The mouth (by chewing) and the stomach (by gastric motion).
Yes, mechanical breakdown increases the surface area available for chemical reactions to occur on and therefore the speed of the chemical processes.
Food is broken down into nutrients by the digestive system. Ingested food is transformed into usable nutrients by mechanical and chemical processes in the digestive system.
While the pharynx and esophagus do not perform any mechanical or chemical digestive processes, they provide a critical service for the digestive system. They move food from the mouth to the stomach.
While the pharynx and esophagus do not perform any mechanical or chemical digestive processes, they provide a critical service for the digestive system. They move food from the mouth to the stomach.
The very minute food enters the mouth it goes through the digestion process. There are 2 digestive system function processes that take place in our body. These 2 processes are the mechanical digestion and the chemical digestion.
No chemical or mechanical digestion occurs in the esophagus, only propulsion, which is one of the six digestive processes.
Hydrolysis is one chemical process that accomplishes chemical digestion. There are other chemical and mechanical digestive processes.
Chemical weathering is not associated with mechanical weathering. Chemical weathering involves the breakdown of rocks through chemical reactions, while mechanical weathering involves physical processes that break down rocks into smaller pieces.
While the pharynx and esophagus do not perform any mechanical or chemical digestive processes, they provide a critical service for the digestive system. They move food from the mouth to the stomach.
mechanical processes such as frost action, temperature changes, and abrasion. These processes break down rocks into smaller pieces without changing their chemical composition. Over time, physical weathering can create sediment that contributes to the formation of soil.
The breakdown of sedimentary rocks is primarily caused by weathering processes such as physical (mechanical) weathering, chemical weathering, and biological weathering. Physical weathering involves the mechanical breakdown of rocks into smaller pieces, while chemical weathering involves the breakdown of rocks through chemical reactions. Biological weathering is the breakdown of rocks by living organisms such as plants and burrowing animals.
Frost wedging is one of the most important mechanical weathering processes. It occurs when water seeps into cracks in rocks, freezes, and expands, causing the rock to break apart.