Hyrogen cations and Hydroxide anions
Water flows faster through cylinders containing large particles because there are larger spaces between the particles, allowing for less resistance to the flow of water. In contrast, cylinders containing smaller particles have more surface area and tighter packing, which creates more friction and resistance to the flow of water.
Particles are closest together in most solids, though there is very little difference between the spacing in solids and liquids. Particles are very far apart in a gas. Water is not a state of matter. It is an individual substance, and can exist as solid, liquid or gas depending on the temperature and pressure. However it is rather unusual in that the particles in solid water (ice) are actually further apart than those in cold liquid water, which is why ice floats.
The flow of water in a pipe is analogous to the flow of charge in a wire as both involve the movement of particles through a medium. In a pipe, water molecules move due to a pressure difference, while in a wire, charges move due to a voltage difference. Both systems exhibit resistance to flow, which can be influenced by factors such as pipe diameter or wire material.
The particles bouncing along a stream bottom is called saltation. This process involves particles being lifted and transported by the flow of water, before being dropped or settling back to the stream bottom. Saltation is common in streams with moderate flow velocities and bed roughness.
When ice melts, the solid water particles gain energy, causing them to break free from their rigid structure and transition into a liquid state. This extra energy is absorbed by the particles as heat, allowing them to move more freely and flow like a liquid.
particles are further apart and allows water to flow
The flow of electrons is a lot like flow of fluid particles(say water particles). This is based upon the so called "hydrostatic analogy" of electrical circuits.
Clean water can flow faster than dirty water because clean water has fewer impurities and particles that can slow down its flow. However, other factors like the volume of water, slope of the terrain, and obstacles in the path can also affect the speed of water flow.
the water will flow in because the molecules in the pouch cannot flow out and the water particles will be able to flow in because they are smaller than the salt particles.
Large particles carried by water include sediment, rocks, debris, and organic matter. These particles can be transported by the flow of water in rivers, streams, and oceans, contributing to erosion and sedimentation processes.
Water resistance occurs when particles in the water disrupt the flow of objects moving through it. These particles can create drag and friction, making it harder for objects to move smoothly through the water. The more particles present in the water, the greater the resistance an object will experience.
Water flows faster through cylinders containing large particles because there are larger spaces between the particles, allowing for less resistance to the flow of water. In contrast, cylinders containing smaller particles have more surface area and tighter packing, which creates more friction and resistance to the flow of water.
Particles of sand and pebbles that are less dense than water are carried by a stream through a process called suspension. The flow of the water exerts enough force to keep these lighter particles suspended in the water and move them downstream. The particles are lifted off the streambed and transported until the flow of the water slows down or they encounter an obstacle that causes them to settle.
Sandy soil allows water to flow fastest due to its large particles and low water retention capacity. Conversely, clay soil, with its small particles and high compaction, slows down water flow. Loamy soil, a mixture of sand, silt, and clay, offers a balance between water flow and retention.
The correct order for the process of water eroding soil is: detachment of soil particles by water flow, transport of detached particles by the water, and deposition of particles when the water slows down or stops.
Flowing water deposits the largest particles first due to their weight and the energy of the flow. Heavier particles require more force to be lifted and transported, so when the water’s velocity decreases, these larger sediments settle out of the flow before smaller particles. This process is known as sedimentation, where particle size and water velocity play crucial roles in determining the order of deposition. As water slows down, it loses the energy needed to carry larger particles, leading to their deposition first.
Smaller soil particles create smaller pore spaces, reducing permeability by slowing water flow. Larger soil particles have larger pore spaces, allowing water to flow more easily through the soil.