what will happen to loamy soil if a heavy shower of rain falls?
415356
I imagine it would become foamy.
1089980
Water\n\nSplash erosion is the detachment and airborne movement of small soil particles caused by the impact of raindrops on soil. Sheet erosion is the result of heavy rain on bare soil where water flows as a sheet down any gradient, carrying soil particles. Where precipitation rates exceed soil infiltration rates, runoff occurs. Surface runoff turbulence can often cause more erosion than the initial raindrop impact. Gully erosion results where water flows along a linear depression eroding a trench or gully.\n\nValley or stream erosion occurs with continued water flow along a linear feature. The erosion is both downward, deepening the valley, and headward, extending the valley into the hillside. In the earliest stage of stream erosion, the erosive activity is dominantly vertical, the valleys have a typical V cross-section and the stream gradient is relatively steep. When some base level is reached the erosive activity switches to lateral erosion which widens the valley floor and creates a narrow floodplain. The stream gradient becomes nearly flat and lateral deposition of sediments becomes important as the stream meanders across the valley floor. In all stages of stream erosion by far the most erosion occurs during times of flood, when more and faster-moving water is available to carry a larger sediment load. In such processes, it is not the water alone that erodes, suspended abrasive particles, pebbles and boulders can also act erosively, as they traverse a surface.\n\nWind\n\nWind erosion, also known as eolian erosion is the movement of rock and/or sediment by the wind. Windbreaks are often planted by farmers to reduce wind erosion. This includes the planting of trees, shrubs, or other vegetation, usually perpendicular or nearly so to the principal wind direction. The wind causes dust particles to be lifted and therefore moved to another region. Wind erosion generally occurs in areas with little or no vegetation, often in areas where there is insufficient rainfall to support vegetation. An example is the formation of sand dunes, on a beach or in a desert.\n\nGlacial\n\nIce erosion is caused by movement of ice, typically as glaciers. Glaciers can scrape down a slope and break up rock and then transport it, leaving moraines, drumlins and glacial erratics in their wake, typically at the terminus or during glacier retreat. Ice wedging is the weathering process in which water trapped in tiny rock cracks freezes and expands, breaking the rock. This can lead to gravity erosion on steep slopes. The scree which forms at the bottom of a steep mountainside is mostly formed from pieces of rock broken away by this means. It is a common engineering problem, wherever rock cliffs are alongside roads, because morning thaws can drop hazardous rock pieces onto the road.
764128
The soil is very iron-rich. When iron oxidizes, it produces iron oxide which is basically rust and it red in color. :)\n\nAnd interesting side fact, the dawn and dusk sky is blue. (It's reddish on Earth :)
422939
The wind blows sand and rubble. Erosion might also cause the land to shift.
7535
The soil moisture and wind speed are both directly proportional to wind erosion.\n\nThe dryer the soil, the more effect wind has on eroding the soil.\n\nThe higher the wind speed, the more soil is eroded.
493080
It is then Acid Rain. Not Good.
597267
Lower pressure will result in more "convection," or vertical movement of moisture.  So in general, the lower the pressure the better chance of precipitation.
124552
Soil absorbs moisture. It has small openings and the water gets in the small holes. The cohesion and adhesion of the water constitute a force that keeps the water in the soil, to a certain extent.
235061
how about post-poned ( you know it not now but latter because of rain)
660157
Soil is the material on the surface of a lithosphere subject to weathering, and especially the earthy portion of that material.\n\nSoil components\n\n    * Composition -- A typical surface soil is half solids and half voids or porosity. Water and air are thus integral components of soils. Water occupies the void space between soil particles and is held by surface tension on particle surfaces. Air occupies the remaining void space. Both water and air components of soils are important to plant growth and other life in the soil profile of a particular ecosystem\n    * Soil texture -- refers to soil grain size, sand = 2 to 0.02 or 0.05 mm; silt = 0.02 or 0.05 to 0.002 mm; clay = <0.002 mm. Soil texture influences available water capacity and movement, fertility, and workability or "tilth". "Loam" is a name for one of various mixtures of these three particle sizes. The ratio of these particles determines soil texture classification.\n    * Soil structure -- the arrangement of soil particles into aggregates, which may have various shapes, sizes and degrees of development or expression. Soil structure influences aeration, water movement, erosion resistance, and root penetration.\n    * Slope -- the inclination of the ground surface. Slope influences runoff of rainfall, soil erosion, stability, and machinery operation.\n    * Soil color -- Soil color often indicates soil moisture status and is used for determining hydric soils. Often described using general terms, such as dark brown, yellowish brown, etc., soil colors are also described more technically by using Munsell soil color charts, which separate color into components of hue (relation to red, yellow and blue), value (lightness or darkness) and chroma (paleness or strength).\n    * Soil chemistry -- A complex subject within soil science; the most important subjects are:\n\n        Soil pH -- The acidity or alkalinity of soils, which affects plant growth and soil fertility.\n        Cation Exchange Capacity -- The soil's ability to retain and exchange positively charged ions, which include major plant nutrients.\n        Reduction and oxidation (Redox) reactions are also important.\n\n    * The soil profile -- A vertical cut that exposes soil layering or soil horizons. Horizons are formed by combined biological, chemical and physical alterations. A, B, and C symbols are used to describe the topsoil, subsoil and substratum, respectively.\n    * Permeability -- The ability of a soil to transmit water or air. Faster or greater permeability often occurs in sandy or gravelly soils due to large pore spaces. Slower permeability typically occurs in finer textured clay soils, or compacted soils with little structure.\n    * Drainage -- The rate in which water is removed from a soil. Drainage influences most uses of soils, whether for agriculture, silviculture or urban. Classes of soil drainage are those found in soil survey reports, such as well drained, moderately well drained, somewhat poorly drained, poorly drained, and very poorly drained. Soil color patterns (such as mottle patterns or redoximorphic features) often indicate soil drainage class. The most productive agricultural soils are typically well drained or moderately well drained, as are the soils easiest to develop for urban use. By contrast, hydric soils are poorly or very poorly drained. A soil's natural drainage rate can be significantly increased by subsurface "tile" drainage.\n    * Soil biology -- Soils serve as habitats for soil organisms varying in size from microorganisms to small animals. The character of soils is intricately tied to bioturbation and the biochemical functions performed by soil organisms. The soil is home to a large proportion of the world's genetic diversity, which changes by soil type: desert soils (like aridisols) generally have more complex soil biotic communities and genetic diversity than tropical soils (like oxisols).\n    * Soil smell -- earthy odor
624441
That answer is true.\n\nThe water table rises & falls in response to rainfall amounts.\n\nWhen there is little rain, the water table will lower thereby affecting the wells in surrounding areas.\n\nOn the flip side, when there are great amounts of rain, the water table will rise. Sometimes the rain is so great that the water table reaches the surface & the ground is saturated.
518077
yeah, if there is a landslide
1084845
When you throw freshly dried wheat in the air wheat falls immediately to the ground and the chaff is BLOWN AWAY\n\nhttp://web.odu.edu/webroot/instr/sci/plant.nsf/pages/tares\nhttp://www.emjc3.com/helland.htm
870765
The rain that falls on the land contains some dissolved carbon dioxide from the surrounding air. This causes the rainwater to be slightly acidic due to carbonic acid (which forms from carbon dioxide and water). The rain erodes the rock and the acid breaks down the rocks and carries it along in a dissolved state as ions. The ions in the runoff are carried to the streams and rivers to the ocean. Many of the dissolved ions are used by organisms in the ocean and are removed from the water. Others are not used up and are left for long periods of time where their concentrations increase over time.\n\nThe two ions that are present most often in seawater are are chloride and sodium. These two make up over 90% of all dissolved ions in seawater. By the way, the concentration of salt in seawater (salinity) is about 35 parts per thousand. In other words, about 35 of 1,000 (3.5%) of the weight of seawater comes from the dissolved salts; in a cubic mile of seawater the weight of the salt, as sodium chloride, would be about 120 million tons. And, just so you don't think seawater is worthless, a cubic mile of it also can contain up to 25 tons of gold and up to 45 tons of silver! Before you go out and try alchemy on seawater, though, just think about how big a cubic mile is.\n\nBy some estimates, if the salt in the ocean could be removed and spread evenly over the Earth’s land surface it would form a layer more than 500 feet (166 m) thick, about the height of a 40-story office building.
1104062
you must be seriously bored... are you serious about this one? its because the soil sokes the water making it wet
680007
when the rain season comes it makes the niles banks flood with water which for the farmers is actually a good thing because the ni le has a lot of nutrients and sediments in its soil and rocks so when it gets on shore it serves as a fertilizer for the plants ! ! ! ! !
260515
Apparently, lesser sunlight will get in. That will cause some imbalance on earth.