This depends on the nature of the solutes and insoluble impurities.
Chemical sediments are sedimentary rocks that form from the precipitation of minerals dissolved in water. These minerals accumulate on the ocean floor or in lakes through processes like evaporation or chemical reactions. Common examples of chemical sediments include limestone, gypsum, and halite.
Water evaporation is a physical process.
Sediments that form from minerals crystallizing from seawater are known as chemical sediments or evaporites. These sediments typically develop in environments where seawater evaporates, leading to the precipitation of minerals such as halite (rock salt), gypsum, and calcite. This process often occurs in arid regions or shallow marine settings where evaporation rates exceed water inflow. As a result, these sediments can accumulate in layers, forming distinct geological deposits.
No, evaporation of water from a lake is a physical process, not a chemical reaction. It involves the transformation of water from a liquid to a gas without any change in the chemical composition of water molecules.
No, evaporation is a change from liquid to gas (water vapour).
Evaporation is a physical change.
One product of chemical weathering is the formation of clay minerals from the alteration of feldspar minerals in rocks. Clay minerals are fine-grained particles that result from the breakdown of silicate minerals through chemical reactions with water and gases in the environment.
Physical. The water is still water afterwards. You must understand that water can be in any one of three PHYSICAL states, liquid, solid or vapor ( a gas ). Changing physical states is not a chemical change, but a direct result of heat or cold application.
The molecule of water remain unchanged.
physical
During evaporation the structure of water remain unchanged.
The equation for water evaporation can be represented as: H2O (liquid) → H2O (gas) This shows the process where liquid water turns into water vapor through evaporation.