WiartonWilly

WiartonWilly t1_jdai6tg wrote

Making concrete requires massive off-gassing of CO2 from limestone, plus a gigantic amount of energy (ie fossil fuels). If they can capture some CO2 in their product, great. However, I doubt this can do much to offset the concrete industry’s gigantic carbon footprint. Sorry if I’m being too negative, but I’ve never seen a carbon capture technology that can balance their chemical equations.

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WiartonWilly t1_jbu2lif wrote

If acidified.

Question is, where are they getting the sodium (Na)? If they expect to take it from abundant salt (NaCl), then they are left with an excess of acid. That acid either needs to be stored perpetually, or it will eventually liberate the CO2 (as you say)

If there is some natural source of NaOH (a strong base) somewhere, then the CO2 can be sequestered. However, I have never heard of a caustic mine. If they plan to take it from something neutral like salt, then they have an acid storage problem.

The alternatives are potassium (K), calcium (Ca) and magnesium (Mg), but similarly, they are naturally found as salts, in combination with acids that we would rather not release.

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WiartonWilly t1_j93qz2a wrote

Your immune system has rhythms. There are a whole zoo of different immune cell types in your blood. The immune system is like a bunch of liquid organs, each with many cell types. Many cell types which are derived from bone marrow have a tendency to return to the bone during the day. They go home. Circulating cells found in a blood draw, such as neutrophils, can increase by 2 fold at night. At night more immune cells are on active duty.

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WiartonWilly t1_j1dzal3 wrote

Fig. 6. Cartoon summarizing observations. Eruptions and intrusions at Kīlauea cause pressure gradients to rapidly propagate through the Kīlauea transport structure to the Pāhala sill complex. Magma is injected into the Pāhala sill complex from the underlying magma- bearing volume; the sills are proximal to the plagioclase-spinel phase boundary, possibly in a polyphase coexistence region. The sills are connected to Kīlauea and the decollement/Ka‘ōiki region within the Mauna Loa edifice along continuous bands of seismicity.

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