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Qaagi - Book of Why

Causes

Effects

crystallization of ice within the larger soil voids and usually a subsequent extension of this ice to form continuous ice lenses , layers , veins , or other ice masses(passive) is caused byFrost heaving of soil

crystallization of ice within the larger soil voids and usually a subsequent extension to form continuous ice lenses , layers , veins , or other ice masses(passive) is caused byFrost heaving of soil

Cold weathercan causefrost to form in the soil

The volumetric tensions arising due to changes in temperature of ground within the annual range of temperature variationscan leadto frost cracking of soil masses

freezing temperaturescan causefrost heaves in the soil

the seasonal freeze - thaw effectcausesfrost heaves in the surrounding soil

Mulching preserves soil temperaturepreventsfrost heave in the soil

The deflection of the pilecausesstrains in the soil mass

the fascinating shapes and textures(passive) created bythe fascinating shapes and textures

very costly problems in various constructions like highways , airport pavements , railways , pipelines and building foundations in the urban cold regions of the worldcausesvery costly problems in various constructions like highways , airport pavements , railways , pipelines and building foundations in the urban cold regions of the world

to formation of intricate , repetitive patterned ground featuresleadto formation of intricate , repetitive patterned ground features

to higher rates of basal heterotrophic CO2 production in surface soil samplesalso ledto higher rates of basal heterotrophic CO2 production in surface soil samples

the wire shortcausedthe wire short

sub - base movement , such as(passive) caused bysub - base movement , such as

problems for gardenerscan also causeproblems for gardeners

push the posts up and out of the groundcan causepush the posts up and out of the ground

a circular split on the cast iron water maincausinga circular split on the cast iron water main

to significantly higher concentrations of dissolved organic carbon ( DOCledto significantly higher concentrations of dissolved organic carbon ( DOC

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