Transcribed by Bert.
[March 1, 2014 Part 2 (30:35 mark)]
Jean: I heard last week that the element of oxygen will no longer bond with a proton. Did I hear correctly?
iON: That’s right! You did!
Jean: So, what I heard tonight was that hydrogen replaces oxygen in that relationship.
iON: It will… a derivation of that! But yes - that’s correct. It’s actually an isotope of hydrogen that will replace it. But when it does, it won’t be an isotope any longer because the base is changed. So, “yes” is the answer to the question, but not exactly as you would say it is today.
Jean: What will it be if it will no longer be an isotope?
iON: It will be an isotope that’s stable - that does not have a half-life. It’s hydrogen, H197.
Jean: So, it won’t be in a single atomic state.
iON: It won’t be an isotope
Jean: It won’t be an element - it won’t be an isotope. It’ll be something entirely different?
iON: It won’t be an isotope - it’ll be a stable element that’s hydrogen with an atomic number not of 1, but of 197.
Jean: It’s a derivative of hydrogen but not an isotope?
iON: It will not be what replaces oxygen.
Caller: It will not be what replaces oxygen.
iON: No, it will not be an isotope when it replaces oxygen.
Jean: OK! So, now…
iON: See, two parts have got to change - two things that got to change - and when they change - then it will - and then that stable hydrogen, H197, will replace oxygen.
[ March 8, 2014 Part 1 (23:27 mark)]
Caller: OK, how about when I was on that cruise ship? What was happening with…
Bob: Yeah!
Caller: … the things that I wasn’t aware of - like the portalling, and people coming from other worlds?
iON: Oh, OK! Hold on! Hold on! Here’s what happens: when you get on the water - that much hydrogen - sometimes you are freed. Like, you’ll get used to the flow - and then, what happens is the connection - there’s not a grounding - there’s no way to ground on that much hydrogen. So, you always have “higher ethered position” in that much water - especially that much salty water. It makes it even easier. Then what happens - you find you have an easier flux - because you are sensitive to it, anyway. It just opened it wide open.
[March 15, 2014 Part 3 (10:05 mark)]
iON: Fire will burn! Hydrogen will burn! Hydrogen burns differently than oxygen. That’s the difference!
[March 22, 2014 Part 2 (1:26:14 mark)]
iON: What “purple" {Fukushima nuclear reactor - Ed.} is supposed to do is increase the levels of H197 -which will decrease the amount of oxygen - as the radial isotope gets greater in the level of the atmosphere condition. In a hydrogen world, you will basically displace or dispel oxygen as you keep knocking out electrons.
[May 10, 2014 Part 1 (1:14:43 mark)]
iON: Why would we choose carbon to balance the hydrogen in the first place?
Caller: Well, they’ve got electrons to donate.
iON: They do that, indeed - ambient one besides, eh!
Caller: You said: “Why would you choose carbon to balance the hydrogen”?
iON: Yes!
Caller: Are you talking regular hydrogen or H197?
iON: To us, regular hydrogen is H197 – to us! What you have as hydrogen, we find as the abomination. Our hydrogen, H197, is hydrogen. Your hydrogen, we don’t acknowledge.
[May 17, 2014 Part 2 (36:09 mark)]
Bob: On Dupes, they were going on about H197 this - H197 that - and I said: “Everybody, please stop saying 'it’s H197 this - H197 that'. The appropriate nomenclature is “stabilized H197 – Super Sugar this or that!” So, MSU1977 says: “Bob, at which stage does H197 become stabilized H197?”
iON: It becomes stable when it’s in the presence of “Insulinose”.
Bob: And what is that?
iON: Super Sugar! Am, Super Sugar is… Super Sugar stabilizes H197. It even contains it - and that half-life of a radial isotope H197 in a bound - like lead that’s radiative, wrapped in lead that’s not - will stabilize it. So, Super Sugar will stabilize H197 if it’s a radial isotope.
Bob: Isn’t Super Sugar made up of stabilized H197?
iON: It is! It is!
Bob: So, you’re saying stabilized H197 stabilizes itself?
iON: Super Sugar will stabilize it, yes. The carbon stops the half-life effect.
[May 31, 2014 Part 2 (1:04:52 mark)]
Caller: I was reading that the Indian Ocean is going to turn red. So, what effect will it have on the form of plankton and the subsequent food chain when that event has taken place?
iON: It changes plankton and the krill - krill itself and that food chain of the whole world. The things that eat krill and the things that eat krill - then eat something else - then they eat something else. It changes the way krill lives. When the H197 hits a certain level, it’ll blossom or bloom. And you start changing the boiling point of water. And when oxygen decreases to a certain level, then all of a sudden - salination isn’t pure anymore - because oxygen is the “oxydator”. Salty water and the salination changes, it freezes at a different point. Once the boiling point changes and H197 becomes radical - or the half-life becomes the integer of the present dichotomy of oxygen’s stable environment minus ozone. But then, that’s not really oxygen either - it’s a byproduct - then you have a shift and then the oceans bloom.
[August 30, 2014 Part 2 (08:21 mark)]
Jean: iON, my friends in the country seem to be having respiratory problems related to the change in the air - the humidity when it’s very humid.
iON: That’s because the potential for hydrogen is changing, and there’s more hydrogen than there is anything else in your environment. And so, when you increase the hydrogen… if you’re trying to be an oxygen-based flora and fauna - you’re going to find it challenging to keep from presenting pulmonary edema - because it can’t move the fluids around. So, it makes the air heavier - and that heavy air is a delicious and wonderful thing that’s coming. So, whatever you do, don’t engage RnA Drops {iON is saying this last sentence ironically - Ed.}.
[January 24, 2015 (1:24:56 mark)]
Caller: Is the hydrogen… is the H197 - is it dead?
iON: Yes, it’s inanimate.
Caller: So, you’re referring to “dead” as “inanimate”?
iON: “Animate” – “inanimate”!
Caller: Well, is it inanimate… “dead" is inanimate, meaning it doesn’t move, or it has no movement? What’s “inanimate" exactly? No movement, no life?
iON: No signs of life.
Dr. Dean: Not alive, especially in the manner of animals and humans.
[October 4, 2014 Part 1 (16:16 mark)]
Dr. Dean: iON, we’re talking about the structured waters - the relationship between hydrogen and oxygen. When oxygen becomes depleted, and there’s more hydrogen, will water continue to look the same?
iON: No, but see, here’s the thing. When you’re dealing with laying out how structured water is. Here’s the difference - the difference is what it will hold - and the landscape that it is. OK, let’s do it this way! If you take water and you put it into a bowl, it’s still water. If you take a bowl that is crafted out of sugar and you put water in a sugar bowl, water changes. Now, set structured water aside because that doesn’t make any difference. It’s a bunch of gibberish! Don’t worry about that! But you’re talking about your landscape is changing - and oxygen is less - and hydrogen is more. Well, you can’t make hydrogen more. It’s already what there’s the most is - you can’t make more hydrogen. So, the bowl, or the Earth that it’s in, is changing. Therefore, when you deplete it - reverse, you’re going to have more hydrogen - because it will eat the oxygen.
Dr. Dean: Well, you deplete oxygen - then you have relatively more hydrogen because you already just said that.
iON: In base, it’s already what the most is - is hydrogen. You have the most hydrogen now. You make all this be about oxygen - and that’s the least in the whole process. It’s what kills you.
[March 1, 2014 Part 2 (30:35 mark)]
Jean: I heard last week that the element of oxygen will no longer bond with a proton. Did I hear correctly?
iON: That’s right! You did!
Jean: So, what I heard tonight was that hydrogen replaces oxygen in that relationship.
iON: It will… a derivation of that! But yes - that’s correct. It’s actually an isotope of hydrogen that will replace it. But when it does, it won’t be an isotope any longer because the base is changed. So, “yes” is the answer to the question, but not exactly as you would say it is today.
Jean: What will it be if it will no longer be an isotope?
iON: It will be an isotope that’s stable - that does not have a half-life. It’s hydrogen, H197.
Jean: So, it won’t be in a single atomic state.
iON: It won’t be an isotope
Jean: It won’t be an element - it won’t be an isotope. It’ll be something entirely different?
iON: It won’t be an isotope - it’ll be a stable element that’s hydrogen with an atomic number not of 1, but of 197.
Jean: It’s a derivative of hydrogen but not an isotope?
iON: It will not be what replaces oxygen.
Caller: It will not be what replaces oxygen.
iON: No, it will not be an isotope when it replaces oxygen.
Jean: OK! So, now…
iON: See, two parts have got to change - two things that got to change - and when they change - then it will - and then that stable hydrogen, H197, will replace oxygen.
[ March 8, 2014 Part 1 (23:27 mark)]
Caller: OK, how about when I was on that cruise ship? What was happening with…
Bob: Yeah!
Caller: … the things that I wasn’t aware of - like the portalling, and people coming from other worlds?
iON: Oh, OK! Hold on! Hold on! Here’s what happens: when you get on the water - that much hydrogen - sometimes you are freed. Like, you’ll get used to the flow - and then, what happens is the connection - there’s not a grounding - there’s no way to ground on that much hydrogen. So, you always have “higher ethered position” in that much water - especially that much salty water. It makes it even easier. Then what happens - you find you have an easier flux - because you are sensitive to it, anyway. It just opened it wide open.
[March 15, 2014 Part 3 (10:05 mark)]
iON: Fire will burn! Hydrogen will burn! Hydrogen burns differently than oxygen. That’s the difference!
[March 22, 2014 Part 2 (1:26:14 mark)]
iON: What “purple" {Fukushima nuclear reactor - Ed.} is supposed to do is increase the levels of H197 -which will decrease the amount of oxygen - as the radial isotope gets greater in the level of the atmosphere condition. In a hydrogen world, you will basically displace or dispel oxygen as you keep knocking out electrons.
[May 10, 2014 Part 1 (1:14:43 mark)]
iON: Why would we choose carbon to balance the hydrogen in the first place?
Caller: Well, they’ve got electrons to donate.
iON: They do that, indeed - ambient one besides, eh!
Caller: You said: “Why would you choose carbon to balance the hydrogen”?
iON: Yes!
Caller: Are you talking regular hydrogen or H197?
iON: To us, regular hydrogen is H197 – to us! What you have as hydrogen, we find as the abomination. Our hydrogen, H197, is hydrogen. Your hydrogen, we don’t acknowledge.
[May 17, 2014 Part 2 (36:09 mark)]
Bob: On Dupes, they were going on about H197 this - H197 that - and I said: “Everybody, please stop saying 'it’s H197 this - H197 that'. The appropriate nomenclature is “stabilized H197 – Super Sugar this or that!” So, MSU1977 says: “Bob, at which stage does H197 become stabilized H197?”
iON: It becomes stable when it’s in the presence of “Insulinose”.
Bob: And what is that?
iON: Super Sugar! Am, Super Sugar is… Super Sugar stabilizes H197. It even contains it - and that half-life of a radial isotope H197 in a bound - like lead that’s radiative, wrapped in lead that’s not - will stabilize it. So, Super Sugar will stabilize H197 if it’s a radial isotope.
Bob: Isn’t Super Sugar made up of stabilized H197?
iON: It is! It is!
Bob: So, you’re saying stabilized H197 stabilizes itself?
iON: Super Sugar will stabilize it, yes. The carbon stops the half-life effect.
[May 31, 2014 Part 2 (1:04:52 mark)]
Caller: I was reading that the Indian Ocean is going to turn red. So, what effect will it have on the form of plankton and the subsequent food chain when that event has taken place?
iON: It changes plankton and the krill - krill itself and that food chain of the whole world. The things that eat krill and the things that eat krill - then eat something else - then they eat something else. It changes the way krill lives. When the H197 hits a certain level, it’ll blossom or bloom. And you start changing the boiling point of water. And when oxygen decreases to a certain level, then all of a sudden - salination isn’t pure anymore - because oxygen is the “oxydator”. Salty water and the salination changes, it freezes at a different point. Once the boiling point changes and H197 becomes radical - or the half-life becomes the integer of the present dichotomy of oxygen’s stable environment minus ozone. But then, that’s not really oxygen either - it’s a byproduct - then you have a shift and then the oceans bloom.
[August 30, 2014 Part 2 (08:21 mark)]
Jean: iON, my friends in the country seem to be having respiratory problems related to the change in the air - the humidity when it’s very humid.
iON: That’s because the potential for hydrogen is changing, and there’s more hydrogen than there is anything else in your environment. And so, when you increase the hydrogen… if you’re trying to be an oxygen-based flora and fauna - you’re going to find it challenging to keep from presenting pulmonary edema - because it can’t move the fluids around. So, it makes the air heavier - and that heavy air is a delicious and wonderful thing that’s coming. So, whatever you do, don’t engage RnA Drops {iON is saying this last sentence ironically - Ed.}.
[January 24, 2015 (1:24:56 mark)]
Caller: Is the hydrogen… is the H197 - is it dead?
iON: Yes, it’s inanimate.
Caller: So, you’re referring to “dead” as “inanimate”?
iON: “Animate” – “inanimate”!
Caller: Well, is it inanimate… “dead" is inanimate, meaning it doesn’t move, or it has no movement? What’s “inanimate" exactly? No movement, no life?
iON: No signs of life.
Dr. Dean: Not alive, especially in the manner of animals and humans.
[October 4, 2014 Part 1 (16:16 mark)]
Dr. Dean: iON, we’re talking about the structured waters - the relationship between hydrogen and oxygen. When oxygen becomes depleted, and there’s more hydrogen, will water continue to look the same?
iON: No, but see, here’s the thing. When you’re dealing with laying out how structured water is. Here’s the difference - the difference is what it will hold - and the landscape that it is. OK, let’s do it this way! If you take water and you put it into a bowl, it’s still water. If you take a bowl that is crafted out of sugar and you put water in a sugar bowl, water changes. Now, set structured water aside because that doesn’t make any difference. It’s a bunch of gibberish! Don’t worry about that! But you’re talking about your landscape is changing - and oxygen is less - and hydrogen is more. Well, you can’t make hydrogen more. It’s already what there’s the most is - you can’t make more hydrogen. So, the bowl, or the Earth that it’s in, is changing. Therefore, when you deplete it - reverse, you’re going to have more hydrogen - because it will eat the oxygen.
Dr. Dean: Well, you deplete oxygen - then you have relatively more hydrogen because you already just said that.
iON: In base, it’s already what the most is - is hydrogen. You have the most hydrogen now. You make all this be about oxygen - and that’s the least in the whole process. It’s what kills you.
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