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of different layers(passive) are composedSoil Profile Soils
of a series of horizons or layers of soil stacked one on top of the other(passive) is composedThe soil profile
12,500 years ... enough timeto createa soil profile
of sand and sabkha layers(passive) was composedThe soil profile
of horizons ( horizontal layers of soil ) which may be characterized by physical , chemical , and biological properties(passive) is composedThe soil profile
a number of soil horizons each characterized by individual soil properties(passive) composed bya soil profile
Three main layers or horizonscreatethe soil profile
a number of distinctly different Soils Color Structure Texture Depth Soil Horizons(passive) is created byThe Soil Profile
of different soil horizons having different vertical extensions di [ mm ] and different soil textures(passive) can be composedThe soil profile
all layers as they were entered in the " Field Tests " frame(passive) is createdthe soil profile
plants and animals which can lead to the development of contrasting A & B Horizons(passive) caused bythe soil profile
of soil layers which are subdivided into equally spaced intervals ( the compartments(passive) is composedThe soil profile
of three layers : a highly permeable sandy loam ( alluvial terrace ) overlying a gravelly sandy till that covers a friable sandy to silty shale(passive) is composedThe soil profile
More mature soils will develop a variety of horizons unique to their environmental conditionscreatinga soil profile
characteristics of the sitecould influencethe soil profile
predominantly(passive) is composedThe soil profile
the natural groundwater table ... constantly high enoughto influencethe soil profile
all the morphological characters , climate and land use practices(passive) is influenced byThe soil profile
wheel traffic by using the fem plaxis code Author(passive) caused bysoil profile
that the weathered bedrock under hillslopes acts like a sponge to hold “ rock moisture(passive) has been discovereda soil profile
of 20 m of loose sand(passive) is composedThe soil profile
tractor wheelings(passive) caused bythe soil profile
Examining the characteristics of the soil at various levels enables scientiststo createa soil profile
The type and depth of these horizonscreatethe soil profile
Manure solutions resulting from surface runoff ... whose leachingcausessalinization of the soil profile
These horizons combineto createa soil profile
a slice of the side of the holewill createa soil profile
This augmentationleadsthe soil profile
of an O horizon ( < 3 cm thick ) , an A horizon ( 40 - 50-cm Figure 1 : Location of the study site in Nagano Prefecture , Japan(passive) is composedThe soil profile
surface runoff after rainfall and water is available for the trees until the next growth phase ( [ 35(passive) caused bythe soil profile
natural factors or machinery traffic(passive) caused bythe soil profile
the plant residue biodegradation(passive) created bythe soil profile
To begin sampling , you needto createa soil profile
stratified soil(passive) caused bythe soil profile
from the data downloaded from STATSGO developed by the US National Cooperative Soil Survey(passive) was createdThe soil profile
humans or parent materialhave influencedsoil profile
of 6 horizons(passive) is typically composedA soil profile
to allow the perfect balance between drainage and moisture retention(passive) was designedThe soil profile
plant roots(passive) created bythe soil profile
The makeup of all of the horizons in a soilcreatethe soil profile
to soil shrinkage and subsidencecontributingto soil shrinkage and subsidence
of silty sand , sandy lean clay , clayey sand , & sandy - Foundation engineering - Eng - Tips Skin Resistance for a soil profile composed of silty sand , sandy lean clay , clayey sand , & sandy thread256 - 406809 13composedof silty sand , sandy lean clay , clayey sand , & sandy - Foundation engineering - Eng - Tips Skin Resistance for a soil profile composed of silty sand , sandy lean clay , clayey sand , & sandy thread256 - 406809 13
in the water table rising to the surfaceresultingin the water table rising to the surface
of sand , clay , and limestoneis composedof sand , clay , and limestone
the water table to rise and eventually to intercept the soil surfacecausingthe water table to rise and eventually to intercept the soil surface
of alternating clay , silty sand layersis composedof alternating clay , silty sand layers
of silty sand , sandy lean clay , clayey sand , & sandy GeoPaveTraffic ( Geotechnicalcomposedof silty sand , sandy lean clay , clayey sand , & sandy GeoPaveTraffic ( Geotechnical
of several layers : litter ... organic material , and humus make up the O horizon ; sand , silt , and clay from the topsoil or A horizonis composedof several layers : litter ... organic material , and humus make up the O horizon ; sand , silt , and clay from the topsoil or A horizon
of alternating hard sandy clay and dense to very dense clayey sand layers down to 110 m while sandstone is encountered below this depthis composedof alternating hard sandy clay and dense to very dense clayey sand layers down to 110 m while sandstone is encountered below this depth
of Saturated brown clay under the pavementis composedof Saturated brown clay under the pavement
from out of season rainfall or the impact of temperature or soil fertilityresultingfrom out of season rainfall or the impact of temperature or soil fertility
turgidity of coffee plants at three different agroclimatesinfluencingturgidity of coffee plants at three different agroclimates
a challenging environment for optimal growth of the turfgrasscreatesa challenging environment for optimal growth of the turfgrass
to productive soils available for growing cropscontributingto productive soils available for growing crops
from tillageresultingfrom tillage
salinity of the surface soil layers and water logging in the deep onescausingsalinity of the surface soil layers and water logging in the deep ones
in more subsoil moisture that can be utilized by crops as well as channels for the following crop to followresultingin more subsoil moisture that can be utilized by crops as well as channels for the following crop to follow
of rock particles typically located beneath the organic - rich soil horizonspredominantly composedof rock particles typically located beneath the organic - rich soil horizons
of clay loampredominantly composedof clay loam
to increasing soil salinationleadingto increasing soil salination
to soil erosion and nutrient loss , as well as the effects of surface water run - offleadingto soil erosion and nutrient loss , as well as the effects of surface water run - off
to plant uptakecontributesto plant uptake
in less rainfall running offresultingin less rainfall running off
a cha decreasing soil compaction and leaving a better playing area for oxygen and nutrients to drain into the soil rootcreatinga cha decreasing soil compaction and leaving a better playing area for oxygen and nutrients to drain into the soil root
to a decline in vegetation conditionleadingto a decline in vegetation condition
to yet further erosionleadingto yet further erosion
in a low vulnerability arearesultingin a low vulnerability area
air spaces for roots to develop which also allows for faster percolation of rainfall through the soil profilecreatingair spaces for roots to develop which also allows for faster percolation of rainfall through the soil profile
to little changes in overall carbon levelsleadingto little changes in overall carbon levels
The extent to which the root systems of tomato plants develop(passive) is influenced byThe extent to which the root systems of tomato plants develop
to the potential of increased runoffleadingto the potential of increased runoff
to be very damp for some time to comeis setto be very damp for some time to come
the loss of irrigation water via deep percolationpreventthe loss of irrigation water via deep percolation
up ... especially on some of our more sandy country.²to setup ... especially on some of our more sandy country.²
from siltation from flooding , faulty construction , or inappropriate topdressing programmeresultingfrom siltation from flooding , faulty construction , or inappropriate topdressing programme
in a better growing medium for rootsresultingin a better growing medium for roots
to poorer root growth and less movement of waterleadingto poorer root growth and less movement of water
of distinguishable layers of sedimentnormally composedof distinguishable layers of sediment
to a healthier , more resilient and even more drought tolerant lawnleadingto a healthier , more resilient and even more drought tolerant lawn
The extent to which the root systems of pepper plants develop(passive) is influenced byThe extent to which the root systems of pepper plants develop