I am a TGV – a very fast train

by | Feb 17, 2013 | France

I am TGV – a very fast train
The TGV (French: Train à Grande Vitesse, meaning high-speed train) is France’s high-speed rail service, operated by SNCF Voyages, the long-distance rail branch of SNCF, the French national rail operator.

TGV was developed during the 1970s by GEC-Alsthom (now Alstom) and SNCF.  Although originally designed to be powered by gas turbines, the TGV prototypes evolved into electric trains with the petrol crisis of 1973.  Following the inaugural TGV service between Paris and Lyon in 1981, the TGV network, centred on Paris, has expanded to connect cities across France and in adjacent countries.
A TGV test train set the record for the fastest wheeled train, reaching 574.8 km/h (357.2 mph) on 3 April 2007.  As of mid 2011, scheduled TGV trains operate at the highest speeds in conventional train service in the world, regularly reaching 320 km/h (200 mph) on the “LGV Est”.

The success of the first line led to an expansion of the network, with new lines built in the south, west, north and east of the country.  Eager to emulate the success of the French network, neighbouring countries such as Belgium, Italy, Spain and Germany built their own high-speed lines.

In 2007, SNCF generated profits of €1.1 billion (approximately US$1.75 billion or £875 million) driven largely by higher margins on the TGV network.

On 28 November 2003 the TGV network carried its one-billionth passenger, second only to the Shinkansen’s five billionth passenger in 2000. The two-billion mark was reached in 2010.

The newest high-speed lines allow speeds of up to 320 km/h (199 mph) in normal operation. Originally, LGVs were defined as lines permitting speeds greater than 200 km/h (124 mph); this guideline was subsequently revised to 250 km/h (155 mph).  Like most high-speed trains in Europe, TGVs also run on conventional track (lignes classiques), at the normal maximum safe speed for those lines, up to a maximum of 220 km/h (137 mph).  This allows them to reach secondary destinations or city centres without building new tracks all the way to the station, reducing costs compared to magnetic levitation trains or high-speed networks with a different gauge than the surrounding conventional network (as in Japan or Spain).

TGV track construction is similar to that of normal railway lines, but with a few key differences.  The radii of curves are larger so that trains can traverse them at higher speeds without increasing the centripetal acceleration felt by passengers.  The radii of LGV curves have historically been greater than 4 km (2.5 mi). New lines have minimum radii of 7 km (4.3 mi) to allow for future increases in speed.

Track alignment is more precise than on normal railway lines and ballast is deeper.  LGV track is anchored by more sleepers per kilometre than normal and all are made of concrete.  Use of continuously welded rails instead of shorter, jointed rails yields a comfortable ride at high speed, without the “clickety-clack” vibrations induced by rail joints.

Because TGVs on LGVs travel too fast for their drivers to see and react to traditional lineside signals, an automated system called TVM, “Transmission Voie-Machine” or track-to-train transmission, is used for signalling. Information is transmitted to trains by electrical pulses sent through the rails, providing speed, target speed, and stop/go indications directly to the driver via dashboard-mounted instruments. There are safeguards that can safely stop the train in the event of driver error.

The line is divided into signal blocks of about 1500 m (≈1 mile) with the boundaries marked by blue boards with a yellow triangle. Dashboard instruments show the maximum permitted speed for the train’s current block and a target speed based on the profile of the line ahead. The maximum permitted speed is based on factors such as the proximity of trains ahead, junction placement, speed restrictions, the top speed of the train. Because trains cannot usually stop within one signal block, drivers are alerted to slow gradually several blocks before a required stop.

Shield Shrimp

When it rains across Australia’s vast inland region, temporary pools crop up all over the arid ground, giving life to a strange desert crustacean known as the shield shrimp (Triops australiensis).

Named after the formidable carapace that shields its head and upper body, T. australiensis can grow up to 7.6 cm long, and it uses its long, segmented tail and mass of 60 or so legs to propel itself through shallow water.

It also breathes through these legs – its sub-class Branchiopoda means ‘gill-legged’ – and in the females these legs bear ovisacs for carrying their tiny eggs.

Several pix in the Photo Gallery and a movie.

Acacia peuce

A rare and endangered plant. The tree grows up to 15 to 18 metres (49 to 59 ft) high, with short horizontal branches and pendulous branchlets covered in needle-like phyllodes adapted for the arid dry climate. It has a distinctive habit more similar to a sheoak or a conifer.

Although speculated to have been widespread across central Australia during wetter climates 400,000 years ago, the population is now mostly restricted to three sites, separated by the encroaching Simpson Desert. In the Northern Territory, the species is restricted to the Mac Clark (Acacia peuce) Conservation Reserve which is surrounded by a pastoral lease, Andado Station. The other two sites are near Boulia and Birdsville in Queensland. The tree is found in open arid plains that usually receive less than 150 millimetres (5.9 in) of rain per annum. They grow on shallow sand aprons overlaying gibber or clay slopes and plains and between longitudinal dunes or on alluvial flats between ephemeral watercourses.

 

Owen Springs Reserve on Hugh River

Owen Springs was a station on the Hugh River. The Hugh River flows into the Finke (when it actually flows). Both cut through the Western MacDonnell Ranges. The image above shows Owen Springs Reserve as a dot at lower right. The river it is next to is the Hugh. Hermannsburg, our next town, is near middle left edge. Hermannsburg is almost on the Finke River. You can see both Hugh and Finke Rivers cutting through sections of MacDonnell Ranges.

Palm Valley

Palm Valley is within the Finke Gorge National Park southwest of Alice Springs. Palm Valley has a smallish population of Red Cabbage Palms (Livistona mariae). The nearest related species is 850 kilometres away in Katherine NT. The average rainfall for Palm Valley is just 200 mm per year. Small pockets of semi-permanent spring-fed pools allow the unique flora and fauna (desert fish, shield shrimps tadpoles and frogs) to survive.

It had been assumed that the cabbage palms were remnants of a prehistoric time when the climate supported tropical rainforest in what is now the arid inland of Australia. Genetic analysis published in 2012 determined that Livistona mariae at Palm Valley is actually the same species as Livistona rigida from samples collected near Katherine and Mount Isa, both around 1,000 kilometres (620 mi) away. It is now thought that aboriginal people brought the palms to here from Mataranka.

Mound Springs

Mound Springs occur around the Western edge of the Great Artesian Basin and represent a natural discharge of Artesian water that was captured many hundreds of kilometers away from rain falling along the Great Dividing Range and New Guinea. This article provides details. Dalhousie is an excellent example of a mound spring.

Great Artesian Basin map Great Artesian Basin diagram