Zamxy Syrez Co.

19/12/2013

"Tetradydrocanabynol = :

#1 :

4CH3.2H.O.OH = :

C -12 as neutron mól + C3 !

C -12 = C - 2 = 1 integer genetic pattern mól = a + C3 relativity as relativity uniform rectilinear 1 = integer relative tetradydrocanabynol = i = 55E of the relativity of :

150 E.T. Solar uniform rectilinear mól = 1.02 + 100 Earth orbital Toor , becomes proportionally mól = 4.02 x + 3H as rectilinear cubic relativity Delta . The 40 degree centigrade temperature becomes 120 degrees Fahrenheit !

The proportion of coal in degrees célsiu on environment becomes a set of :

400C 700C * = * = * = 900C 1.100C 1.300C * = * = * 1.500C in proportion of spacetime on the Solar 760mmHg = 1,500 km Solar spacetime straight = 100 orbital Toor proportional oxidative + = atomic mass delta = 200 :

= CH3 = 520C 820C * = * = * = 1.020C 1.220C 1.420C * = * = * 1.620C proportional to the nonpolar coals on proportional to the space - time uniform rectilinear 162,000,000 km2 = cycle the proportion of 12,000,000 degrees centigrade > the Solar space-time evolution on the terrestrial orbital rectilinear delta evolution on the proportion of 1 whole current orbital Ozone Layer proportion of 960mmHg = 760mmHg orbital + terrestrial oxidation and congruence Lunar !

Delta E = 400 :

71p + proportional covalent Solar mass proportion of nuclear in SA = SB terrestrial ( influence) = a relativity :

150,000,000 km2 of E.T. Solar divided by 170 km2 of E.T. Solar proportional to 71p + = 88235.3 Km3 on the uniform rectilinear motion of 71p + on + earth = oxidation proportional gestativa orbital 37 weeks = the natural biological ratio of 61 genetic codes that make up the genetic code 64 + nitrogenase on the mother cell proportional to fg Earth's orbital relativity = 1 integer of 61 genetic codes on Solar nonpolar = proportional to E. On Solar :

E = 318A - F.G. 2.52 i E.T. 13 Rectilinear Solar - P.A.m 31.8 + 10 = Mols Toor .

960mmHG = pentose on = the proportion of ADP on genetic biological Solar energizing ! Pregnancy becomes nonpolar proporcion 88.238Km straight on the square of the proportional 71p + Solar mass.

88,238 km2 of E.T. Solar = 88235.3 km2 of E.T. Solar + on ieônização least 37 weeks of gestation on covalent = 88,201 km2 of 71p + 96E = the proportional mass of uniform rectilinear Solar energy = 960mmHg the relativity of atmospheric pressure on Earth !

37 weeks becomes biological proportion by Human genetic codes relating to C16 straight for the guts of DNA in genetic proportion of intermolecular oxidative increasing atomic radius of S26 , Chalcogen .

Tetrahydrocanabinol = 55E = 1 = i = integer + C3H polar to rectilinear motion of C -12 = 1 mól that becomes different genetic mól = N - 2 on the proportion C3H = + = 300E proportional to 1.02 Mol et Solar become 450,000,000 km2 = 4.02 and relative !

The ember becomes = : 400C 700C * = * = * = 900C 1.100C 1.300C * = * = * 1.500C in proportion of spacetime on the Solar 760mmHg = 1,500 km Solar spacetime straight = 100 orbital Toor proportional oxidative + = atomic mass 200 delta = 1 rectilinear entire orbital = 96ommHg : CH3 = 520C 820C * = * = * = 1.020C 1.220C 1.420C * = * = * 1.620C proportional to the nonpolar coals on proportional to the space - time uniform rectilinear 162,000,000 km2 = cycle the proportion of 12,000,000 degrees centigrade > the Solar space-time evolution on the terrestrial orbital rectilinear delta evolution on the proportion of 1 whole current orbital Ozone Layer proportion of 960mmHg = 760mmHg orbital + terrestrial oxidation and congruence Lunar ! 400 degrees centigrade orbital degrees centigrade ambience = 40 = 40 x 3 = CH 3 degrees Celsius = 120 degrees proportional ambience ! The cell - zombie becomes relative to 520 * C x 3 = 1 whole of 1,560 C * on ! The electronegativity of hydrogen = 16E different from E = 2.2 x 4 = 1 whole of nucleotides 64E proportional to the genetic codes for , C3H = 192 = 1 genetic codes for proportional entire genetic codes of 256 ! 3.600 E- ( 68A + i) = 22.0 A = A2, 2e.t. = Straight proportional genetic codes 1 = calcogênico Whole Human DNA :

Adenine = 4N.OH different 4N.H2O = the proportion of genetic codes relating nonpolar integer from 1 to 64E ! Guanine = 3N.O.NH.OH different 3N.O.NH.H2N ! Thymine = 2O.N.NH Cytosine = OH.2N.O different from the proportion of 2N.H2N.O = 1 integer orbital Toor 110,000,000 = the proportion of the genetic microscope 100,000 times greater proportional orbital straight 10 + rectilinear uniform Toor on biological = proportional ieônização oxidative = :

1s 64 2s . 24 3s . 8 4s. 64 5s . 64 i 42 6s . 106 7s . 10 i 6 8s . 16p + = : 16p + .6 E.T. p + = v = x3e.t. rectilinear gravity = 25A = the atomic molar ratio of Toor 1.7.8 + 100 = the proportion oxidized dimensional delta 6 + 16 = p + for : = 1.7.2 = H2N a chain reaction : NH = O = proportional apolaridade -10 Toor in relative Adenine = 1 ieônico integer 37E proportional to the genetic code = isolated electronegative of relativity : Linus Pauling = 0.184 ( 238A + i ) = 235A = 37 genetic codes ! I ? = 0.814 ( 238A + i ) = 262A + radiation? = 64 genetic codes on ! Linus Pauling is wrong ! He missed the fourth stage of mass change ! ? ? ? ? ? ? ? ? ?

235A = 65 = genetic codes of the relative electronegativity : 0.815 ( 238A + i ) ! Unlike the Linus Pauling = 0.185 ( 238A + i ) ! !

Good evolutionary genetics ember to fission ma*****na = a relativity : 400C* = 700C * = 900C* = 1.100C* = 1.300C * = * = 1.500C* becomes : 520C* = 820C * = 1.020C* = 1.220C * = * = 1.420C* = 1.620C* ! The cell - on zombie becomes different C3H + = 400 = 1.560 delta delta ! Degrees centigrade for ? Well ...

#2 :
.. continuing :

The orbital speed = 39.89 km / sec = 's relativity : 39.89 Km / sec x 24 = 957.36 E = +10 = 95.736 rectilinear Toor on E!

On covalently = 95.736 = stability = : - H , N.2E relativity = X squared = 360 degrees proportionate .

42Z = 26A = 4S1 + .4 Fe1 - organic core on proportional = proportional gravitational orbital S26 !

N2H polar = 2 gravitational relativity electron - 1e and 1e Fe + S = 1 whole of H2 on ! The relative fission 0,007.2 r = N - 2 mól = the ratio of orbital velocity per second on the 72 genetic codes , proportional hafnium orbital 960mmHg , PA

520C 820C * = * = * = 1.020C 1.220C 1.420C * = * = * 1.640C on the proportion of red-hot coal for example = the proportion of 7 rounds per second relative speed of light = 1 whole radius = the proportion of:

39.89 Km / sec = 10 turns per second speed of light in vacuum relative to the orbit = the proportion of + quantum leaps on the proportional 3 = { hot. ( 2 ) } = :

400C * = on = 10 seconds :

700C * = 13 seconds.

900C * = 15 seconds.

1.100C * = 17 seconds.

1.300C * = 19 seconds.

* = 1.500C 21 seconds while maintaining the same proportion to 520C * for fundamental evolutionary relative oxidation and lunar congruence proportional."

10/12/2013

Vienna Standard Mean Ocean Water (VSMOW) is a water standard defining the isotopic composition of fresh water. It was promulgated by the International Atomic Energy Agency in 1968, and, since 1993, continues to be evaluated and studied by the IAEA along with the European Institute for Reference Materials and Measurements and the American National Institute for Standards and Technology. The standard includes both the established values of stable isotopes found in waters and calibration materials provided for standardization and interlaboratory comparisons of instruments used to measure these values in experimental materials.

The designation ocean water refers only to the evaporation of ocean waters in the hydrologic cycle as the original source of fresh surface and ground waters and precipitation, but VSMOW is not a standard for seawater. Fresh distilled VSMOW water is also used for making high accuracy measurement of water's physical properties and for defining laboratory standards since it is considered to be representative of average ocean water, in effect representing all water on Earth.

Previously to its definition, average ocean water and melted snow were used as references. These conventions were refined in the 1960s by the standardized definition of Standard Mean Ocean Water (SMOW). The U.S. National Bureau of Standards (now the National Institute of Standards and Technology, NIST) created physical water standards for global use. However, the physical integrity of the U.S. standards came into question. The use of the SMOW standard was discontinued.

VSMOW is a recalibration of the original SMOW definition and was created in 1967 by Harmon Craig and other researchers from Scripps Institution of Oceanography at the University of California, San Diego who mixed distilled ocean waters collected from different spots around the globe. VSMOW remains one of the major isotopic water benchmarks in use today.

09/12/2013

Harold Clayton Urey (April 29, 1893 – January 5, 1981) was an American physical chemist whose pioneering work on isotopes earned him the Nobel Prize in Chemistry in 1934 for the discovery of deuterium. He played a significant role in the development of the atom bomb, but may be most prominent for his contribution to theories on the development of organic life from non-living matter.

Born in Walkerton, Indiana, Urey studied thermodynamics under Gilbert N. Lewis at the University of California. After he received his PhD in 1923, he was awarded a fellowship by the American-Scandinavian Foundation to study at the Niels Bohr Institute in Copenhagen. He was a research associate at Johns Hopkins University before becoming an associate professor of Chemistry at Columbia University. In 1931, he began work with the separation of isotopes that resulted in the discovery of deuterium.

During World War II Urey turned his knowledge of isotope separation to the problem of uranium enrichment. He headed the group located at Columbia University that developed isotope separation using gaseous diffusion. The method was successfully developed, becoming the sole method used in the early post-war period. After the war, Urey became professor of chemistry at the Institute for Nuclear Studies, and later Ryerson professor of chemistry at the University of Chicago.

Urey speculated that the early terrestrial atmosphere was probably composed of ammonia, methane, and hydrogen. One of his Chicago graduate students, Stanley L. Miller, who showed in the Miller-Urey experiment that, if such a mixture be exposed to electric sparks and water, it can interact to produce amino acids, commonly considered the building blocks of life. Work with isotopes of oxygen led to pioneering the new field of paleoclimatic research. In 1958, he accepted a post as a professor at large at the new University of California, San Diego (UCSD), where he helped create the science faculty. He was one of the founding members of UCSD's school of chemistry, which was created in 1960. He became increasingly interested in space science, and when Apollo 11 returned moon rock samples from the moon, Urey examined them at the Lunar Receiving Laboratory.

08/12/2013

A view of the Sausage device casing of the Ivy Mike hydrogen bomb, with its instrumentation and cryogenic equipment attached. This bomb held a cryogenic Dewar flask containing room for as much as 160 kilograms of liquid deuterium. The bomb was 20 feet tall. Note the seated man at the right of the photo for the scale.

08/12/2013

The 62-ton Ivy Mike device built by the United States and exploded on 1 November 1952, was the first fully successful "hydrogen bomb" or thermonuclear bomb. In this context, it was the first bomb in which most of the energy released came from nuclear reaction stages that followed the primary nuclear fission stage of the atomic bomb. The Ivy Mike bomb was a factory-like building, rather than a deliverable weapon. At its center, a very large cylindrical, insulated vacuum flask or cryostat, held cryogenic liquid deuterium in a volume of about 1000 liters (160 kilograms in mass, if this volume had been completely filled). Then, a conventional atomic bomb (the "primary") at one end of the bomb was used to create the conditions of extreme temperature and pressure that were needed to set off the thermonuclear reaction.

Within a few years, so-called "dry" hydrogen bombs were developed that did not need cryogenic hydrogen. Released information suggests that all thermonuclear weapons built since then contain chemical compounds of deuterium and lithium in their secondary stages. The material that contains the deuterium is mostly lithium deuteride, with the lithium consisting of the isotope lithium-6. When the lithium-6 is bombarded with fast neutrons from the atomic bomb, tritium (hydrogen-3) is produced, and then the deuterium and the tritium quickly engage in thermonuclear fusion, releasing abundant energy, helium-4, and even more free neutrons.

08/12/2013

Shortly before the war, Hans von Halban and Lew Kowarski moved their research on neutron moderation from France to England, smuggling the entire global supply of heavy water (which had been made in Norway) across in twenty-six steel drums.

During World War II, N**i Germany was known to be conducting experiments using heavy water as moderator for a nuclear reactor design. Such experiments were a source of concern because they might allow them to produce plutonium for an atomic bomb. Ultimately it led to the Allied operation called the "Norwegian heavy water sabotage", the purpose of which was to destroy the Vemork deuterium production/enrichment facility in Norway. At the time this was considered important to the potential progress of the war.

After World War II ended, the Allies discovered that Germany was not putting as much serious effort into the program as had been previously thought. The Germans had completed only a small, partly built experimental reactor (which had been hidden away). By the end of the war, the Germans did not even have a fifth of the amount of heavy water needed to run the reactor, partially due to the Norwegian heavy water sabotage operation. However, even had the Germans succeeded in getting a reactor operational (as the U.S. did with a graphite reactor in late 1942), they would still have been at least several years away from development of an atomic bomb with maximal effort. The engineering process, even with maximal effort and funding, required about two and a half years (from first critical reactor to bomb) in both the U.S. and U.S.S.R, for example.

08/12/2013

Deuterium is used in heavy water moderated fission reactors, usually as liquid D2O, to slow neutrons without high neutron absorption of ordinary hydrogen. This is a common commercial use for larger amounts of deuterium.

In research reactors, liquid D2 is used in cold sources to moderate neutrons to very low energies and wavelengths appropriate for scattering experiments.

Experimentally, deuterium is the most common nuclide used in nuclear fusion reactor designs, especially in combination with tritium, because of the large reaction rate (or nuclear cross section) and high energy yield of the D–T reaction. There is an even higher-yield D–3He fusion reaction, though the breakeven point of D–3He is higher than that of most other fusion reactions; together with the scarcity of 3He, this makes it implausible as a practical power source until at least D–T and D–D fusion reactions have been performed on a commercial scale. However, commercial nuclear fusion is not yet an accomplished technology. The machine below showed ionized deuterium in an IEC Fusion reactor giving off its characteristic pinkish-red glow .

07/12/2013

Deuterium (symbol D or 2H, also known as heavy hydrogen) is one of two stable isotopes of hydrogen. It has a natural abundance in Earth's oceans of about one atom in 6,420 of hydrogen. Thus deuterium accounts for approximately 0.0156% (or on a mass basis: 0.0312%) of all the naturally occurring hydrogen in the oceans, while the most common isotope (hydrogen-1 or protium) accounts for more than 99.98%. The abundance of deuterium changes slightly from one kind of natural water to another (see VSMOW).

06/12/2013

Since the mid-1200s, the state has controlled Niepolomice Forest, which contains some of the mineral that can be used in extracting deuterium-2 from the ocean wave .

Since the mid-1200s, the state has controlled Niepołomice Forest, which contains some of the last pockets of old-growth forest in Poland.

19/10/2013

Two Generations of Windblown Sediments on Mars:

This colorful scene is situated in the Noctis Labyrinthus region of Mars, perched high on the Tharsis rise in the upper reaches of the Valles Marineris canyon system.

Targeting the bright rimmed bedrock k***s, the image also captures the interaction of two distinct types of windblown sediments. Surrounding the bedrock k***s is a network of pale reddish ridges with a complex interlinked morphology. These pale ridges resemble the simpler “transverse aeolian ridges” (called TARs) that are common in the equatorial regions of Mars.

The TARs are still poorly understood, and are variously ascribed to dunes produced by reversing winds, coarse grained ripples, or indurated dust deposits.Dust deposite also suspected containing a massive amount of deuterium that commonly used in fussion process.

18/10/2013

Zamxy Syrez Company. Company with highly-skilled scientist and bio-tech engineered worker. We are currently introducing the worldwide about our achievement in this field. Along in 2011, our company had managed developed a new massive machine called tocometer. This invention was assumed in seperating deuterium that only appear in sea water. Next, that radioisotop element are use to creat a devastating energy by fussion process which only occur in the sun . This machine was originally found by a physician from New Zealand who is also a close companion of Ernest Rutherford in late 1960's . Unfortunately, he cannot continued his research because of lack of fund. We from this company also facing the same problem. We are now in the effort of looking a huge sponsorship to continue this development . We can say that , if we manage finish this complex project , we should not have problem in finding the sources of energy .