Thursday, October 15, 2009

Earthquake

What is an earthquake?
An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter. (figure 1)
Sometimes an earthquake has foreshocks. These are smaller earthquakes that happen in the same place as the larger earthquake that follows. Scientists can’t tell that an earthquake is a foreshock until the larger earthquake happens. The largest, main earthquake is called the mainshock. Mainshocks always have aftershocks that follow. These are smaller earthquakes that occur afterwards in the same place as the mainshock. Depending on the size of the mainshock, aftershocks can continue for weeks, months, and even years after the mainshock!
What causes earthquakes and where do they happen?
The earth has four major layers: the inner core, outer core, mantle and crust. (figure 2) The crust and the top of the mantle make up a thin skin on the surface of our planet. But this skin is not all in one piece – it is made up of many pieces like a puzzle covering the surface of the earth. (figure 3) Not only that, but these puzzle pieces keep slowly moving around, sliding past one another and bumping into each other. We call these puzzle pieces tectonic plates, and the edges of the plates are called the plate boundaries. The plate boundaries are made up of many faults, and most of the earthquakes around the world occur on these faults. Since the edges of the plates are rough, they get stuck while the rest of the plate keeps moving. Finally, when the plate has moved far enough, the edges unstick on one of the faults and there is an earthquake.
Why does the earth shake when there is an earthquake?
While the edges of faults are stuck together, and the rest of the block is moving, the energy that would normally cause the blocks to slide past one another is being stored up. When the force of the moving blocks finally overcomes the friction of the jagged edges of the fault and it unsticks, all that stored up energy is released. The energy radiates outward from the fault in all directions in the form of seismic waves like ripples on a pond. The seismic waves shake the earth as they move through it, and when the waves reach the earth’s surface, they shake the ground and anything on it, like our houses and us! (see P&S Wave inset)
How are earthquakes recorded?
Earthquakes are recorded by instruments called seismographs. The recording they make is called a seismogram. (figure 4) The seismograph has a base that sets firmly in the ground, and a heavy weight that hangs free. When an earthquake causes the ground to shake, the base of the seismograph shakes too, but the hanging weight does not. Instead the spring or string that it is hanging from absorbs all the movement. The difference in position between the shaking part of the seismograph and the motionless part is what is recorded.
How do scientists measure the size of earthquakes?
The size of an earthquake depends on the size of the fault and the amount of slip on the fault, but that’s not something scientists can simply measure with a measuring tape since faults are many kilometers deep beneath the earth’s surface. So how do they measure an earthquake? They use the seismogram recordings made on the seismographs at the surface of the earth to determine how large the earthquake was (figure 5). A short wiggly line that doesn’t wiggle very much means a small earthquake, and a long wiggly line that wiggles a lot means a large earthquake. The length of the wiggle depends on the size of the fault, and the size of the wiggle depends on the amount of slip.
The size of the earthquake is called its magnitude. There is one magnitude for each earthquake. Scientists also talk about the intensity of shaking from an earthquake, and this varies depending on where you are during the earthquake.
How can scientists tell where the earthquake happened?
Seismograms come in handy for locating earthquakes too, and being able to see the P wave and the S wave is important. You learned how P & S waves each shake the ground in different ways as they travel through it. P waves are also faster than S waves, and this fact is what allows us to tell where an earthquake was. To understand how this works, lets compare P and S waves to lightning and thunder. Light travels faster than sound, so during a thunderstorm you will first see the lightning and then you will hear the thunder. If you are close to the lightning, the thunder will boom right after the lightning, but if you are far away from the lightning, you can count several seconds before you hear the thunder. The further you are from the storm, the longer it will take between the lightning and the thunder.
P waves are like the lightning, and S waves are like the thunder. The P waves travel faster and shake the ground where you are first. Then the S waves follow and shake the ground also. If you are close to the earthquake, the P and S wave will come one right after the other, but if you are far away, there will be more time between the two. By looking at the amount of time between the P and S wave on a seismogram recorded on a seismograph, scientists can tell how far away the earthquake was from that location. However, they can’t tell in what direction from the seismograph the earthquake was, only how far away it was. If they draw a circle on a map around the station where the radius of the circle is the determined distance to the earthquake, they know the earthquake lies somewhere on the circle. But where?
Scientists then use a method called triangulation to determine exactly where the earthquake was (figure 6). It is called triangulation because a triangle has three sides, and it takes three seismographs to locate an earthquake. If you draw a circle on a map around three different seismographs where the radius of each is the distance from that station to the earthquake, the intersection of those three circles is the epicenter!
Can scientists predict earthquakes?
No, and it is unlikely they will ever be able to predict them. Scientists have tried many different ways of predicting earthquakes, but none have been successful. On any particular fault, scientists know there will be another earthquake sometime in the future, but they have no way of telling when it will happen.
Is there such a thing as earthquake weather? Can some animals or people tell when an earthquake is about to hit?
These are two questions that do not yet have definite answers. If weather does affect earthquake occurrence, or if some animals or people can tell when an earthquake is coming, we do not yet understand how it works.

Source:http://earthquake.usgs.gov

Ways to relese stress

We are currently living in a capitalist society where money and power rule. Therefore, many of us have become workaholics and often overlook signs of tiredness in order to stay on track. I am not saying that people should stop working hard to achieve their goals. However, there is a slight problem we do not know how to manage our stress, which is definitely not a good thing! Stress has been linked to mental/emotional (depression, anxiety, and anger) and physical illnesses (weakens the immune system). Therefore, it is more than important that you constantly work on reducing your stress level in order to maintain your overall health. The bottom line is, if we are not healthy there is no money or power that will make things better. So, take care of yourself. Below, I have added six stress releasing tips.
Exercise: even if you go for a walk for 15-25 minutes four days a week it will help your body to get rid of adrenaline and produce endorphins (a natural tranquilizer). Not to mention you will not only feel better, you will also look the part.
Yoga: Many ramble that practicing yoga is the best way to manage or release stress. It focuses on breathing techniques, exercises, connecting with the universe on a spiritual and mental level. If this option seems interesting to you I suggest you do some research in order to learn the principles and decide if it is for you.
Stretch: People often stretch before and after a workout. However, learning stretching and flexing exercises to use as a way to relieve tension on many different areas of the body can help a great deal.
Massage: We all know how massages can help us relax and release tension. Prices start around $40 for 30 minutes; it all depends on what extra relaxation techniques you would like to add to the massage such as aromatherapy, oils, etc. There are also different types of massages so this will also affect the price. I actually found a therapist that charges $33 for a 30 minute session. It sounds pretty good to me. We waste money in so many different ways so investing on a massage once in a while will not kill our pockets.
Laugh it off: Rent a funny movie and laugh out loud. Go out with friends or host gatherings. Tell everyone to bring a platter. Remember the key is to release tension not, add to it. Use paper plates and plastic cups to reduce the amount of work.
Take a break- Take time to relax, sleep, and maybe even take a vacation if you can. Your body does not only need it; you deserve it.
Source:http://ezinearticles.com

Saturday, October 10, 2009

Hepatitis B

Hepatitis B
From Wikipedia, the free encyclopedia
Hepatitis B is a disease caused by hepatitis B virus (HBV) which infects the liver of hominoidae, including humans, and causes an inflammation called hepatitis. Originally known as "serum hepatitis",[1] the disease has caused epidemics in parts of Asia and Africa, and it is endemic in China. [2] About a third of the world's population, more than 2 billion people, have been infected with the hepatitis B virus.[3] This includes 350 million chronic carriers of the virus.[4] Transmission of hepatitis B virus results from exposure to infectious blood or body fluids containing blood.
The acute illness causes liver inflammation, vomiting, jaundice and—rarely—death. Chronic hepatitis B may eventually cause liver cirrhosis and liver cancer—a fatal disease with very poor response to current chemotherapy.[5] The infection is preventable by vaccination.[6]
Hepatitis B virus is an hepadnavirus—hepa from hepatotrophic and dna because it is a DNA virus[7]—and it has a circular genome composed of partially double-stranded DNA. The viruses replicate through an RNA intermediate form by reverse transcription, and in this respect they are similar to retroviruses.[8] Although replication takes place in the liver, the virus spreads to the blood where virus-specific proteins and their corresponding antibodies are found in infected people. Blood tests for these proteins and antibodies are used to diagnose the infection.[9]
Medical aspects
[edit] Prevention
Several vaccines have been developed for the prevention of hepatitis B virus infection. These rely on the use of one of the viral envelope proteins (hepatitis B surface antigen or HBsAg). The vaccine was originally prepared from plasma obtained from patients who had long-standing hepatitis B virus infection. However, currently, these are more often made using recombinant DNA technology, though plasma-derived vaccines continue to be used; the two types of vaccines are equally effective and safe.[26]
Following vaccination Hepatitis B Surface antigen may be detected in serum for several days; this is known as vaccine antigenaemia.[27] Vaccine is generally administered in either a two, three, or four dose schedules; and can be received by infants to adults. It provides protection for 85-90% of individuals,[28] and lasts for 23 years.[29]
Unlike Hepatitis A, Hepatitis B does not generally spread through water and food. Instead, it is transmitted through body fluids, from which prevention is taken to avoid: unprotected sexual contact, blood transfusions, re-use of contaminated needles and syringes, and vertical transmission during child birth. Infants may be vaccinated at birth.[30]
Symptoms
File:Jaundice2008.jpg
Jaundice in a man with hepatic failure.
Acute infection with hepatitis B virus is associated with acute viral hepatitis - an illness that begins with general ill-health, loss of appetite, nausea, vomiting, body aches, mild fever, dark urine, and then progresses to development of jaundice. It has been noted that itchy skin has been an indication as a possible symptom of all hepatitis virus types. The illness lasts for a few weeks and then gradually improves in most affected people. A few patients may have more severe liver disease (fulminant hepatic failure), and may die as a result of it. The infection may be entirely asymptomatic and may go unrecognized.
Chronic infection with Hepatitis B virus may be either asymptomatic or may be associated with a chronic inflammation of the liver (chronic hepatitis), leading to cirrhosis over a period of several years. This type of infection dramatically increases the incidence of hepatocellular carcinoma (liver cancer). Chronic carriers are encouraged to avoid consuming alcohol as it increases their risk for cirrhosis and liver cancer. Hepatitis B virus has been linked to the development of Membranous glomerulonephritis (MGN).[31]
[edit] Diagnosis
The tests, called assays, for detection of hepatitis B virus infection involve serum or blood tests that detect either viral antigens (proteins produced by the virus) or antibodies produced by the host. Interpretation of these assays is complex.[9]

Hepatitis B viral antigens and antibodies detectable in the blood following acute infection.


Hepatitis B viral antigens and antibodies detectable in the blood of a chronically infected person.
The hepatitis B surface antigen (HBsAg) is most frequently used to screen for the presence of this infection. It is the first detectable viral antigen to appear during infection. However, early in an infection, this antigen may not be present and it may be undetectable later in the infection as it is being cleared by the host. The infectious virion contains an inner "core particle" enclosing viral genome. The icosahedral core particle is made of 180 or 240 copies of core protein, alternatively known as hepatitis B core antigen, or HBcAg. During this 'window' in which the host remains infected but is successfully clearing the virus, IgM antibodies to the hepatitis B core antigen (anti-HBc IgM) may be the only serological evidence of disease.
Shortly after the appearance of the HBsAg, another antigen named as the hepatitis B e antigen (HBeAg) will appear. Traditionally, the presence of HBeAg in a host's serum is associated with much higher rates of viral replication and enhanced infectivity; however, variants of the hepatitis B virus do not produce the 'e' antigen, so this rule does not always hold true. During the natural course of an infection, the HBeAg may be cleared, and antibodies to the 'e' antigen (anti-HBe) will arise immediately afterwards. This conversion is usually associated with a dramatic decline in viral replication.
If the host is able to clear the infection, eventually the HBsAg will become undetectable and will be followed by IgG antibodies to the hepatitis B surface antigen and core antigen, (anti-HBs and anti HBc IgG).[7] The time between the removal of the HBsAg and the appearance of anti-HBs is called the window period. A person negative for HBsAg but positive for anti-HBs has either cleared an infection or has been vaccinated previously.


Ground glass hepatocytes as seen in a chronic hepatitis B infection. Liver biopsy. H&E stain.
Individuals who remain HBsAg positive for at least six months are considered to be hepatitis B carriers.[32] Carriers of the virus may have chronic hepatitis B, which would be reflected by elevated serum alanine aminotransferase levels and inflammation of the liver, as revealed by biopsy. Carriers who have seroconverted to HBeAg negative status, particularly those who acquired the infection as adults, have very little viral multiplication and hence may be at little risk of long-term complications or of transmitting infection to others.[33]
More recently, PCR tests have been developed to detect and measure the amount of viral nucleic acid in clinical specimens. These tests are called viral loads and are used to assess a person's infection status and to monitor treatment.[34] Individuals with high viral loads, characteristically have ground glass hepatocytes on biopsy.
[edit] Treatment
Acute hepatitis B infection does not usually require treatment because most adults clear the infection spontaneously.[35] Early antiviral treatment may only be required in fewer than 1% of patients, whose infection takes a very aggressive course ("fulminant hepatitis") or who are immunocompromised. On the other hand, treatment of chronic infection may be necessary to reduce the risk of cirrhosis and liver cancer. Chronically infected individuals with persistently elevated serum alanine aminotransferase, a marker of liver damage, and HBV DNA levels are candidates for therapy.[36]
Although none of the available drugs can clear the infection, they can stop the virus from replicating, and minimize liver damage such as cirrhosis and liver cancer. Currently, there are seven medications licensed for treatment of hepatitis B infection in the United States. These include antiviral drugs lamivudine (Epivir), adefovir (Hepsera), tenofovir (Viread), telbivudine (Tyzeka) and entecavir (Baraclude) and the two immune system modulators interferon alpha-2a and pegylated interferon alfa-2a (Pegasys). The use of interferon, which requires injections daily or thrice weekly, has been supplanted by long-acting pegylated interferon, which is injected only once weekly.[37] However, some individuals are much more likely to respond than others and this might be because of the genotype of the infecting virus or the patient's heredity. The treatment works by reducing the viral load (the amount of virus particles as measured in the blood), which in turn reduces viral replication in the liver.
Infants born to mothers known to carry hepatitis B can be treated with antibodies to the hepatitis B virus (hepatitis B immune globulin or HBIg). When given with the vaccine within twelve hours of birth, the risk of acquiring hepatitis B is reduced 95%. This treatment allows a mother to safely breastfeed her child.
Source:http://en.wikipedia.org/wiki/Hepatitis_B

Tuesday, September 29, 2009

Proton Exora

Proton Exora
From Wikipedia, the free encyclopedia
The Proton Exora is a compact MPV vehicle produced by Malaysia car manufacturer Proton and launched on 15 April 2009. It is a new model from Proton based on a new chassis. The development of this MPV starts from scratch and it is the first Malaysian-designed MPV. Fully undisguised photos of Proton Exora were leaked onto the internet on the 23rd of January 2009, ahead of the MPV's April 2009 launch date.
The Proton Exora chassis uses a MacPherson strut design at the front and a torsion beam at the rear. It measures 4,592mm long, 1,809mm wide and 1,691mm tall with a wheelbase of 2,730mm. It is powered by the Campro CPS engine producing 125 horsepower and 150Nm of torque, resulting the top speed of165 km/h (103 mph).
The average fuel consumption of 7.2 L/100 km (39 mpg-imp; 33 mpg-US). The gearbox is similar to the Proton Waja and Proton Gen-2 but has a higher final drive ratio to help with power delivery.
The Exora features a Body Control module which allows automatic activation and configuration of various vehicle functions such as door locking/unlocking, interior lamps, headlamps, brake lamps and wipers.
Source:http://en.wikipedia.org/wiki/Proton_Exora

Sunday, August 30, 2009

iPhone 3GS

Apple unveiled a new version of the iPhone. Dubbed the iPhone 3G S, the latest version of Apple’s popular smartphone promises to launch applications and run software faster than the previous model, as well as take advantage of faster cellular networks. It debuts in the U.S. on June 19, two days after the iPhone 3.0 software update arrives.
The new phone will also be available in Canada, France, Germany, Italy, Spain, and Switzerland on June 19. A week later, Apple says, the phone will launch in six more countries, with more launches to come in July and August.
“The ‘S’ stands for speed,” Phil Schiller, Apple’s senior vice president of worldwide product marketing, told Worldwide Developers Conference attendees during Monday’s conference-opening keynote.
“Overall, it’s just a faster better, quicker, snappier experience,” Bob Borchers, senior director of worldwide iPhone product marketing, told Macworld. Borchers said that developers of iPhone apps would have “a lot more headroom to play with,” and suggested that users would appreciate “the speed of the processor and the overall experience.” While Apple is loath to discuss technical specifications of iPhones, the technical message here is clear: the iPhone 3G S is faster at least in part because it’s powered by a faster processor, has more available onboard memory, and perhaps features improved display circuitry.
The iPhone 3G S can also take advantage of 7.2 Mbps HSDPA, a faster cellular networking format that’s becoming available in some countries, including the U.S.
For new and qualifying AT&T customers, the new iPhone will sell for $199 for the 16GB version and $299 for a 32GB model. Apple is also cutting the price on the current iPhone 3G to $99 for the 8GB phone. However, people who bought the iPhone 3G last year will discover that the cost to upgrade to this new model will be higher. Because AT&T subsidizes the purchase of iPhones and amortizes those costs over a two-year contract commitment period, many existing iPhone users will need to pay higher prices, which can vary based on each person’s individual contract standing with AT&T.
Physically, the iPhone 3G S is almost identical to the previous iPhone 3G model. The only exterior differences are painfully subtle: the “fine print” writing on the back of the phone is now color-matched to the silver Apple logo, and the screen is covered with a new oil-resistant coating.
But there are changes on the inside. the new phone offers a brand-new camera that lets you control the focus either by tapping on the screen or using the autofocus feature. In addition, the iPhone’s new camera also captures standard-definition video.
The iPhone 3G S also comes with Apple’s new standard for headphones, previously found in the second-generation iPod touch, fourth-generation iPod nano, and fourth-generation iPod shuffle. This set of headphones includes a microphone, a clicker, and volume controls.
Holding down the clicker — or, if you’re not using headphones, the iPhone 3G S’s Home button — activates the phone’s new Voice Control feature, which allows users to speak commands for applications on the phone, including dialing contacts and playing music. Accessibility improvements on the iPhone 3G S include VoiceOver support for reading to users and the ability to zoom in on the phone’s display for larger icons.
Enterprise users get a requested feature in the form of hardware encryption. For anyone using an Exchange service or the Find Your iPhone feature in the iPhone 3.0 software update, remote wipe is instantaneous and backups are encrypted whenever hardware encryption is enabled.
Apple promises improved battery life with the iPhone 3G S. The new phone offers nine hours of Internet access on Wi-Fi, 10 hours of video, 30 hours of audio playback, and 12 hours of 2G talk time. The five hours of 3G talk time on the new model is consistent with the estimated talk time of the previous iPhone 3G.
In keeping with Apple’s ongoing push to tout the environmental friendliness of its products, the company noted that it reduced packaging for the phone by 23 percent. The iPhone 3G S also features arsenic-free glass and a mercury-free LCD; the phone is also free of brominated flame retardant (BFR) and PVC.

Source:http://www.macworld.com/article/141031/2009/06/iphone3gs.html

Friday, July 10, 2009

Hi, world. This is my first post at UMP. Everything is ok over here.