Acid lava comes from composite cone volcanoes, is slow moving and viscous. Basic lava comes from shield volcanoes, is runny and flows faster. Acidic lava is felsic, or high in quartz and potassium feldspars. Basic lava is mafic, and higher in plagioclase feldspar.
Acidic lava is different from basaltic lava because it has a higher silica content in it than basaltic lava. The higher the silica level in a lava, the more viscous and less runny the lava is. Also, with acidic lava being more viscous, it traps gases in it more easily (for example blowing bubbles in water using a straw is easier than doing it in a milkshake), causing more violent eruptions to take place when released from a volcano. Lastly, because basaltic lava is more viscous and runny than more acidic lavas it can cover larger areas (up to 10,000s km) once erupted.
Acid lava- viscous, slow-moving, cool quickly, produced at destructive plate boundary, rich in silica
Basaltic lava - less viscous, fluid, cool slowly, produced at constructive plate boundary, lower silica content, rich in Iron and magnesium
"Acidic lava" is an outdated term. It was once belived that high-silica lavas such as rhyolitic lava contained significant quantities of silicic acid. This has been disproven.
Currently, the term "felsic" is used instead. Felsic is a somewhat broader term than rhyolitic. It can refer to rhyolitic lava or other lavas of somewhat similar composition.
Lava is molten rock that is on Earth's surface. Basalt is one type of igneous rock that forms when lava cools. It is characterized by a low about of silica, aluminum, and alkali metals and higher levels of iron and magnesium. Other, less common types of lava with different chemical makeups will cool to form other types of rock such as andesite.
Is acid lava lighter than basic lava
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Basic discovers large area after cooling
Litmus papers can only be used to determine whether the solution is acidic or basic. But from pH meter, the pH range of the solution can be determined.
The pH is acidic.
The stability of the archaea enables then survive in extreme temperature and areas that are highly alkaline and highly acidic.
Neutralization
because the lower the pH the more acidic something is
At the standard temperature of 298 K, it is acidic.
pH is a measure of the acidity or basicity of a solution. The pH of a solution is temperature-dependent.pH is a measure of how acidic or alkaline (the opposite of acidic) a material is. It has nothing to do with temperature.
Acidic pH is a reading of between pH7 (neutral) and pH 0 (highly acidic).
At the temperature of 298 K, any pH value lesser than 7.0 is considered to be acidic.
Litmus papers can only be used to determine whether the solution is acidic or basic. But from pH meter, the pH range of the solution can be determined.
The pH is acidic.
you can't change the pH level of the contents no matter where you store it. storage space has air, which is composed of our standard gases--nitrogen, oxygen, hydrogen, etc. over time, molecular interference (van der Waals forces) between the "juice" and the gases can develop as part of a chemical reaction creating OH- (base) or H+ (acid) molecules as reagents. this would surely affect the pH level of juice.
acidic buffers increase pH as temperature increases, basic buffers decrease pH as temperature increases I am still searching for the reason.
Where the environment is very hot and very acidic.
At the temperature of 298 K, the pH 7.0 indicates neutral solution. Any value below is acidic and any value above is basic.
The effects of low acidic pH in the differences of enzymatic activity can be seen in its amino acid sequence and the environment of the solution it is mixed into. Enzymes are tertiary proteins. The acid can effect the structure by making it less accessible to the substrates or ligands.
The stability of the archaea enables then survive in extreme temperature and areas that are highly alkaline and highly acidic.