1. A key quality of the brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater is the carrying capacity, i.e. how well the ground supports a machine in brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater conditions.
2. This factor is of the utmost importance because it strongly brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater the possibility for driving a fully loaded forwarder.
3. If the carrying brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater is not taken into account the planning can go totally awry, causing vast additional costs, especially for the forwarding.
4. Furthermore, the carrying capacity can vary during timber brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater, e.g. due to changing weather conditions.
5. For example, the brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater may be hard as concrete initially at a site on till if harvesting brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater start at the end of a dry summer, but following persisting autumn brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater the ground at the site may be like liquid brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
6. Consequently, the water content of the soil strongly affects the ground’s brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater capacity and is a crucial brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater to consider when assessing it.
7. Other important factors are the soil type, brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater, hydrological parameters (water brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater), ground frost and the thawing of frozen brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
8. In addition, you must also try to assess how much the stumps and brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater reinforce the ground and thus improve the carrying capacity.
9. Clay soil is often referred to as "brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater[?]".
10. Clay soil that becomes too brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater can take a long time to restore to a good soil texture.
11. The wet quality of clay soil requires the addition of large amounts of organic brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater such as green plant material, animal manures, leaf mold and compost to improve its structure.
12. Contrary to sandy soil, clay soil has very small brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater with tiny pore spaces or brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
13. Since there are more pore spaces, brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater soil has a larger total pore space than sandy brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater, due to which the soil absorbs and retains more brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
14. This makes clay soils poorly aerated and poorly brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
15. Since clay soils have a high water-retentive capacity, they are prone to alternating brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater and brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater when the ground freezes and brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
16. When a clay soil dries, it crusts and brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
17. The cracking of the soil damages the brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater and other parts of the plants.
18. Water brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater and nutrient relations in forested soils on sloping topography greatly affect soil development and site brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater.
19. Water movement in soils is one of the most important brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater affecting soil genetic and morphological characteristics and, in turn, affects the vegetation.
20. Knowledge of water movement in forest soils on sloping brushwoodcapacitycarryingclaycompactedcontractioncracksdrainedexpansionfactorfactorsflowsgroundharvestingheavy soilinfluencesmattermicroporesmovementmudoperationsparticlesprecipitationqualityrainfallrootssoilterrainthawstopographyvaryingwater is necessary for better evaluation of the soil productivity and understanding soil development.