What are soil remediation techniques?

What are soil remediation techniques? Remediation techniques which have been commonly used include: containment, pump-and-treat, extraction, stabilization/solidification, soil washing, air stripping, precipitation, vitrification, thermal desorption and biological remediation. What are the methods of soil remediation? Options for treating contaminated soil include: Biological treatment/bioremediation uses bacteria to break down substances in the soil. Chemical oxidation converts […]

Why energy is stored in form of ATP?

Why energy is stored in form of ATP? Cellular energy is primarily trapped and stored in the form of adenosine triphosphate or ATP. To trap energy released from exergonic catabolic chemical reactions, the cell uses some of that released energy to attach an inorganic phosphate group on to adenosine diphosphate (ADP) to make adenosine triphosphate […]

Is friction useful in rowing?

Is friction useful in rowing? The force of the water pushing on the spoon during rowing will make the boat speed up, and the force of the drag will cause the boat to slow down. Another important point is that static friction between the rower’s backside and the boat is causing the rower to stay […]

What is the hardest question to ask?

What is the hardest question to ask? Hard Questions to Ask Yourself, and Even Harder Questions to Answer Do you feel like you’ve lived this same day many times before? Are you living the life of your dreams? What would you do if fear was not a factor and you could not fail? What were […]

How did Earths oceans form?

How did Earths oceans form? According to this theory, the ocean formed from the escape of water vapor and other gases from the molten rocks of the Earth to the atmosphere surrounding the cooling planet. After the Earth’s surface had cooled to a temperature below the boiling point of water, rain began to fall—and continued […]

What keeps the heat in Earth?

What keeps the heat in Earth? There are three main sources of heat in the deep earth: (1) heat from when the planet formed and accreted, which has not yet been lost; (2) frictional heating, caused by denser core material sinking to the center of the planet; and (3) heat from the decay of radioactive […]

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