Loading ...
manure applicationresultedin higher soil organic carbon , active carbon , phosphorus , and water stable aggregates , and lower bulk density
The manure applicationhas clearly resultedin higher soil organic carbon , active carbon , phosphorus , and water stable aggregates , and lower bulk density
changing soil and site - specific factors , associated with the changing depth of the permafrost table due to thawinginfluencethe spatial distribution and variability of soil organic carbon ( SOC ) and total nitrogen ( N ) stocks in high - latitude mineral soils
factorsinfluencingorganic matter content , nutrient supply , soil vegetation cover and soil compaction
the experimental scenarioresultsin the very high recovery rates for total organic carbon and black carbon
the manure applicationresultedin higher soil organic carbon , active carbon , Phosphorus , and water stable aggregate
land management practiceswill influencesoil organic carbon , soil organic matter , water , sediment and agricultural chemical accumulation
Agricultural practices such as burning of biomass and deforestation and removal of native vegetationresultwidespread clearing of land and losses of organic carbon in vegetation and soils
Intensive agriculture has been well knownto causedecline in soil organic matter and nutrient content of the soils
Soil carbon loss ... tillagecausessoil aeration and soil aggregate destruction that increases the decomposition of soil organic carbon
Perennial vegetationresultedin significantly higher total soil carbon and stable aggregate content
No - tillcan contributeto higher soil organic matter and organic carbon content in soils
The composition of soil microbial communitiescan directly influencenutrient availability , C stability , and soil organic matter
The increased plant biomasscausedan increase in soil organic carbon and soil total nitrogen
by climate(passive) are influenced bysoil organic carbon ( SOC ) storage , crop yield , and yield stability
that the degradation of residues was notinfluencedby the soil organic carbon and pH. Dissipation data in soils
that the degradation of residues wasinfluencedby the soil organic carbon and pH. Dissipation data in soils
soil fertility ( fresultingfrom low organic carbon and total nitrogen contents of the soils
the type of the agroforestry system established(passive) is however influenced byThe amount of soil organic carbon ( SOC ) sequestered ... the soil and climatic conditions and management
land management practiceswill influencesoil organic carbon , soil organic matter , water , sediment and
Land use changescan influencesoil organic carbon content , fractions and stability
Rotation of cash crops with grazed cover crops and grazed perennial pasturescan contributeto surface soil organic carbon and nitrogen accumulation
the use of compost and bio compost at all levelsleadsto increase soil organic carbon , soil respiration and soil fertility
Long - term intensive cultivationleadsto the decrease of soil organic carbon ( SOC ) and soil fertility
Land usestrongly influencessoil organic carbon and bacterial community
black carbon(passive) is contributed byPresence in soils Up to 60 % of the total organic carbon stored in soils
by long - term fertilization application(passive) caused bysoil organic and soil total nitrogen
Nitrogen applicationsignificantly influencessoil organic matter and total nitrogen
sandy soilsinfluencevarious soil properties and soil organic carbon
degrade soil healthleadingto losses of soil organic carbon and soil fertility
by forest type change(passive) caused bysoil organic carbon mineralization rate
Soil propertiescontributingto soils aggregation Soil organic carbon fraction Soil organic carbon
addition of farmyard manure and agro - forestrywere contributingto sustainability of soil organic carbon and bulk density
black carbon(passive) is contributed byUp to 60 % of the total organic carbon stored in soils
by black(passive) is contributed byUp to 60 % of the total organic carbon stored in soils
by grassland degradation(passive) caused bysoil organic carbon and soil erosion
when a weight ( tire , piece of equipment , container , etc . ) compresses voids within the soilresultingin rearrangement of soil inorganic and organic material
this method(passive) can be caused bythis method
infiltration capacityinfluencedinfiltration capacity
the functional diversity of the soil microbial communities in rubber plantationsinfluencedthe functional diversity of the soil microbial communities in rubber plantations
to greater biological diversity in the soilleadsto greater biological diversity in the soil
alsocontributedalso
These factors(passive) are influenced byThese factors
in a better erosion control and increased plant available waterresultingin a better erosion control and increased plant available water
to this variationcontributingto this variation
in more plant - available mineral N and hence more vigorous crop growthresultin more plant - available mineral N and hence more vigorous crop growth
the maximum thaw depth in permafrost regionsinfluencesthe maximum thaw depth in permafrost regions
The spring wheat yield(passive) was significantly influenced byThe spring wheat yield
to assist in the processes of aggregationcontributeto assist in the processes of aggregation
by different land use systemsinfluencedby different land use systems
alsocan ... leadalso
to erosion and runoffleadingto erosion and runoff
to bacterial proliferationcan contributeto bacterial proliferation
from Forest Conversion to Maize Fields in Eastern ThailandResultingfrom Forest Conversion to Maize Fields in Eastern Thailand
from spring dust emission resultedfrom spring dust emission
from spring dust emission resultedfrom spring dust emission
to sustainable intensification of crop productioncontributesto sustainable intensification of crop production
a decrease in the bioavailability of contaminantscauseda decrease in the bioavailability of contaminants
Presence in soils(passive) is contributedPresence in soils
to soils that are more resilient to drought and extreme precipitation events , exactly the kinds of weather we can expect to see more of with climate changeleadsto soils that are more resilient to drought and extreme precipitation events , exactly the kinds of weather we can expect to see more of with climate change
to the functional signatures of particular nifH phylotypes in fields under no - till managementmight contributeto the functional signatures of particular nifH phylotypes in fields under no - till management
from 4.8 % in the Alfisolcontributedfrom 4.8 % in the Alfisol