Gravity causes water to flow downwards. In porous ground the water will seep into the soil. If the water hits a non-porous layer (clay, for instance) the water will spread horizontally.
Fresh water can infiltrate the ground and move through porous layers of soil and rock to reach underground aquifers. This process, known as groundwater recharge, occurs when precipitation seeps into the ground and fills the spaces between particles in the soil or rock. The water then flows slowly through these underground layers, eventually replenishing underground water sources.
Maybe because when the water is in the soil and is going through the roots up the stem some soil particles can go in the water and travel with it.
The speed at which water moves through soil depends on factors such as soil texture, porosity, and saturation levels. In general, sandy soils allow water to pass through more quickly than clay soils. The process can range from minutes to hours for water to move through soil.
It goes into interstitial gaps in the soil particles.
Capillary action and gravity.
Sand moves fastest through water, where it can be carried along by water currents. It moves slower through sandy soil due to friction, and even slower through silty soil due to smaller pore spaces and more resistance. Overall, the speed of sand movement depends on factors like water flow rate, soil composition, and grain size.
Groundwater can flow in various directions, depending on factors like the water table level and underground geology. Typically, groundwater moves through permeable rock or soil layers, eventually discharging into streams, lakes, or oceans. In some cases, groundwater can also be extracted through wells for human use.
Yes, water can pass through loam soil due to its balanced mixture of sand, silt, and clay particles. Loam soil has excellent drainage properties, allowing water to percolate through the soil and reach plant roots while still retaining enough moisture for healthy plant growth.
Through Des Moines
Go underground and you could get a water stone there
The water goes to the sewers or underground.
The water will go through the soil but not as fast as the regular-or dirt but sand it will go through very slow butt if you have very little sand it will go through it just a little bit faster than all that sand that you put in a jar to play with or stor away some time for your kids or your self to pla with butt any wayhe water will go through mud and dirt faster than sand but you should know that wright. Hopefully you don't know that, because it is WRONG! In fact, the opposite is true. Water flows through the tiny void spaces between the soil particles. That is, the larger the void spaces the greater the velocity of water flowing through the soils. So now we just need to know the void ratio of different types of soils. In simplest terms, the smaller the particles, the smaller the void ratio. However, the void ratio is also dependent on the angularity and shape of the soil, the moisture content of the soil and the density of the soil. But for all things equal, the velocity of water following through the following soil types are listed in order of greatest to smallest: Boulders (Fastest) Gravel (Fast) Sand (Average) Silt (Medium Slow) Clay (Slow) This is a very simplified answer.