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| Fig. 1 "Spontaneously" is a magic word |
I asked the AI entity "how does an atom determine or detect a photon should be emitted because a cooler atom is within second law of thermodynamics range".
In other words:
"How does an atom 'realize' that, according to the laws of physics that apply, the laws that it obeys, that a cooler atom is in the vicinity and the laws of physics says it must send a photon to that atom so that the second law of thermodynamics is obeyed?"
The graphic at Fig. 1 shows how important it is to know how the second law of thermodynamics impacts photon radiation, because it is happening in the oceans (and everywhere else) at all depths and all times (more graphs in Appendix One)..
The AI entity mentioned 'spontaneous' in its replies, so I asked about 'spontaneous'.
Among other things the AI entity responded, intimating some of the dynamics, but didn't seem to grasp the fact that its assertion about 'nature' and "without any external assistance" means , then, that the detection system required to 'be aware' of other atoms and their 'temperature' was inside the atom:
"In thermodynamics, spontaneous means a process that occurs naturally, without the need for external energy input. In the context of the second law, it means heat will flow from a hotter to a cooler body without any external assistance."
(AI entity). That did not answer my question, so I was reminded of how AI, in some areas of knowledge, is so human in the way it receives and passes on information (The Pillars of Knowledge: Faith and Trust?).
The link at Fig. 1 has this to ponder, which IMO is relevant:
"...we have a kind of metaphysical belief that there are laws of nature that are outside time and those laws of nature are causing the outcome of the experiment to be what it is. And laws of nature don't change in time. They're outside of time. They act on the system now, they acted on the system in the same way in the past, they will act the same way in a year or a million or a billion years, and so they'll give the same outcome. So nature will repeat itself and experiments will be repeatable because there are timeless laws of nature.
But that's a really weird idea [for scientists] if you think about it because it involves the kind of mystical and metaphysical notion of something that is not physical, something that is not part of the state of the world, something that is not changeable, acting from outside the system to cause things to happen. And, when I think about it, that is kind of a remnant of religion. It is a remnant of the idea that God is outside the system acting on it."
(Small Brains Considered - 7). That series discusses "small brains" of quanta that would have to exist to bring about the enormous quantity of data/knowledge required for atoms to have a part in collecting, storing, and radiating photons of specific energy levels to a colder atom in their vicinity.
So, the question remains, can atoms receive and pass on tiny information in a language much smaller than now-known photon sizes (like the microbes discussed in the video below)?
Organic life, especially marine organisms like phytoplankton and other microbes, plays a significant role in the ocean's carbon cycle, which indirectly influences ocean heat absorption and climate regulation.
Here's how, paraphrased from various encyclopedic sources:
Photosynthesis and Carbon Sequestration: Phytoplankton, microscopic plant-like organisms in the ocean, absorb carbon dioxide (CO2) from the atmosphere through photosynthesis, similar to land plants. This process incorporates the carbon into their organic matter.
The Biological Pump: As phytoplankton die or are consumed by other marine organisms, a portion of the carbon they've absorbed sinks to deeper ocean layers. This process, known as the "biological pump," effectively transfers carbon from the atmosphere to the deep ocean, where it can be stored for long periods, mitigating the greenhouse effect and indirectly influencing ocean temperatures.
Impact of Warming Oceans: However, rising ocean temperatures can negatively impact this process. Warmer waters can cause phytoplankton and other organisms to dissolve in the upper ocean before they can sink, keeping the carbon in the surface waters where it can be released back into the atmosphere. Additionally, warming can lead to increased ocean stratification, reducing the mixing of water layers and hindering the supply of nutrients from the deep ocean that phytoplankton need to grow.
Potential for Reduced Carbon Sequestration: If warming oceans lead to a decline in phytoplankton populations and a weakening of the biological pump, the ocean's capacity to absorb atmospheric CO2 could be reduced, further exacerbating climate change. In summary, while the ocean absorbs most of the excess heat from the atmosphere, organic life, particularly phytoplankton, plays a crucial role in regulating atmospheric CO2 levels, which in turn influences ocean temperatures and overall climate stability. Understanding how these organisms are affected by climate change is crucial for predicting future climate scenarios.
While it's the ocean itself that absorbs the vast majority of excess heat due to its high heat capacity, certain organic processes within the ocean are affected by and in turn influence ocean temperature:
Ectothermic marine life: "Cold-blooded" animals like fish, reptiles, amphibians, and most invertebrates have body temperatures that largely depend on the surrounding water temperature. This means they are directly impacted by ocean heat and may need to adapt through behavioral or physiological changes, or by migrating to cooler waters.
Phytoplankton: These microscopic plants absorb carbon dioxide through photosynthesis. Warmer ocean temperatures can negatively impact their growth and productivity, potentially affecting the ocean's ability to sequester carbon,. A recent study also suggests that some phytoplankton may shift to releasing more CO2 than they absorb in warmer conditions.
Impact on Food Webs: Changes in phytoplankton populations due to warming can have cascading effects on the marine food web, as they form the base of the food chain.
Deep-Sea Life and Carbon Storage: Deep-sea ecosystems play a role in climate mitigation by storing large amounts of CO2 and absorbing heat. Microorganisms in these environments are essential for breaking down organic matter and preventing greenhouse gases like methane from reaching the surface.
In summary, while organic life doesn't directly absorb and "remove" heat in the same way the ocean water does, it is significantly affected by ocean warming, and its processes, particularly those involving carbon sequestration, can influence the Earth's climate system.
Future posts in this series will detail more of the full conversation with the AI entity and my responses, along with further discussions.
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