This 17mins is better than the 50mins in my school's leture
@nicozhang11327 жыл бұрын
true
@ericjoseph21222 жыл бұрын
Absolutely
@antonioclimax83469 жыл бұрын
This is one of the best explanations I've ever come across. Thanks Callan.
@justinparker93036 жыл бұрын
Terrific video, thanks a lot for the time. You've explained these concepts thoroughly and clearly. This video, as a complete introduction to isotope fractionation, is unparalleled in its quality.
@KenDBerryMD4 жыл бұрын
Excellent primer on Isotope Fractionation
@heatherlerner9 жыл бұрын
Excellent intro to isotopes and fractionation--assigned it to my class. Thanks!
@nericerezo76258 жыл бұрын
you make all this isotope fractionation stuff right and clear. I`m dealing with the PETM and, as you say, some issues are somewhat tricky. Greetings from Mexico!
@edenmagana46735 жыл бұрын
These 17 minutes were the best of my day...even, when you finished I said that´s all (referring me to...I want to hear more)...it´s extremely easy to hear you and understand you...MANY THANKS!
@mahmoudhasan66668 жыл бұрын
Thank you Callan. By far the best video out there explaining isotope fractionation. It would have been nice to include potential energy well and how fractionation is related to temperature. I would love to see more of those video about proxies used in paleoclimate. Cheers.
@rapauli8 жыл бұрын
This is a terrific presentation. Thank you so much. Helps one understand the fundamental background science. Now I better understand how those charts and graphs are generated. More please.
@danielmercado95755 жыл бұрын
This has been such a great explanation and so easy to understand. Thank you so much!
@avonalexson12945 жыл бұрын
Wonderfully clear explanation, the best I've heard. Please make more.
@callanbentley9 жыл бұрын
To "A kuitin": isotope fractionation isn't "of an" atom, but is "between" atoms. It's the separation of isotopes by different weights. Sometimes this fractionation is mass dependent, as in the examples discussed in this video, and sometimes it's mass independent, as with sulfur isotopes in early Earth history. Perhaps it would help to think of the mass difference between isotopes as a % of the total mass. Hydrogen vs. deuterium is huge then: 200% more mass in D than H. But with U-235 and U-238, that percentage is much smaller relative to the whole. It's only about a 1% difference: apparently not enough to make a difference to the physical systems which would fractionate smaller atoms of different isotopes.
@luisasalce9002 жыл бұрын
A very clear explenation! Thank you so much!
@MadFCE20129 жыл бұрын
Great explanation about isotope fractionation. Thank you very much!!!
@55lorus5 жыл бұрын
Great explanation - you make it so simple. Keep producing videos!
@Ging_106 жыл бұрын
Thank you for the clear and simplified presentation. I was looking for that equation of how to calculate the D excess using the VSMOW and its much clearer now.
@joshbutters19616 жыл бұрын
Amazing and very clear, thank-you!
@MohammadAli-sg8bj3 жыл бұрын
Damn, i never knew stable isotopes could be that easy, please keep on making these videos.
@namesan17182 жыл бұрын
Great video! Thank you so much for making this work :)
@PlayNowWorkLater2 ай бұрын
The measuring of Hydrogen isotopes is new to me. Makes sense. My understanding is what you mention later in the video, in measuring the oxygen isotopes stored in oceanic creatures, like diatoms, that use the oxygen available at the time to generate a shell. And then when that creature dies and it sinks to the bottom of the ocean. Over time you get ocean floor layers that are sometimes rich in Oxygen 16/18 alternating with ones that have lower in oxygen 16, as they have evaporated and been stored in ice sheets. Cool presentation though, much more thorough in the whole picture. Your students are lucky to have a teacher like you.
@sinzianathurm9466 жыл бұрын
Thank you so much!!! This was beautiful & so easy to understand! :)
@pallavinayak63454 жыл бұрын
The way he explained is just amazing....thanks a lot.
@nawazkhan-eo8fv3 жыл бұрын
Just brilliant. Thank you.
@tiatistimaren4 жыл бұрын
What a wonderful explanation...thank you!!
@rensdyret9 жыл бұрын
Taking "Paleoclimate" as a course at Copenhagen University and this is amazing!!
@anastassiyatchaikovsky64273 жыл бұрын
Very good and clear explanation! Thank you very much.
@fridtjofsobanski3593 жыл бұрын
Awesome, this helped me so much! Thanks alot!
@dustinheese3 жыл бұрын
KZfaq recommend this to me and it helped remind me of something I needed to know. I'd already liked the video previously..not sure when. Thanks!
@minamazaheri38982 жыл бұрын
Great explanations which helped me a lot to understand the isotope fractionation very well. Many thanks .
@seshasainishmakurapati7105 жыл бұрын
thank u, nice presentation..now i understood clearly.thank u
@tylerjaglal6663 жыл бұрын
Thank you very much for this valuable information!
@bobbyyankey59677 жыл бұрын
Alright, much clearer illustration. Thank you very much for the video, Callan.
@geobrume54163 жыл бұрын
Excellent presentation
@ardhi1087 жыл бұрын
Thank you very much for the lecture. It's really easy to understand :-)
@taladiv34157 жыл бұрын
Well explained and helps put concepts in place.
@manishaluthra65164 жыл бұрын
Sir great video.. Thankyou....
@explorers75479 жыл бұрын
Great work.
@cheemakhaled20924 жыл бұрын
I love the Detective work of "travelling" back in Time
@nicozhang11327 жыл бұрын
It is very useful! Thanks a lot!!!
@shradhasingh18236 жыл бұрын
Thanks sir...it is very helpful!
@roadrageYXE7 жыл бұрын
Great video, thanks!
@manaskar37374 жыл бұрын
Very useful,,
@Envnmt6 жыл бұрын
A very nice lecture.
@devaney187 жыл бұрын
Thank you so much for this!!!!
@MUSARNA8 жыл бұрын
Excellent. Thanks very much
@pooriamohammadzadehshaghoo2448 Жыл бұрын
amazing video
@shaikhhasina67513 жыл бұрын
Amazing lecture !
@dilshananuranga31619 жыл бұрын
thank u sir. realy great
@bid_zy19305 жыл бұрын
Best explanation
@rouzbehgh16062 жыл бұрын
very practical and simple
@mercygift36317 жыл бұрын
this is great thank you
@rezahasibuan50899 жыл бұрын
very helpfull, thanks
4 жыл бұрын
Thank you!
@AsgharAli-dz4nq3 ай бұрын
Brilliant
@MohammadAli-sg8bj3 жыл бұрын
your voice is so crisp
@nikolzelikova58879 жыл бұрын
Firstly, thank you for the best explanation! I just have one question: 18O, OCEAN PART (12:44): T is growing, amount of 18O in ocean decreases due to higher amoutn of E, so the number in numerator is lower too, hence the result of ratio is lower because we are dividing by higer number of 16O? But 16O is lighter than 18O in any occasion, so during that warmer period the ratio should be still higher than in colder periods (amount of evaporated 16O is higher than amount of 18O) but evidently my cogitation is not right, so what am I missing :D
@maddiemcshinee8 жыл бұрын
THANK YOU!!
@TheSultrySalesman3 жыл бұрын
Why do you show delta deuterium in one slide as the ratio of D/H, then in the next slide show delta deuterium as the ratio of H/D? That would cause the inverse, wouldn't it?
@TR-rx5ej5 ай бұрын
From where extra neutrons come into nucleus of carbon 13 and carbon 14?
@pratyushanand69806 жыл бұрын
like delta o-18 two cases should be there for delta-D ! please clarify my curiosity.
@prateekyadav98114 жыл бұрын
THANK YOU!!!
@mamirza868 жыл бұрын
great thanks
@hollowmoon76364 жыл бұрын
Is this an equilibrium or kinetic fractionation process? I'm unsure of their differences
@osnatmarzook44536 жыл бұрын
thank you thank you thank you
@farrishdaniel21793 жыл бұрын
thank you so muchh
@Vishnoipraveen6 ай бұрын
Hello Challan at 08.31 you have used H/D instead D/H as in Oxygen 18O/160 I am bit confused the heavier isotope should be in numerator as in the formula
@Francisssssssss8 жыл бұрын
hey Callan, many thanks for this enlightening video! One curiosity-question: for which elements is this isotope fractionation method available? Are rare earth elements also included, e.g. Cerium, Yttrium...? Can the isotope fractionation be employed in an industrial scale? Cheers!
@callanbentley8 жыл бұрын
I'm not sure I could quote a complete list to you of all elements that have stable isotopes that get fractionated in geological systems, but there are big ones like covered here, and some rare ones too, and there are even some like sulfur that were fractionated on means other than mass in early Earth's different conditions.
@Francisssssssss8 жыл бұрын
+Callan Bentley thanks for you reply, if you have that list at hand and the time to quote it here it would be great, I am completely new in this topic
@SrikanthGDr5 жыл бұрын
Nice presentation. Wondering if there is evidence that life - plants have methods to select C12 (Not C13) during photosynthesis? Is it simply an axiomatic Model? As a consequence, all animals that survive on plant source of food, also needs to be C12 based without C13.
@callanbentley5 жыл бұрын
Hello - There certainly is evidence that they have "methods" in that when we measure plants' C signatures, we find a higher 12C/13C ration than in the ambient CO2. I cannot speak to the biochemical discrimination mechanism in detail, though - but the result is empirically measurable in modern plants. You're right about the trophic cascade - all else being equal, the "downstream" organisms (primary consumers, secondary consumers, etc.) would carry that same ratio forward.
@nandikagirish4887 Жыл бұрын
At time 8:46 , why is it written delta D =H/D...It should be delta D= D/H right?
@AndresRamirez-dz8kd15 күн бұрын
8:20: for the summary, what is the sample (water or ice) from which you calculate H/D? thank you
@callanbentley15 күн бұрын
Either
@patldennis2 жыл бұрын
great explanation! you need a microphone shield however!
@flowerpowerocks32837 жыл бұрын
Thankyou, just to be clear this is an example of equilibrium isotope fractionations.
@ku_teen9 жыл бұрын
quick question who would answer the question "what isotope fractionation? because i get the concept of how it can be used to to deduce paleoclimates but what exactly is isotope fractionation of an atom fundamentally. for example when they say U 235 and 238 have little natural factionalism naturally but like H 1 and 2 deoes. what does that mean?
@depressedrobot24917 жыл бұрын
Probably not relevant for you anymore, but I'll respond that anyways. Isotope fractionation exists when there exists some mecanism that prefers one isotope over another. For example evaporation "prefers" lighter water molecules over heavier molecules. This means that lighter water molecules are more likely to evaporate than heavier molecules. This natural process tends to enrich the oceans in Deuterium (because they have a hard time getting out) and enrich the atmosfere with normal Hydrogen. U235 and U238 on the other hand have no or very little natural fractionalism, because there is no important process that prefers U235 over U238 or viceversa. To name some examples: None of those two uranium isotopes "evaporate" in our atmosfere, so you cannot say that U235 evaporates more readily than U238. Also, there are no living organisms that use Uranium, so by logic there exist no living organisms that prefer one isotope of uranium over the other.
@akashdesai73172 жыл бұрын
Sir, please discuss waht is mass fractionation?
@StereoSpace8 жыл бұрын
Mil - Abbreviation from Latin: millesimus - one thousandth.
@jessleita64146 жыл бұрын
thaaaaaankssss
@Paul-pd9uw5 жыл бұрын
Good job, too bad N-isotopes weren't included though.
@jollyjokress38524 жыл бұрын
flavours....
@peruviangames94502 жыл бұрын
ta bien explicado
@shielas4 жыл бұрын
Why I didn't watch this Video before my terrible class..
why didn't you mention the influence of water vapor on atmospheric temperature. Water vapor is a bigger player in global temperature than CO2. Regardless, thank you for the video!
@callanbentley4 жыл бұрын
Because that's not the focus of the video?
@chiragvanecha63216 жыл бұрын
Amazing video for understanding the stuff...Thank you...