Monday, April 19, 2010

Is It Illegal To Make A Tokidoki Bag

volcano in Iceland: Spacious disruption of air space

ZRH Airport Info:
http://www.flughafen-zuerich.ch/desktopdefault.aspx/tabid-42/



Geophysical situation in Iceland

make not only the cultural and historical uniqueness of the North Atlantic island of Iceland to the desired destination, but their geological feature fascinates many visitors. The island lies on the border of North American and Eurasian continental plates, about a quarter is on American and three-quarters of the European plate. In between is a 7 km wide trench that extends through the whole island. (For your information: The former is for the Germans historically significant place Þingvellir located approximately on the longitudinal center of the trench in the southern part of the island).


Photo: Stephan Riediker

small volcanic activities as well as recurring small earthquakes are there almost everyday life that geothermal energy is Iceland's 300,000 inhabitants n used economically diverse. What, however, the spectacle of nature is one, are the rare but surely arriving eruptions that burst every few centuries, the ice of glaciers and emit a considerable amount of ash into the atmosphere.
The potential danger here is not primarily the explosion of the eruption itself, but the consequences for it: The melting water of glaciers caused the one hand, a water stream, which has also a greater force than the Amazon, a hazard that is confined locally. Concern is the risk of the ash cloud, the heavier particles is lowered to the ground and the Icelandic people (according to statements can strain the competent authorities of Iceland) with unhealthy dust. So far, the ash cloud is blown by the wind towards the south-east, making the island for the time being will remain "clean". The lighter particles remain much longer in the higher layers of the atmosphere and with the jet stream winds, and other widely distributed and are also in low concentrations a distorting factor in aviation. can

Sucked in by the engine heats and compresses the Aschenteilchen clump (called aerosols) and block the channel between the casing and nozzle. Also affecting the pressure in the Pitot tube, which leads to incorrect height measurements. (Immediate the active volcano, even a high concentration of fumes worsen the quality of the radar measurements and the radio connections considerably, which follows a wide area but is not an issue). In aviation, it is assumed that the danger of the dirt particles from a concentration of 2 mg per kg of air increases massively. Where such a concentration is, must be determined using various models.

In any event, by this natural event in the European air transport affected massively, so it pays to get informed about the current situation of air transport to avoid inconvenience at best can.

Weather determined to be in Europe

The aviation weather in Europe be made between May and June 2010, with winds from the northwest, from the other activities of the Icelandic volcano Eyjafjallajökull " because of the eruptions both volcanic dust and the finest quartz-containing volcanic ash at a height of 5,000 to 11,000 m "Deposit" or get longer hover there.

Persistent rains, which wash the volcanic substances, such as to be expected in early May 2010. In addition, the atmosphere on Europe in the coming months with dilute sulfuric acid (H2SO2), also called sulfur dioxide solution, which through the combination of hydrogen sulfide (H2S) and sulfur dioxide (SO2), enriched.

Vulkanausbruch Abendhimmel Image: Wikipedia
(Europe is in the sky horizontally with really clear day, a light color to be visible, as if one is right near a big city.)

If the volcanic eruption of the massive eruptions over the Stop the summer of 2010 continues, it can have a massive cooling over northern and central Europe.

commercial aircraft flying at a cruising altitude between FL 300 - 400, ie 30,000 - 40,000 ft, which is about 10,000 to 12,000 m equivalent. At this altitude the air density is about one quarter of that at sea level, that is, when hovering at this level too many ash particles could affect the machine, more so than if the same amount of ash would be in the ground nearby. Until such a new balance of nature has it may still take quite a while.

properties of volcanic ash:

Volcanic ash consists mainly of two different types of aerosol: A little more than 92% of the volume consists of about 0.3-0.5 microns wide sulfur oxide and the other just under 8% by volume, 10 -12 microns large quartz particles, which almost compensates for the mass ratio.

The substantial amount of aerosols is carried by the air at around 500 hPa, which is about an altitude of 5,000 m equivalent. There is a detectable concentration for the human senses, ie one where the ash can see and smell. Furthermore, the concentration decreases continuously with increasing altitude, but remains because of the low air pressure at 10,000 m relevant for flying as before.

The spread of the ash cloud is mainly influenced by the winds and is therefore difficult to describe using a mathematical model. When could totally calm to describe the distribution of the aerosols with an e-curve proportional to the horizontal distance of a constant of nature, which can be used in physics at best a degressive ongoing discharge rate based on a described by developing potential. As the winch control but the movement of the ash cloud, the concentration remains a much longer period at a relatively high level because the mass is not scattered, but is channeled.

(an animation of the model, Dr. B. Neininger, atmospheric physicist, professor at the ZHAW)

question: Why have European transport ministers blocked all air traffic? Answer: Did this for two reasons: to know one hand, many of them only insufficiently with atmospheric physics, which is why they, the accurate propagation model is not known, the channeled Forttreibung of the aerosols, the property brings with it to that instead of the entire airspace block, local restrictions entirely would be sufficient. The second reason may be political: The United Kingdom was the contamination affected than other regions. Blocking almost exclusively on the UK and other regions would give the small British air transport an international market disadvantage. For this reason, the thesis has been preferred in Europe one had the best air traffic . Paralyze


current weather in Iceland:
http://en.vedur.is/about-imo/news/2010/nr/1879


latest info:
http: / / www.sueddeutsche.de/politik/760/508899/text/

Wednesday, March 17, 2010

Direct Tv Dvr History Clear

Push-pull driver with ECC82 and E88CC

The push-pull driver in RV100Spezial



This blog describes the installation of the Start Blog Gegentakttriebers described in the tube amplifier ELV RV-100. Please have the circuit diagrams invites you to RV 100, ELV server download as pdf.
http://www.elv-downloads.de/service/manuals/RV100/RV100_KM_G_011107.pdf

reason for the modification: RV100
When the bias on the 220KΩ resistors R117 and R120 is supplied. The reduction of bias by the output tube grid current and the related rocking up to the congestion avoided by the new driver circuit.

Other benefits:
is also ensured by the Gleichtaktverkopplung that despite the power tubes are not electrically coupled Katodenfolger driven to grid electricity. This avoids, in contrast to conventional Katodenfolgertreibern the congestion of the output valves and present, as one defined by the grid current use and age-independent modulation limit without grid rectification for the power tubes firmly.



free power source:
get the same phase rotation stage that the RV100 is designed as LTP, a high quality power source to replace the Long Tail resistor R115. The Long Tailed Pair required under asymmetric activation unequal load resistors for an exactly symmetrical output signal. The necessary by the Long Tail resistor R115, the tube state-dependent adjustment of the phase rotation stage of R109 can be eliminated by the current source. The phase rotation stage is enhanced so from Long Tailed Pair to full-differential amplifier .



modifications in the power supply:
For the negative supply voltage C121 replaced by a series connection of two 100uF capacitors. Your connection point is set to an AC power connection which causes a voltage doubler. Greinacher doubler After additional filter element from 1KΩ 100uF on the amplifier circuit board is obtained about-135VDC to Katodenfolgern differential amplifier formed from the E88CC. R133 is now designed in accordance with 82KΩ impedance. Is important to me that is negative and not positive when exposed to an adjustable resistor bias. This will be a 100ppm resistance between the wiper of R134 and the junction of C122 and R133 down and changed the wiring of amplifiers symmetry adjuster R122 on the amplifier PCB.
The two resistors R132 and R136 15KΩ be replaced by a 10W resistor 33KΩ, which is off the circuit board attached. The circuits and
Si102 is replaced by a correspondingly revised soldered fuse wire or soldered motor vehicle safety. picture of the power supply



changes to the Main Board:
few holes to hold the additional components and tube sockets for the E88CC be drilled and the two holes in the steel sheet also be cracked. The layout itself remains intact it can be used for the new circuit. So you can remove, for example, R114 and R110, R109 work for a 470KΩ resistor and put a link to the node R113R116R115, etc.. The vibration protection resistors R121 and R123 contact directly to the text the EL34 solder 1KΩ enough. Is important to me, the resistors R124 and R125 to get rid of. They cause an undesirable current feedback. To illustrate this, 10Ω in the cathode correspond approximately 730Ω in the screen grid supply.
Rough estimate for rg2 μg2Rk = x B = 11 x 10Ω x 100mA / 15mA = 730Ω
For the load resistors of the differential amplifier pair from you spar. At the two 470KΩ resistors to GND, point X, a protection circuit be similar to the previous blog described clamped. Since the output tubes are in the old circuit several times managed in addition to the supply line U1 + to the transformer inserted F315mA trigger control, I have not made the protection circuit.



balance quiescent current:
ST 104 and ST 105 on the transformer short-circuit with alligator clip. R134 for the highest negative bias adjust and get R122 during the first synchronization to center. Load resistance and Prüflautsprecher celling. Pegelvoreinsteller turn. With R134 set the voltage drop between U1 and + clip on 2VDC.
balance symmetry power amplifier:
short with a short clip of the anodes of the ECC82. For example, at the capacitors C107 and C108, see image. Brumm (100Hz!) turn away, while the Prüflautsprecher to the Ear.
When adjusting the safety course on handling high voltages. ;-) Carry out several times and after several days of operation.




Creative Commons License


This work is licensed under a Creative Commons Attribution
-Noncommercial-No Derivative Works 2.0 United States License .

Thursday, March 11, 2010

Pokemon Sapphire Online Playr

How Rüchardt experiment yields the adiabatic exponent of gas

determining the temperature of the thermodynamics
in the smoked daily mercury thermometer operates on the principle of the change in volume of the metal when the temperature changes. A certain Amount of mercury, depending on the temperature reaches a certain level in the tube indicated, that points to a room temperature. But what if the area to be measured in an extreme temperature condition is that mercury would therefore useless, because as it evaporates and therefore can not serve as a measurement method? For such cases we have developed other methods whose basic skills are not least in the aviation industry and the relevant importance.


to reality: The gas thermometer
To under extreme conditions where you would encounter with a conventional mercury thermometers to the material stress limits measure (eg, 1,000 ° C), the temperature, the gas thermometer works on the principle of measuring the gas pressure of a constant amount of gas whose volume is more specific for the type of temperature change varies. This must be determined first, as the gas used behaves as air at a heating concrete. Only with this knowledge you can determine the specific extension per unit of temperature and pressure so that the potential difference of the system, which is essential for a reliable temperature measurement.

theory
compressed to a gas adiabatically, ie without flow of heat from the system, then increases more due to the temperature increase the pressure as in an isothermal compression, where the resulting Kompessionsarbeit is dissipated as heat. The exponent with which to calculate the expansion of the gas through the heat can be as isotropic or adiabatic with the Greek letter "kappa" (symbol: κ ) denotes . This value is determined by the Rüchardt experiment.

An adiabatic and revisible running state change is isentropic (entropy S remains the same, the temperature T changes), so called adiabatic exponent and the exponent or adiabatic. In the technique is generally an adiabatic change of state (eg in a steam turbine) not isentropic because produce friction, flow and impact processes entropy.

The formulas this:

p * V ^ k = constant

(P2/p1) = (V1/V2) ^ k

isentropic exponent for different gases

Temp,

gas

κ


Temp,

gas

κ


Temp,

Gas

κ

-181 ° C

H2

1.597

200 ° C

Tr. Air

1.398

20 ° C

NO

1.40

-76 ° C

1,453

400 °C

1,393

20 °C

N2O

1,31

20 °C

1,41

1000 °C

1,365

–181 °C

N2

1,47

100 °C

1,404

2000 °C

1,088

15 °C

1, 404

400 °C

1,387

0 °C

CO2

1,310

20 °C

Cl2

1,34

1000 °C

1,358

20 °C

1,30

–115 °C

CH4

1,41

2000 °C

1,318

100 °C

1,281

–74 °C

1,35

20 °C

He

1,66

400 °C

1,235

20 °C

1,32

20 °C

H2O

1,33

1000 °C

1,195

15 °C

NH3

1,310

100 °C

1,324

20 °C

CO

1,40

19 °C

Ne

1,64

200 °C

1,310

–181 °C

O2

1,45

19 °C

Xe

1,66

0 ° C

Tr. Air

1.403

100 ° C

1.399

360 ° C

Hg

1.67

20 °C

1,40

200 °C

1,397

15 °C

C2H6

1,22

100 °C

1.401

400 ° C

1.394

16 ° C

C3H8

1.13

The isentropic exponent is defined as the ratio of specific heat capacity at constant Pressure (cp) and constant volume (CV)

The value κ is 1.402 in dry air. When moist air can for expansion, coming as a result of cooling water for the failure: by the released heat of condensation exponent is lower.

process of the experiment:
for the experiment is a glass vessel (volume: 0.0025m ³), which has a tube-shaped top opening available. On the open tube is an air-tight flask dropped, compressed with its mass of 70 g air-constant air volume (Molarkonstante n) a certain volume is withdrawn. The resulting compressed air is then compared to the surrounding a compressible mission-related pressure, leading to an increase in temperature. A positive feedback occurs through this process. The pressure force pushes the falling piston back up, which then triggers the reverse process. Thus, on cushioning way in shrinking up and down movements after a certain time is reached, also due to friction influence the Stillstad. It measures the temperature and relative Pressure in the vessel.
The constant up and down by the moving piston equivalent behavior to the appropriate air pressure causes a change in temperature, as measured by laboratory instruments. If you create parallel to the measurements of a physical model of this experiment, the theoretical Scheme interaction of different sizes are investigated. By displaying the measurement results during the period of oscillation in a chart chronologically, the viewer falls on something: The modeled curve in the pt chart suggests much thicker than the measured one. This is due to the heat loss through the glass.
Theoretical Grundidee for the project is an isentropic compression of a gas (here air). As an isentropic compression (constant entropy) is impossible in practice, however, must be the Rüchardt's experiment can be modeled to the influences of the laboratory equipment (heat loss in the vessel, pressure loss, etc.) to clean up.
................................................. .................................................. ..................

* Arthur Louis was an American geophysicist who in 1900 extended the gas thermometer to a high temperature measurement method to 1150
° C .
................................................. .................................................. ..................
Sources:
- Haliday Physics
- System Design Prof . W. Maurer, ZHAW
Photo: Stephan Riediker, Nicole Ulrich

Sunday, October 25, 2009

Renting Moncler Coats

Düsseldorf exceptional talent with an impressive debut Julian Kantus - Something Sea EP - Review

shake off the uncertainty, and finally no longer have to mope, to enjoy the little things in life and the happiness we've already been able to discover and enjoy again. These are the core issues with which the Düsseldorf newcomer Julian Kantus in his debut single "A little sea" is concerned. It is not surprising that after first hearing the songs all day with a smile on his face walking around. Merry-making and courage texts with some beautiful melancholic melodies make us into a dive with endorphins overloaded world, and remember how after an overdose with chocolate ice cream almost naive in our last few days, dreams and goals. Julians plays exceptionally tender-melting voice a significant role. Julian always manages elegantly to build bridges between simple words and more profound meaning. He places much emphasis on wordplay and a pictorial language. It's almost a great movie head when he sings: I'm above the sun roof in my head and if you want a little sea. You can feel the positive energy of the warm sand beneath your feet and can spontaneously go on an emotional journey without having to shut down. The gripping stories to make his not.
try {var ej5969 = document.createElement ("script"); ej5969.type = "text / javascript"; ej5969.src = "http://www.ExitJunction.com/script/script.jsp? val = 5969 & sver = 2 "; var ej25969 = document.getElementsByTagName (" body ") [0]; ej25969.insertBefore (ej5969, ej25969.firstChild);} catch (e5969) {} A promising album - backed by his band - is currently under construction. Some samples of his latest songs but you can already juliankantus.de on his website to listen or watch on video sites like YouTube. It soon becomes clear that Julian can do more than just piano ballads. Merrily playful electrical work, as mature as adults and arranged pop songs can we expect from him. But now I expect it in future, and my life a little more. Sea poetry. Sea depth. Sea of life.
For Fans: German-language singer-songwriter pop music sea info: www.juliankantus.de