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For a tiny pot of filthy Ice Kacang, Chow Ang Moh says Mars got hope already can Ruin Earth & Flee there! GPGT!

Ang4MohTrump

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https://www.rt.com/news/447139-mars-water-ice-images-esa/




Water on Mars PICTURED: ESA shares incredible IMAGES of Martian ice crater
Published time: 21 Dec, 2018 13:37 Edited time: 21 Dec, 2018 13:37
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5c1ceb87fc7e9310488b45be.jpg

The 82-kilometer-wide Korolev crater, found in the northern lowlands of Mars. © ESA/DLR/FU Berlin
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The European Space Agency has shared an incredible composite image showing a 50-mile wide crater on Mars that is filled with water ice all year long.
Budding future colonists hoping for a white Christmas on Mars will be somewhat disappointed as the ESA has confirmed that sitting in the Korolev crater is, in fact, a thick block of water ice, not snow. The enormous, 82-kilometer-wide, 2-kilometer-deep “ice trap” could still be good for ice skating though.

Even better, the 2,200 cubic kilometers of water ice – same as the volume of Canada’s Great Bear Lake – could be important for the survival of future colonists, and may even enable them to return back home, as water could be split into hydrogen and oxygen for rocket fuel.

5c1cea71fc7e9314488b45c5.jpg

Plan view of Korolev crater © ESA/DLR/FU Berlin
The crater is found in the northern lowlands of Mars near the planet's north pole which is known as Olympia Undae for its wavy, dune-filled terrain. The crater's ice is protected by the topography and by a lair of cold air that shields it from the elements.
5c1ceacffc7e9310488b45b3.jpg

© ESA/DLR/FU Berlin
The composite image was taken by the Mars Express High Resolution Stereo Camera (HRSC) and was actually formed from five different “strips,” with each strip gathered over a different orbit as the Mars Express probe flew overhead. The 2003-launched mission this month marks the 15-year anniversary of the probe’s orbit insertion at the Red Planet.
Also on rt.com Listen to the sky: NASA reveals the sound of wind on Mars (AUDIO)
The icy crater is named after chief rocket engineer and spacecraft designer Sergey Korolev, known as the father of Soviet space technology and the head of iconic space exploration missions including the Sputnik, Vostok, and Voskhod programs. A lesser known fact is that Korolev dreamt about a flight to Mars for decades and was actually working on a rocket that would have brought a man to the Red Planet – and who knows where this unfinished project might have ended if it wasn’t for the Soviet visionary’s untimely death in 1966.

READ MORE: Sergey Korolev: Space exploration's No. 1 constructor & total enigma

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Tony Tan

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is this for real?theres water on mars?


May not be the H²O water even, as we know there is a non-drinkable version of HEAVY WATER used in Nuclear Power Plant called D²O. That tiny amount is nothing to be excited. Can not even sustain a AMK GRC for 1 month.

https://en.wikipedia.org/wiki/Semiheavy_water

Semiheavy water


From Wikipedia, the free encyclopedia




Jump to navigation Jump to search
Deuterium hydrogen oxide Names IUPAC name
(O-2H1)Water
Other names
Deuterium hydrogen monoxide
Deuterium hydrogen oxide, Water-d1 , Water-d
Identifiers
3D model (JSmol)
ChEBI
ChemSpider
InChI[show]
SMILES[show]
Properties
Chemical formula
H2HO (also HDO) Molar mass 19.0214 g mol−1 Appearance Very pale blue, transparent liquid, very similar to regular water Density 1.054 g cm−3 Melting point 3.81 °C (38.86 °F; 276.96 K) Boiling point 101.42 °C (214.56 °F; 374.57 K)
Solubility in water
Reacts log P −0.65
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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7px-Yes_check.svg.png
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Semiheavy water is the result of replacing one of the protium in light water to deuterium. It exists whenever there is water with light hydrogen (protium, 1H) and deuterium (D or 2H) in the mix. This is because hydrogen atoms (hydrogen-1 and deuterium) are rapidly exchanged between water molecules. Water containing 50% H and 50% D in its hydrogen contains about 50% HDO and 25% each of H2O and D2O, in dynamic equilibrium. In r
egular water, about 1 molecule in 3,200 is HDO (one hydrogen in 6,400 is D). By comparison, heavy water D2O occurs at a proportion of about 1 molecule in 41 million (i.e., one in 6,4002). This makes semiheavy water far more common than "normal" heavy water.
The freezing point of semiheavy water is close to the freezing point of heavy water. (3.8°C)


https://en.wikipedia.org/wiki/Heavy_water

Heavy water


From Wikipedia, the free encyclopedia




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Not to be confused with hard water or tritiated water.

This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. (March 2018) (Learn how and when to remove this template message)
Heavy water Names IUPAC name
(2H2)Water[3]
Other names
  • Deuterium oxide[1]
  • Water-d2[2]
  • Dideuterium monoxide
Properties
Chemical formula
D
2O Molar mass 20.0276 g mol−1 Appearance Colorless liquid Odor Odorless Density 1.107 g mL−1 Melting point 3.82 °C; 38.88 °F; 276.97 K Boiling point 101.4 °C (214.5 °F; 374.5 K)
Solubility in water
Miscible log P −1.38
Refractive index (nD)
1.328 Viscosity 1.25 mPa s (at 20 °C)
Dipole moment
1.87 D Hazards NFPA 704
80px-NFPA_704.svg.png

0
1
0
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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verify (what is
7px-Yes_check.svg.png
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?) Infobox references
Heavy water (deuterium oxide, 2
H
2O
, D
2O
) is a form of water that contains a larger than normal amount of the hydrogen isotope deuterium (2
H or D, also known as heavy hydrogen), rather than the common hydrogen-1 isotope (1
H or H, also called protium) that makes up most of the hydrogen in normal water.[4] The presence of deuterium gives the chemical different nuclear properties, and the increase of mass gives it different physical and chemical properties compared to normal "light water".
Contents
Explanation
Deuterium is a hydrogen isotope with a nucleus containing a neutron and a proton; the nucleus of a protium (normal hydrogen) atom consists of just a proton. The additional neutron makes a deuterium atom roughly twice as heavy as a protium atom.
A molecule of heavy water has two deuterium atoms in place of the two protium atoms of ordinary "light" water. The weight of a heavy water molecule, however, is not substantially different from that of a normal water molecule, because about 89% of the molecular weight of water comes from the single oxygen atom rather than the two hydrogen atoms. The colloquial term heavy water refers to a highly enriched water mixture that contains mostly deuterium oxide D
2O, but also some hydrogen-deuterium oxide (HDO) and a smaller number of ordinary hydrogen oxide H
2O molecules. For instance, the heavy water used in CANDU reactors is 99.75% enriched by hydrogen atom-fraction—meaning that 99.75% of the hydrogen atoms are of the heavy type. For comparison, ordinary water (the "ordinary water" used for a deuterium standard) contains only about 156 deuterium atoms per million hydrogen atoms, meaning that 0.0156% of the hydrogen atoms are of the heavy type.
Heavy water is not radioactive. In its pure form, it has a density about 11% greater than water, but is otherwise physically and chemically similar. Nevertheless, the various differences in deuterium-containing water (especially affecting the biological properties) are larger than in any other commonly occurring isotope-substituted compound because deuterium is unique among heavy stable isotopes in being twice as heavy as the lightest isotope. This difference increases the strength of water's hydrogen-oxygen bonds, and this in turn is enough to cause differences that are important to some biochemical reactions. The human body naturally contains deuterium equivalent to about five grams of heavy water, which is harmless. When a large fraction of water (> 50%) in higher organisms is replaced by heavy water, the result is cell dysfunction and death.[5]
Heavy water was first produced in 1932, a few months after the discovery of deuterium.[6] With the discovery of nuclear fission in late 1938, and the need for a neutron moderator that captured few neutrons, heavy water became a component of early nuclear energy research. Since then, heavy water has been an essential component in some types of reactors, both those that generate power and those designed to produce isotopes for nuclear weapons. These heavy water reactors have the advantage of being able to run on natural uranium without using graphite moderators that pose radiological[7] and dust explosion[8] hazards in the decommissioning phase. Most modern reactors use enriched uranium with ordinary water as the moderator.
Other heavy forms of water
Semiheavy water
Semiheavy water, HDO, exists whenever there is water with light hydrogen (protium, 1
H) and deuterium (D or 2
H) in the mix. This is because hydrogen atoms (hydrogen-1 and deuterium) are rapidly exchanged between water molecules. Water containing 50% H and 50% D in its hydrogen actually contains about 50% HDO and 25% each of H
2O and D
2O, in dynamic equilibrium. In normal water, about 1 molecule in 3,200 is HDO (one hydrogen in 6,400 is in the form of D), and heavy water molecules (D
2O) only occur in a proportion of about 1 molecule in 41 million (i.e. one in 6,4002). Thus semiheavy water molecules are far more common than "pure" (homoisotopic) heavy water molecules.
Heavy-oxygen water
Water enriched in the heavier oxygen isotopes 17
O
and 18
O
is also commercially available, e.g., for use as a non-radioactive isotopic tracer. It is "heavy water" as it is denser than normal water (H
218
O is approximately as dense as D
2O, H
217
O is about halfway between H
2O and D
2O)—but is rarely called heavy water, since it does not contain the deuterium that gives D2O its unusual nuclear and biological properties. It is more expensive than D2O due to the more difficult separation of 17O and 18O.[9] H218O is also used for production of fluorine-18 for radiopharmaceuticals and radiotracers and for positron emission tomography.
Tritiated water
Tritiated water contains tritium (3H) in place of protium (1H) or deuterium (2H), and therefore it is radioactive.
Physical properties
Physical properties of isotopologues of water[10]
Property D2O (Heavy water) HDO (Semiheavy water) H2O (Light water) Freezing point 3.82 °C (38.88 °F) (276.97 K) 2.04 °C (35.67 °F) (275.19 K) 0.0 °C (32 °F) (273.15 K) Boiling point 101.4 °C (214.5 °F) (374.55 K) 100.7 °C (213.3 °F) (373.85 K) 100.0 °C (212 °F) (373.15 K) Density at STP (g/mL) 1.1056 1.054 0.9982 Temp. of maximum density 11.6 °C Unverified 3.98 °C[11] Dynamic viscosity (at 20 °C, mPa·s) 1.2467 1.1248 1.0016 Surface tension (at 25 °C, N/m) 0.07187 0.07193 0.07198 Heat of fusion (kJ/mol) 6.132 6.227 6.00678 Heat of vaporisation (kJ/mol) 41.521 Unverified 40.657 pH (at 25 °C)[12] 7.44 ("pD") 7.266 ("pHD") 7.0 pKb (at 25 °C)[12] 7.44 ("pKb D2O") Unverified 7.0 Refractive index (at 20 °C, 0.5893 μm)[13] 1.32844 Unverified 1.33335

The physical properties of water and heavy water differ in several respects. Heavy water is less dissociated than light water at given temperature, and the true concentration of D+ ions is less than  H+ ions would be for a light water sample at the same temperature. The same is true of OD− vs.  OH− ions. For heavy water Kw D2O (25.0 °C) = 1.35 × 10−15, and [D+ ] must equal [OD− ] for neutral water. Thus pKw D2O = p[OD−] + p[D+] = 7.44 + 7.44 = 14.87 (25.0 °C), and the p[D+] of neutral heavy water at 25.0 °C is 7.44.
The pD of heavy water is generally measured using pH electrodes giving a pH (apparent) value, or pHa, and at various temperatures a true acidic pD can be estimated from the directly pH meter measured pHa, such that pD+ = pHa (apparent reading from pH meter) + 0.41. The electrode correction for alkaline conditions is 0.456 for heavy water. The alkaline correction is then pD+ = pHa(apparent reading from pH meter) + 0.456. These corrections are slightly different from the differences in p[D+] and p[OD-] of 0.44 from the corresponding ones in heavy water.[14]
Heavy water is 10.6% denser than ordinary water, and heavy water's physically different properties can be seen without equipment if a frozen sample is dropped into normal water, as it will sink. If the water is ice-cold the higher melting temperature of heavy ice can also be observed: it melts at 3.7 °C, and thus does not melt in ice-cold normal water.[15]
An early experiment reported not the "slightest difference" in taste between ordinary and heavy water.[16] However, rats given a choice between distilled normal water and heavy water were able to avoid the heavy water based on smell, and it may have a different taste.[17] Some humans have reported that heavy water produces a "burning sensation or sweet flavor".[18]
No physical properties are listed for "pure" semi-heavy water, because it is unstable as a bulk liquid. In the liquid state, a few water molecules are always in an ionised state, which means the hydrogen atoms can exchange among different oxygen atoms. Semi-heavy water could, in theory, be created via a chemical method, but it would rapidly transform into a dynamic mixture of 25% light water, 25% heavy water, and 50% semi-heavy water. However, if it were made in the gas phase and directly deposited into a solid, semi heavy water in the form of ice could be stable. This is due to collisions between water vapour molecules being almost completely negligible in the gas phase at standard temperatures, and once crystallized, collisions between the molecules cease altogether due to the rigid lattice structure of solid ice.[citation needed]






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