Monday, October 31, 2011

cash for votes case proceeds on

cash for votes case proceeds on

The Delhi Police arrested Sohail Hindustani, a Bharatiya Janata Yuva Morcha activist, at Chanakyapuri here on Wednesday after questioning him for more than seven hours in the cash-for-votes scam case.

He was formally arrested around 6 p.m., under the Prevention of Corruption Act, and will be produced in court on Thursday. Hindustani is the second person to be arrested in the case in less than a week.

Sanjeev Saxena, alleged to be an aide of the then Samajwadi Party general secretary, Amar Singh, was arrested on July 17, after the Supreme Court pulled up the Delhi Police for a shoddy probe.

Earlier, Hindustani told journalists outside the police complex that he would tell the police whatever he had told the Parliamentary Committee that probed the scandal, which rocked Parliament on July 22, 2008.

Hindustani alleged that he was approached by Mr. Amar Singh and several Congress leaders for “arranging” Bharatiya Janata Party MPs for the trust vote.

The Supreme Court on Friday August 05 2011 asked the police to take the probe to its logical conclusion and submit a final report in three weeks.

A bench of justices Aftab Alam and RM Lodha, while lamenting that a middleman of the "cheapest kind" was allowed to derail parliamentary proceedings, termed the probe conducted so far as "half-hearted, meaningless and hopeless". "Delhi police is capable of doing investigation as good as any other agency. But Delhi police seems to be having inhibitions. You should drop the inhibition," the bench told Additional Solicitor General Haren Rawal appearing for the police department.

Delhi Police on Wednesday chargesheeted Amar Singh, Ashok Argal, Mahaveer Bhagoda, Phagan Singh Kulaste, Sudheendra Kulkarni, Sanjeev Saxena and Sohail Hindustani in the cash-for-votes case. The police has asked for the sanction of the Lok Sabha Speaker to chargesheet Ashok Argal as he is a sitting BJP MP. Delhi Police will file the status report in the Supreme Court on September 2. The police on August 18 told a Delhi court that the probe in the 2008 cash-for-vote scam was nearing completion and it would file the chargesheet before it on August 25.



Hindustani's counsel accused the police of not providing them or even the court the complete facts of the case.

Mr Singh, a former Samajwadi Party leader, was arrested on September 6 and sent to Tihar Jail for his alleged involvement in bribing of MPs ahead of the trust vote in Parliament in July 2008.

The court had, last Wednesday, reserved its order on the bail applications till October 24. The ruling had come after the Delhi Police submitted before the court that the All India Institute of Medical Sciences (AIIMS), where Amar Singh is admitted, said in its report that the MP's condition was critical and he needed constant monitoring.

The 55-year-old leader is currently admitted at AIIMS where he was brought to on September 12 from Tihar Jail after complaining of vomiting and pain in the kidneys. He has been undergoing treatment for renal infection there ever since.

Mr Singh, who is a diabetic, underwent a renal transplant in September 2009 and intestinal surgery 10 years ago. He also suffers from hypertension, tuberculosis infection, chronic kidney disease and urinary tract infection.

Mr Singh is an accused along with the three BJP MPs who were allegedly bribed in 2008 - Ashok Argal, Faggan Singh Kulaste and Mahavir Singh Bhagora. Of the trio, only Mr Argal is a serving party MP. Senior BJP leader LK Advani's former aide Sudheendra Kulkarni and activist Suhail Hindustani and Sanjeev Saxena are also named as accused in the case. All of them have been chargesheeted by the Crime Branch of the Delhi Police. It has been alleged that Mr Singh hatched a criminal conspiracy to bribe the then BJP MPs to influence their voting in the confidence motion in the Lok Sabha in 2008 against Manmohan Singh-led UPA government. At the time of the trust vote, he was a senior leader with the Samajwadi Party.

BJP Tuesday questioned the investigations into the 2008 cash-for-votes case saying while no action has been taken against those who benefited in the scam, the ones who exposed it are behind bars. He said it was unfortunate that those who "exposed" the scam are behind bars "even on Diwali".

Former BJP MPs Faggan Singh Kulaste and Mahavir Bhagora along with former aide of party leader L K Advani Sudheendra Kulkarni are in judicial custody while expelled Samajwadi Party leader Amar Singh has been granted bail on health grounds.

"The entire country is agitated," Prasad said ahead of Leader of Opposition in Lok Sabha Sushma Swaraj's meeting with the three in Tihar Jail.

The Delhi high court on Monday stayed a trial court order issuing summons to Samajwadi Party  Raman Singh to appear as an accused in 2008 cash-for-vote scam case.

"The proceedings before the trial court shall be stayed till the next date of hearing that is November 15," Justice Suresh Kait said while allowing Raman's plea that he be not forced to appear as an accused before the trial court. The court, which issued a notice to Delhi Police after taking note of the petition, said the "audio-video CDs of the sting operation" be also submitted to it on the next date of hearing.

Earlier, the lower court had brushed aside the clean chit given to Singh in the scam and issued a summon as an accused to him for November 3, saying "there was sufficient material to show that he was a part of alleged criminal conspiracy."

Sosurces:
dnaindia.com
EconomicTimes
ndtv.com
ibnlive.in
zeenews
thehindu.com
en.wikipedia

ปูตินและพันธมิตร Medvedev คู่แข่งไม่โชคดีรัสเซีย


ปูตินและพันธมิตร Medvedev คู่แข่งไม่โชคดีรัสเซีย

หลังจากที่คาดเดาระยะเวลาที่เกี่ยวกับการเลือกตั้งประธานาธิบดี 2012 ในรัสเซียทั้งสองผู้นำที่แข็งแกร่งของรัสเซียทำให้มันสมบูรณ์ชัดเจนว่าสิ่งที่ผูกพวกเขาที่พวกเขาเป็นพันธมิตรไม่คู่แข่ง

Medvedev แต่งตั้งปูตินเป็นผู้สมัครที่พรรคเพื่อการเลือกตั้งประธานาธิบดีรัสเซีย




อ่านเพิ่มเติม :
b92.net/eng/news
naharnet.com
bbc.co.uk/news
menafn.com

AAE cilvēki ir sadalītas AAE sievietēm laulības ar ārzemnieku


AAE cilvēki ir sadalītas AAE sievietēm laulības ar ārzemnieku

Apvienoto Arābu Emirātu cilvēki dalās jautājumā par laulības Emaratean sieviete, lai ārzemju vīru. Dažas no tām ir pret šo laulību, kamēr citi pieņem to ar vienu nosacījumu, ka vīrs ir Arabian vēlams līča arābu.

Related Sites:

Apakah di sebalik kejayaan laman web atas Rusia


Apakah di sebalik kejayaan laman web atas Rusia

Vkontakte.ru - laman ini mengintegrasikan fungsi Facebook bersama-sama dengan posting video dengan cara yang sama photos are posted dalam Facebook. Sedikit kekurangan dalam keupayaan kerana ia tidak membuka API. Walaupun terdapat profil newsfeed Vkontakte adalah laman yang paling banyak dikunjungi di Rusia, dengan lebih daripada 13 juta pengguna berdaftar.

Mail.ru berjaya menjadi tapak kedua yang paling banyak dikunjungi di Rusia menurut Alexa, dan mel terkemuka Rusia portal, yang termasuk banyak ciri-ciri rangkaian sosial yang lain seperti perkongsian gambar dan video, blog, penanda buku, peta, berita dan lain-lain lagi.

Yandex.ru telah menjadi carian Rusia terbesar enjin, digabungkan dengan perkhidmatan tambahan

seperti e-mel, berita, peta, kamus, penanda buku dan sebagainya. Enjin carian dioptimumkan kursus untuk morfologi bahasa Rusia.

Odnoklassniki.ru memilih rakan-rakan sekolah menjadi kunci bagi perkumpulan orang untuk berkomunikasi. Kejayaan yang amat besar bahawa ia telah disapu Rusia oleh ribut. Ia adalah alat mudah untuk mencari rakan sekolah. Pendaftaran hanya boleh dilakukan jika pengguna memberikan maklumat tentang sekolah mereka. Setelah mendaftar mereka boleh post gambar, menghantar mesej kepada pengguna lain yang boleh diperiksa menggunakan sekolah atau kolej mereka pergi kepada atau melalui nama. Ia juga mengandungi ciri-ciri forum, tetapi nilai utamanya adalah untuk membantu mencari orang bukannya mengekalkan perhubungan yang tetap dan berkongsi maklumat di luar gambar. Odnoklassniki dianggap sebagai tapak keempat yang paling banyak dikunjungi dan mempunyai lebih daripada 18 juta pengguna berdaftar.

Laman Rusia teratas:



활성 태풍은 여전히​​ 꿈을 그것이 가능 적대감이나


활성 태풍은 여전히​​ 꿈을 그것이 가능 적대감이나

허리케인 아이린 활성화와 동해안 미국 과학자와 엔지니어를 향하고있다는 자연 기상 재해 컨트롤의 꿈을 리콜 도울 수로.

수동 및 활성 같은 현상 제어 두 개의 접근로 구성되어 있습니다.

수동 방식에서는 노력은 현재의 위치를​​ 결정하기 위해 태풍을 감시는 예상 궤도를 예측하고 마지막으로 가장 취약한 건물을 강화하고 최고의 예상 손실 및 사상자 와 장소의 사람들을 철수를 포함한 필요한 조치가 필요 복용을 기반으로합니다.

반면에 적극적인 접근은 또한 모니터링 및 예측을 포함하지만, 그것은 적절한 기술적 장치를 설계하고 허리케인 전체 에너지의 일부 금액을 소비하는 그들에게 목적으로 일부 선택된 위치를 전개와 피난의 일부를 거래하는 피난에 올 때 포함되어 있습니다.

다른 모든 엔지니어링 문제와 마찬가지로 취할 조치의 비용은 당신이 피하려고하는 손해 및 사상자 와 관련이 있습니다. 이 연구는 예를 들어 지난 20 년 동안 허리케인의 사상자 과 손해의 역사를 함께 넣어하는 것입니다 중 하나가 간소화 것을 의미합니다.

예를 들어 허리케인 플로이드 57 사망, 주 전체 커뮤니티 수중 계속되는 손해 및 광범위한 홍수에 45억달러을 담당했습니다.

수동 접근법은 국가 기관의 연구와 의사 결정을 기반으로하지만, 일부 특정 기술 장치를 설계에 따라 활성 접근뿐만 아니라 해외 지식인을 수용할 수 있습니다. 과학은 국가 간의 경계를 인식하지 못합니다. 인류 한 인간입니다.

Ert þú áhuga á að humar í Flórída


Ert þú áhuga á að humar í Flórída

Á síðasta ári var 4.000.000 £ í atvinnuskyni veiddur í Keys. Það var sjötti versta veiða á 19 árum færslur hafa verið haldið, en táknar `` nýja meðaltali''eins og það er sagt.

Humar sjómenn hafa haft erfitt að fara af henni undanfarin ár, frá og með 2001-2002 árstíð þegar auglýsing löndun í Monroe County féll til 2.700.000 £ í næstum £ 5.000.000 í fyrra og 6800000 £ árinu áður.

Lækkaði einnig vegna þess að um heim allan samdráttur verulega minni eftirspurn eftir sjávarafurðum lúxus.

Humar sjómenn einnig hafa verið skellur með hækkandi eldsneytiskostnaður, ódýr innflutningur og hellingur af fellibylja í gegnum árin sem eyðilagt þúsundir Ótryggðir gildrur þeirra hver verður um $ 35 til $ 50.

Gildrur líka ekki koma með viðvörun. Trap ræna hefur alltaf verið stórt vandamál.

Heimildir:



چین اور دنیا کی سب سے لمبی پر پانی پل کھول دیا ہے

چین اور دنیا کی سب سے لمبی پر پانی پل کھول دیا ہے

جمعرات ، 30 جون کو چین دنیا میں سب سے طویل سمندری پل کھول دیا ، Qingdao کے شہر اور شیڈونگ مشرقی ایران میں صوبے میں Jiaozho Huangdao کی خلیج میں شہر سے منسلک. پل 36،48 کلومیٹر کی لمبائی ہے اور 8 لائنوں پر مشتمل ہوتا ہے.

توقع ہے کہ پل نصف Qingdao اور Hoangdo ئ. آئ کے شہروں کے درمیان وقت کو کاٹ دے گا 20 منٹ سے 40 منٹ سے وقت کو کم کرنے.

پل 30،000 کاروں ایک دن میں لے جانے کا امکان ہے. اس پر کام مارچ 2007 میں 2.3 ارب ڈالر کی لاگت سے شروع کر دیا ہے ،.

ذرائع کے مطابق :

Sunday, October 30, 2011

bail pleas of four accused in the Cash-for-votes

bail pleas of four accused in the Cash-for-votes

The four accused approached the high court challenging the order of the trial court dismissing their bail pleas.

Kulkarni, who is in jail since September 27, has challenged the trial court's order which had rejected his bail plea saying that he was the 'guiding star' and 'facilitator' of the conspiracy aimed at mocking the Republic of India.

Meanwhile, BJP MP Ashok Argal, an accused in the case, has also moved the Delhi High Court seeking anticipatory bail in the case and his bail plea is likely to be heard on Tuesday.

The Delhi High Court on Monday sought response from the police on the bail pleas of four accused, including Sudheendra Kulkarni, a former aide of BJP leader LK Advani, and two ex-BJP MPs in the cash-for-vote scam.

Issuing notice to Delhi Police, Justice ML Mehta sought its response by November 14 on the bail pleas of Kulkarni, former BJP MPs Faggan Singh Kulaste, Mahabir Singh Bhagora and alleged BJP activist Suhail Hindustani.

Source: IBNLive

Saturday, October 29, 2011

How the strength of earthquakes is determined

How the strength of earthquakes is determined

Earthquakes occur when the tectonic plates that make up the earth’s crust interact with one another. Some earthquakes are caused by the plates moving passed one another and others are caused by one plate sliding under the other. The size of an earthquake depends on the amount of force that has built up at the point of contact. Sometimes the plates moving causes only a slight tremor, whereas in other instances the movement can cause cataclysmic destruction.

Earthquakes usually occur in places where two plates meet, called faults. Earthquakes are mostly generated deep within the earth's crust, when the pressure between two plates is too great for them to be held in place. The underground rocks then snap, sending shock waves out in all directions. These are called seismic waves. The underground origin of an earthquake is called the focus. The point at which an earthquake originates on the surface is called the epicentre.

Earthquakes are commonly measured by their magnitude and intensity.Magnitude is a measure of the total energy released during an earthquake. It is determined from a seismograph, which plots the ground motion produced by seismic waves.

The Japanese "shindo" scale for measuring earthquakes is more commonly used in Japan than the Richter scale to describe earthquakes. Shindo refers to the intensity of an earthquake at a given location, i.e. what people actually feel at a given location, while the Richter scale measures the magnitude of an earthquake, i.e. the energy an earthquake releases at the epicenter. The shindo scale ranges from shindo one, a slight earthquake felt only by people who are not moving, to shindo seven, a severe earthquake. Shindo two to four are still minor earthquakes that do not cause damage, while objects start to fall at shindo five, and heavier damage occurs at shindo six and seven.

Magnitude is a measure of the amount of energy released during an earthquake. The magnitudes measured using the Richter scale. The logarithms of the wave heights on seismograms measured in microns (1/1,000,000th of a meter, or 1/1000th of a millimeter) because some earthquakes made very small waves whereas others produced large waves..A wave one millimeter (1000 microns) high on a seismogram would have a magnitude of 3 because 1000 is ten raised to the third power. In contrast, a wave ten millimeters high would have a magnitude of 4.

A seismograph as a kind of sensitive pendulum that records the shaking of the Earth. The output of a seismograph is known as a seismogram. In the early days, seismograms were produced using ink pens on paper or beams of light on photographic paper, but now it's most often done digitally using computers. John Milne was the English seismologist and geologist who invented the first modern seismograph and promoted the building of seismological stations. The horizontal pendulum seismograph was improved after World War II with the Press-Ewing seismograph, developed in the United States for recording long-period waves. It is widely used throughout the world today. The Press-Ewing seismograph uses a Milne pendulum, but the pivot supporting the pendulum is replaced by an elastic wire to avoid friction.



Today, state of the art seismic systems transmit data from the seismograph via telephone line and satellite directly to a central digital computer. A preliminary location, depth-of-focus, and magnitude can now be obtained within minutes of the onset of an earthquake. The only limiting factor is how long the seismic waves take to travel from the epicenter to the stations - usually less than 10 minutes.

The seismograph that Dr. Richter used amplified movements by a factor of 3000, so the waves on the seismograms were much bigger than those that actually occurred in the Earth. Seismologists today do not use the Richter scale as a universal tool for measuring earthquakes, because it does not accurately measure the energy emitted in jolts as big as the one that hit Japan.

Instead Seismologists have since developed a new measurement of earthquake size, called moment magnitude. Moment is a physical quantity more closely related to the total energy released in the earthquake than the Richter magnitude. It can be estimated by geologists examining the geometry of a fault in the field or by seismologists analyzing a seismograph. Moment magnitude has many advantages over other magnitude scales. First, all earthquakes can be compared on the same scale. (Richter magnitude is only precise for earthquakes of a certain size and distance from a seismometer.) Second, because it can be determined either instrumentally or from geology, it can be used to measure old earthquakes and compare them to instrumentally recorded earthquakes. Third, by estimating how large a section of fault will likely move in the future, the magnitude of that earthquake can be calculated with confidence.

To measure all the energy produced by a colossal earthquake, seismologists sometimes have to wait days or weeks to analyze the vibrations of the entire Earth. Using seismic data for an earthquake from a variety of sensors, researchers can infer what they call a “moment tensor,” a three-dimensional plot of both a fault’s orientation and the direction in which it slipped, as well as the distance the fault slipped. This is then used to calculate the total energy released by the earthquake, which the moment magnitude scale’s numbers represent. The moment magnitude scale is calibrated so that it roughly matches the Richter scale’s numbers up to 7.0 or so. But unlike the Richter scale, the moment magnitude scale does not suffer from the saturation problem, and can account for the energy released by unexpectedly large earthquakes.

On the Richter scale, each whole-number step represents an approximate thirty-two fold increase in released energy. For example:
6.0 is equal to 32 times the energy of a 5.0
1,000 times the energy of a 4.0 and
32,000 times the energy released by a 3.0

Two tenths rule:
Every two-tenths of a unit represents double the energy released at the focus.
5.0 to a 5.2 is twice as big
5.4 is four times as large as a 5.0
5.6 is eight times as large as a 5.0

Scientists also guage earthquakes by intensity, which is the degree of damage from an earthquake at a particular location. The intensity scale, the Modified Mercalli Scale, is divided into 12 degrees, each identified by a Roman numeral. Modern seismographic systems precisely amplify and record ground motion (typically at periods of between 0.1 and 100 seconds) as a function of time. This amplification and recording as a function of time is the source of instrumental amplitude and arrival-time data on near and distant earthquakes.

Based on their magnitude, quakes are assigned to a class, according to the U.S. Geological Survey. An increase in one number, say from 5.5 to 6.5, means that a quake's magnitude is 10 times as great. The classes are as follows:
Great: Magnitude is greater than or equal to 8.0. A magnitude-8.0 earthquake is capable of tremendous damage.
Major: Magnitude in the rage of 7.0 to 7.9. A magnitude-7.0 earthquake is a major earthquake that is capable of widespread, heavy damage.
Strong: Magnitude in the rage of 6.0 to 6.9. A magnitude-6.0 quake can cause severe damage.
Moderate: Magnitude in the rage of 5.0 to 5.9. A magnitude-5.0 quake can cause considerable damage.
Light: Magnitude in the rage of 4.0 to 4.9. A magnitude-4.0 quake is capable of moderate damage.
Minor: Magnitude in the rage of 3.0 to 3.9.


Category
Strength
Occurence
Great
9.3
Sumatra 2004
Major
7.9
China 2006

7.0
Haiti 2010
Strong
6.3
New Zealand 2011
Moderate


Light


Minor



The largest earthquake ever recorded on Earth was a magnitude 9.5 that occurred in Chile in 1960, followed in size by the 1964 Good Friday earthquake in Alaska (magnitude 9.2), a magnitude 9.1 earthquake in Alaska during 1957, and a magnitude 9.0 earthquake in Russia during 1952. Two large earthquakes, one a magnitude 9.0 and one a magnitude 8.2, occurred on Dec. 26, 2004 and March 28, 2005, respectively, along the same fault zone off the coast of Sumatra, Indonesia.

A longer fault can produce a bigger earthquake that lasts a longer time.MagnitudeDateLocationRupture Length
(kilometers)Duration
(seconds)9.1 December 26, 2004 Sumatra, Indonesia 1200 500
7.9 January 9, 1857 Fort Tejon, CA 360 130
7.9 May 12, 2008 Sichuan, China 300 120
7.8 April 18, 1906 San Francisco, CA 400 110
7.3 June 28, 1992 Landers, CA 70 24
7.3 August 17, 1959 Hebgen Lake, MT 44 12
7.0 October 17, 1989 Loma Prieta, CA 40 7
7.0 October 28, 1983 Borah Peak, ID 34 9
6.8 February 28, 2001 Nisqually, WA 20 6
6.7 January 17, 1994 Northridge, CA 14 7
6.4 March 10, 1933 Long Beach, CA 15 5
5.9 October 1, 1987 Whittier Narrows, CA 6 3
5.4 July 29, 2008 Chino Hills, CA 5 1

The effects of an earthquake will be dependant upon where you live. we have seen over the years that a smaller earthquake, such as a 4.3 can be felt by those who live close to the rivers, in the floodplain, and not felt by anyone else. This is due to the geological makeup of the ground, nearest the river more sand and more shallow water tables. When earthquake vibrations pass through soil which has a high liquid water content, the soil loses the properties of a solid and takes on those of a semi-liquid, like quicksand or pudding, this process is called liquefaction. The foundations of heavy buildings suddenly lose the support of the soil, and they may topple, or settle deeper into the Earth.

Within the past 15 years building codes have become more strict. Those buildings built within this period will have a better chance of riding out an earthquake, however, this does not mean that it will not sustain any damage.

Sources:
consrv.ca.gov
geology.about
en.wikipedia
library.thiques
tremor.nmt
BookRags.com
bbc.co.uk
geo.mtu.edu
earthquakes
CBS News
visual.ly
japan-guide.com
dnr.mo.gov
pnsn.org
bigsiteofamazing
LifesLittle
scchealth.org
earthquake.usgs
answers.com
ScienceBreak
invetors.about
geography.inf
wanttoknowit
en.rian.ru
scign.jpl
en.wikipedia
buzzle.com

En rask metode for engelskspråklige læring basert på toppen tilbakevendende ord


En rask metode for engelskspråklige læring basert på toppen tilbakevendende ord

Hvert språk, inkludert engelsk er et levende vesen som vokser stadig, og skiftende, anskaffe nye ord hvert år. Noen av disse ordene kan være importert fra et annet språk, kan noen være fra samme språk, men med endret betydning og bruk gjerne ordet kule i engelsk for eksempel, mens andre ord kan være helt ekte. Dette skyldes det faktum påpekt av Shanon at kombinasjoner av et språk alfabetet ikke er fullt utnyttet.

Når det gjelder det engelske språket, er det funnet at på tross den økende størrelsen på leksikonet, de hyppigste ordene på engelsk er de samme.

Selv om, ble dette temaet mye dekket i litteraturen, gjorde vi et nytt besøk til emnet. Tretti bøker ble tatt som dekker flere fag. Disse fagene er: romaner, romere, historie, selvbiografi, psykologi, historier, geografi, poesi og andre emner fra nyheter på Internett.

Det totale antall ord anses overskredet 2.5 millioner ord. Våre funn som er oppført i følgende tabell er enig med tidligere studier og belyser forekomsten av de vanligste ordene på engelsk språk.

Totalt antall ord = 2586473

Tabell for valgte First Words, deres antall av utseende, og andelen av dette antallet som det totale antall ord i disse bøkene.


Antall Valgte First Words
Antall ord i Delsett
Prosent
30
685383
26.50
50
854403
33.03
80
996872
38.54
100
1063252
41.11
150
1177135
45.51
200 
1257791
48.63
250
1318285
50.97
350
1410478
54.53
500   
1509797
58.37
700
1606602
62.12
1000
1711982
66.19
1500   
1832929
70.87
2000
1920343
74.25
2500
1988075
76.86
3000
2042203
78.96
3500 
2086843
80.68


Fra tabellen er det funnet at de fleste tilbakevendende 50 ord utgjør 33% av det engelske språket, mens de første 250 ord utgjør mer enn 50% av språket.

Blant listen over de 100 mest hyppige ord i det engelske ordforrådet er restriktive føringer som bestemte artikler og eiendomspronomen pronomen samt preposisjoner, konjunksjoner, verb, hjelper verb og en rekke andre viktige deler av talen.

Tilsvarende er tallene en til seks, som fungerer som substantiv, pronomen og adjektiv, inkludert blant de 500 mest hyppige ord. Hjelpe verb også kalt hjelpepleiere, som inkluderer har, hatt, har og vil, var, er, var, etc., konsekvent rangerer blant de mest brukte ordene.

Internasjonale forskjeller mellom amerikansk engelsk, britisk engelsk og australsk variasjoner, påvirker ikke den hyppigste ordene på engelsk som er svært konsekvent.

I tillegg til ovennevnte, er det funnet at blant 30 disse bøkene inkludert ord som oversteg 2.5 millioner ord en betydelig mengde ord dukket opp bare én gang, to ganger, tre ganger, fire ganger, fem ganger, osv. Disse ordene og deres frekvens er notert i tabellen nedenfor.

Antall ord som finnes bare 1 til 7 ganger:


vises Bare n ganger

Antall Ord

1
24847
2
8388
3
4654
4
3056
5
2265
6
1729
7
1434



De faktiske forhold er beskrevet ovenfor er benyttet til å etablere en rask læring system for engelsk språk.

For å benytte dette systemet, abonnere. Du vil motta vårt nyhetsbrev på hva som kan kalles kunde utformet læringsprogram. Målet er å gjøre deg i stand til å erverve de første 1000 ordene som utgjør 66% av det engelske språket over en periode på 3 måneder, fordelt på 50 ord, 100 ord, 200 ord, osv. Nyhetsbrevet vil inneholde utvalgte topp ordene sammen med setninger med dem, og ordforrådet i disse setningene.

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