1. ¿Cuántos gramos de H2SO4 están contenidos en 6 litros de solución 3 molar? El peso molecular del H2SO4 es 98 gr/mol. 2. Se disuelven 25 gramos de Ca(OH)2 hasta completar 100cc de solución. ¿Cuál será la molaridad resultante? El peso molecular del Ca(OH)2 es 74 gr/mol.
3. Calcular la Normalidad (N) del H3PO4 si tenemos 8 gramos de ácido disuelto en 0,35 litros de solución. El peso molecular del H3PO4 es 98 gr/mol.
4. ¿Cuántos gramos de H2SO4 hay en 300 mililitros de solución uno normal. El peso molecular del H2SO4 es 98 gr/mol.​

Why does a red shoe appear red in daylight

Which are examples of how technology has advanced scientific understanding.1using hot water to sterilize medical equipment.2transplanting a human organ into another individual.3inserting genes from one sheep into another cell to make a cloneunderstanding the different structures that make up a cell.4examining microorganisms from the deepest parts of the ocean

What is the relationship between wind and ocean waves? question 17 options: wind moving at higher speeds will transfer more energy to the water, resulting in stronger waves. wind moving at higher speeds will transfer energy over a larger part of the ocean water, resulting in waves with a shorter wavelength. winds moving at higher speeds with cause water to move forward at faster rates, causing larger ocean waves. winds moving at higher speeds will affect deeper water, resulting in waves that move at a faster rate. how do temperature and salinity affect deepwater currents? question 15 options: as temperatures and salinity levels of water increase, the water rises to the surface where it creates currents as it moves to colder regions. they create changes in wind direction, moving denser water in the same direction as the wind and causing the deepwater circulation patterns found in the ocean. they equalize the forces on undersea currents caused by the coriolis effect as they replace more dense water with less dense water. they create density differences that cause dense deepwater currents to flow toward the equator where they displace less dense, warmer water above them.