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根据大家的JJ找出的背景知识

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楼主
发表于 2003-7-30 12:05:00 | 只看该作者

根据大家的JJ找出的背景知识

Big eyed Bug Rearing


Natural History
Big-eyed bugs are true bugs in the order Hemiptera.  The two most common species are Geocoris pallens and Geocorcis  punctipes.  Both are predators and occur in many habitats, including fields, gardens, and turf grass. Big-eyed bugs are considered an important predator in many agricultural systems and feed on mites, insect eggs, and small insects such as pink bollworm, cabbage loopers and whiteflies.  Adult Big-eyed bugs are small (about 3 mm) black, gray, or tan with proportionately large eyes.  Eggs are deposited singly or in clusters on leaves near potential prey.  They develop with incomplete metamorphosis (there is no pupa) and take approximately 30 days to develop from egg to adult depending on temperature.  Both nymphs and adults are predatory, but can survive on nectar and honeydew when prey are scarce.  Big-eyed bugs, like other true bugs, have piercing-sucking mouthparts and feed by stabbing their prey and sucking or lapping the juices.  Although their effectiveness as predators is not well understood, studies have shown that nymphs can eat as many as 1600 spider mites before reaching adulthood, while adults have been reported consuming as many as 80 mites per day.

Rearing
Big-eyed bugs are easy to rear.  Adults can be purchased (see Suppliers) or collected in the wild by using a sweep net in a local alfalfa field, roadside or other lush area that may have potential insect prey.  A Petri dish provides adequate housing when a piece of paper towel or filter paper is placed in the bottom and cut to fit the dish.  Adults and nymphs should be housed separately as the larger individuals will eat the smaller ones.  If you plan on raising large numbers of them, you may want to invest the time in making an artificial diet (see Cohen in the References), however they will also do well with fresh insect eggs (purchased), whitefly nymphs or aphids provided every few days.  For moisture, place a one-inch piece of fresh green bean (replaced every couple of days) in the dish.  A small piece of cotton placed in the adult cage provides a place for oviposition as well as a hiding place.  eriodically remove the cotton from the cage (eggs are pale orange) and place it in a new cage with a fresh piece of green bean.  In a week to ten days, nymphs will emerge and a protein source (eggs, diet, etc...) will need to be added.  When cages become dirty or moldy, transfer adults and nymphs to a fresh cage.  Adults can be handled with soft forceps or with a small soft paintbrush.  Nymphs should be handled with a soft brush only.


沙发
 楼主| 发表于 2003-7-30 12:06:00 | 只看该作者
Giant Shield Volcanoes

The giant shield volcanoes on Mars are truly huge. The largest are three times as high as the biggest Earth volcanoes. They also are bigger in diameter. Thus, the biggest volcano on Mars is comparable to a pile of nearly 100 Hawaiian volcanoes. Despite this difference in size, the Mars shields look a lot like shield volcanoes on Earth. Both have the same broad flat profiles, large central calderas, and similar lava flow features. The giant martian shields are also much older than any Earth volcano. The youngest lavas on the martian shields are about 20 to 200 million years old. The oldest lavas are near 2.5 billion years old. Thus, these giant volcanoes were active for billions of years. This may explain their large size. On Earth, plate tectonics is always moving volcanoes away from their magma sources. Such movements are very slow, but they mean that most Earth volcanoes have distinct lifetimes. In the Hawaiian islands, for instance, volcanism lasts fo only a few million years on any given island. In contrast, the lack of plate tectonics on Mars allowed volcanoes to just keep growing. The only limit on their final size was the volume of lavas available.
板凳
 楼主| 发表于 2003-7-30 12:06:00 | 只看该作者
A Brief History of the Guitar

There is evidence that a four string, guitar-like instrument was played by the Hittites (who occupied a region now known as Asia Minor and Syria) around 1400 BC. It had characteristically soft, curved sides--one of the primary features of anything identifiable as a guitar or predecessor. The Greeks also produced a similar instrument which was later modified by the Romans, though both versions appear to have lacked the curved sides. What is interesting here is that it seems this Roman cithara appeared in Hispania (now known as Spain) centuries before the Moorish invasion.

It had long been assumed that it was only after this invasion and the introduction of the Arabic ud in the South that a guitar-like instrument first appeared in Spain. But with the Roman cithara arriving centuries prior, we might say that although the ud influenced the development of the guitar it is not the true ancestor. According to this theory, the Spanish guitar derived from the tanbur of the Hittites, kithara with a "k" of the Greeks and then the cithara with a "c" of the Romans.

However, following the arrival of the Moors, the Roman cithara and the Arabic ud must have mixed and exerted mutual influences on one another for many centuries. Although there is no specific documentation, it is likely that makers of uds and citharas would have seen each other's work, if only through presentation by traveling troubadours. By 1200 AD, the four string guitar had evolved into two types: the guitarra morisca (Moorish guitar) which had a rounded back, wide fingerboard and several soundholes, and the guitarra latina (Latin guitar) which resembled the modern guitar with one soundhole and a narrower neck.

In the late 1400's, the vihuela was born by adding doubled strings and increasing its size. It was a large plucked instrument with a long neck (vibrating string length: 72 to 79 cm) with ten or eleven frets and six courses. It was the vihuela which became the preferred instrument of the Spanish and Portuguese courts and remained so until the late 1600's when orchestral and keyboard instruments became more prominent.

Although the guitar existed concurrently during this period, the vihuela and lute had overshadowed it until the end of the 17th century when the lute had acquired too many strings, was too hard to play and tune, and the vihuela was slowly replaced by the four and five course guitars (which had seven and nine strings respectively: one single high string, and three or four remaining courses--or pairs--of strings). It was perhaps the addition of the fifth course in the late 16th century that gave the guitar more flexibility and range and thus improved the potential of the repertoire that led to its ascent.

By the end of the 18th century and the beginning of the 19th, some guitars already used six single strings and employed fan struts under the soundboard. These struts were added for structural support to allow thinning of the top for greater resonance and for better distribution of sound across the board. Other contemporaneous developments included the use of a reinforced, raised neck using ebony or rosewood for the fingerboard, and the appearance of machine tuners in place of the wooden pegs. (It is noteworthy that the raised fingerboard had a great impact on the technique of the instrument since the strings were then too far from the soundboard to rest one's finger on the face for support.) These guitars would be unmistakably recognized by us as early classical guitars.

Beginning with the early 19th century, in the works of Agustin Caro, Manuel Gonzalez, Antonio de Lorca, Manuel Guiterrez from Spain and other European makers including Rene Lacote, and Johann Staufer, we find the direct predecessors of the modern classical guitar. By 1850, the guitar was prepared for its most important breakthrough since its inception, the work of Antonio Torres Jurado. With the encouragement of Julian Arcas and his own brilliant intuitions, Torres refined the strutting of the guitar to include as many as seven struts spread out like a fan under the soundboard. He increased the body size and the width of the neck considerably. These improvements allowed for greater volume and bass response as well as the development of a left hand technique for richer repertoire. The guitar was now prepared for the demands of the solo performer and the concert stage.

Although there have been continued developments since the middle 1800's, our modern guitar retains most of what was developed nearly 150 years ago. No one can say if we have reached the end of the evolution of the guitar, but until now, many of the best guitars from the point of view of volume, projection and sheer beauty of tone were made by the great makers, Torres, Ramirez and Arias from the second half of the last century!



地板
 楼主| 发表于 2003-7-30 12:10:00 | 只看该作者


INSOMNIA

Self-Care Techniques
In addition to the wise use of supplements and maintaining a healthy lifestyle, there are a number of other methods you can adopt to capture elusive sleep. You may find one particular technique does the trick or that a combination of several works best for you.

ACUPRESSURE
Many of my insomnia patients report significant relief when they do acupressure self-massage. Stimulating specific points on your heel, wrist, and ankle can help to calm the nerves, relieve anxiety, and induce sound sleep. While you may feel immediately relaxed, it may take a month or more of doing acupressure daily to improve your troubled sleep patterns.

PROGRESSIVE MUSCLE RELAXATION
Both sleep researchers and the American Psychological Association have found progressive muscle relaxation to be beneficial for insomnia. In this exercise you learn what it feels like to relax by comparing relaxation with muscle tension. Deep breathing is also an integral part of the technique.
   
BACH FLOWER REMEDIES
Flower remedies are a very safe and natural way to treat the anxieties, stress, and depression that often underlie insomnia. Many brands of flower remedies are currently available, with virtually thousands of flower products from which to choose. I like the original extracts, known as the Bach flower remedies (named for Dr. Edward Bach, who originated the method in the early 20th century), which I find the most reliable.
There are 38 Bach flower remedies, each one intended to treat a different negative emotion. For my patients struggling with insomnia, I often recommend white chestnut and scleranthus. White chestnut helps to chase away those obsessive worries that can keep you awake, while scleranthus dispels feelings of uncertainty and indecision. Other Bach flower remedies you might try are vervain, which fights tension; vine, to tackle the torments of ambition; and elm, to combat the sensation of being overwhelmed by responsibilities.

   
LIGHT THERAPY
Our bodies have their own internal clocks called circadian rhythms, and when we tamper with them by flying across too many time zones or shifting working hours (or spending too much time indoors), they react by pulling the rug of sleep from under our toes.
While natural daylight is still the best therapy for light-deprived sleep disorders, such as jet lag, the sun is not always there when you need it. Therefore I often suggest a light visor for my patients whose insomnia is caused by long-distance travel or shift work.

A light visor is fitted with a high-intensity full-spectrum bulb and worn on the head like a tennis visor. Unlike its big brother the light box, the visor can be worn around the house while you do other things, and be stowed in a backpack or purse for traveling. Many people find that while flying across times using a light visor to read helps to reset the body's biological clock even before the plane lands. (The directions that come with the light visor should clue you in on how to use the device during travel.)

Studies also show that light therapy is very effective for those who can't fall asleep at night or who tend to wake up too early in the morning—a typical sleep pattern in older people.






[此贴子已经被作者于2003-7-30 12:11:23编辑过]
5#
 楼主| 发表于 2003-7-30 12:13:00 | 只看该作者
不是给GOOGLE做广告,都是用它搜索出来的。
6#
发表于 2003-7-31 07:52:00 | 只看该作者
我也覺得gogle很讚,找不到的東西,去google就對了
謝謝luoluo11 MM !
7#
发表于 2003-7-31 08:56:00 | 只看该作者
Olympus Mons is the largest volcano on Mars. This shield volcano, similar to volcanoes in Hawaii, measures 624 km (374 mi) in diameter by 25 km (16 mi) high. It is 100 times larger than Mauna Loa on Earth. Located on the Tharsis Plateau near the equator, Olympus Mons is bordered by an escarpment. The caldera in the center is 80 km (50 mi) wide and contains multiple circular, overlapping collapse craters created by different volcanic events. The radial features on the slopes of the volcano were formed by overflowing lava and debris.
This 3-dimensional image was created from several images of Olympus Mons. Each image was taken from a different spacecraft position and combined with a computer model of the surface topography to generate a perspective view. The final mosaic shows Olympus as it would be seen from the northeast. It's possible that volcanoes of such magnitude were able to form on Mars because the hot volcanic regions in the mantle remained fixed relative to the surface for hundreds of millions of years.
8#
发表于 2003-7-31 11:07:00 | 只看该作者
哎呀,太爱你们了,省了我不少时间呢。谢谢!
9#
发表于 2003-7-31 11:30:00 | 只看该作者
我听的那个关于mars上火山的例子是Olympus Mons 火山,说的全是Olympus Mons ,说它是
mars上最大的火山,还有那个big eye bug,吃一种叫***-spider的虫子,题目里会出现,问关系,大眼睛吃***-spider的.
10#
发表于 2003-7-31 12:24:00 | 只看该作者
Olympus Mons, a gigantic (about 600 km/375 mi in diameter) shield volcano on Mars, is larger across than the length of the Hawaiian Islands strung together. The Mars Pathfinder Mission of 1997 returned data that Martian volcanic rocks appear to be similar to those found on Earth, including some evidence of the rock andesite. The volcanism on
加一下^^
the Earth's moon, Mars, Mercury, and Venus mostly occurred billions of years ago; these planetary bodies are now cold and dead. However, scientists have found evidence in Martian meteorites that indicates volcanic activity on Mars may have occurred as recent as 150 million years ago.

Mars has the largest volcano in the solar system, Olympus Mons. It is 26 km (16 mi) high (almost twice as high as Earth¡¦s Mount Everest) and covers an area comparable to the state of Arizona. Near it, three other volcanoes almost as large¡XArsia Mons, Pavonis Mons, and Ascraeus Mons¡Xform a line running from southwest to northeast. These four volcanoes are the most noticeable features of a large bulge in the surface of Mars, called Tharsis. Another volcano, Alba Patera, is also part of the Tharsis bulge, but is quite different in appearance. It is probably less than 6 km (4 mi) high, but has a diameter of 1,600 km (1,000 mi). None of Mars¡¦s volcanoes appear to be active.

The Tharsis bulge has had a profound effect on the appearance of the surface of Mars. The Tharsis bulge includes many smaller volcanoes and stress fractures, in addition to the large volcanoes. Its presence affects the weather on Mars and may have changed the climate by changing the rotation of the planet.

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