, after repeated attempts to contact Kursk had failed, a search and rescue operation was launched.

The submarine was found in an upright position, with nose plowed about 2 meters deep into the clay seabed, in depth of 108 meters. The periscope was raised, indicating the accident occurred in a low depth. The nose and the bridge showed signs of damage, the conning tower windows were smashed and two missile tube lids were torn off.

Rescue attempts

The United States offered the use of one of its two Deep Submergence Rescue Vehicles, as did the British government, but all offers were refused by the Russian government. Four days after the accident on 16 August 2000, the Russian government accepted the British and Norwegian governments' assistance and a rescue ship was dispatched from Norway on 17 August and reached the site on 19 August. British and Norwegian deep-sea divers reached the ninth compartment escape hatch on Sunday, 20 August. They were able to determine that the compartment was flooded, and all hope of finding survivors was lost.