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the way the sand grains are packed together.[6(passive) are directly influenced byThe porosity and permeability
the way the sand grains are packed together.[5(passive) are directly influenced byThe porosity and permeability
the way the sand grains are packed together.[7(passive) are directly influenced byThe porosity and permeability
the way the sand grains are packed together.[4(passive) are directly influenced byThe porosity and permeability
directly(passive) are ... influencedThe porosity and permeability
a careful selection of the grading curve , the former ( concrete ) getting to outcomes ( 17 % ) completely comparable to the corresponding values of a draining and noise - reducing asphalt pavement ( 18÷20%)[8(passive) are positively influenced byBoth porosity and permeability
groundwater ... where fracturing and weatheringhas createdporosity and permeability
the lithologic factorsinfluencedporosity and permeability in them
geological factorsinfluencingporosity and permeability
1.7 km / km2 Roads within 1 km of coast : 714 km Railway : Total length = 293 km WATER RESOURCES Highly fractured bedrockcreatesporosity and permeability
The nitrogen and oxygen of the atmosphere , if allowed to come in contact with the molten weld metalcauseporosity and brittleness
Facies variability , mineralogical composition , and sequence - stratigraphic origin ... additional factorsinfluenceporosity and permeability
linear or nonlinear deformation(passive) caused byporosity and permeability
the depositional pore - geometries of the reservoir sediments and the post - depositional diagenetic changes that take place(passive) are influenced byPorosity and permeability
that dolomitizationcreatesporosity and permeability
sustem(passive) are influencedBoth porosity and permeability
the size , gradation and angularity of the particles(passive) are directly influenced byPorosity and permeability
alteration in the upper part of the subducting slab(passive) caused byporosity and permeability contrasts
the components of porous media(passive) caused bythe porosity and permeability
being captured within the wall of the matrixpotentially causingporosity and delamination
Another mechanismto createporosity and permeability in carbonates
The colonic irrigationpreventspermeability , porosity and diverticulum
sol textureCreatehas on porosity and permeability
The way a rock is packed greatlyinfluencesits porosity and permeability
in - situ remobilization ( Duranti et al . , 2002(passive) caused byporosity and permeability
localized leaching of nonreservoir - quality rockto createenhanced porosity and permeability
the inclusion of silt in the shales(passive) created bysilt permeability and porosity
We 'd liketo createporosity and permeability
What is needed isto createporosity and permeability
different materialsto discovertheir porosity and permeability
intentionally(passive) is ... createdPorosity and permeability
weak mortars(passive) caused byporosity and permeability issues
the roles played by sedimentary facies (influenceporosity and permeability
the way the sand .. has been proposed for nomination to the Global Heritage Stone Resource(passive) are directly influenced byThe porosity and permeability
By fracking that shale , we ’re pumping sand into createthat porosity and permeability
the above phenomena(passive) caused byrock porosity and permeability
basement structural patterns and subaerial exposures(passive) influenced byporosity and permeability
The reservoir quality ... clay contentinfluencesporosity and possibly permeability
as targets to the network predictor(passive) are setCore porosity and permeability
the fracturing that precedes an earthquake(passive) caused byporosity and permeability
to higher sustainable oil flow ratesleadingto higher sustainable oil flow rates
to the loss of mechanical strengthleadingto the loss of mechanical strength
to suppression of fluid flowleadingto suppression of fluid flow
infiltration of waterpreventinginfiltration of water
extensive crack sealing ... locally impeding the solute diffusion ( at d > 100 μm ... so that stresses do not relaxcould causeextensive crack sealing ... locally impeding the solute diffusion ( at d > 100 μm ... so that stresses do not relax
the processes controlling salinity(passive) are ... influenced bythe processes controlling salinity
to loweringthe reservoirleadingto loweringthe reservoir
a portion of the undesirable particulate matter passing through the broken primary filter element to become embedded in the back - up filtercausesa portion of the undesirable particulate matter passing through the broken primary filter element to become embedded in the back - up filter
through the diagenesis and catagenesis of kerogencreatedthrough the diagenesis and catagenesis of kerogen
in a non - uniform flow pattern during liquid molding [ 114may resultin a non - uniform flow pattern during liquid molding [ 114
surface pondingcausingsurface ponding
to water management problems and massleadingto water management problems and mass
to optimize production at multiple specified intervalsdesignedto optimize production at multiple specified intervals
at time =are setat time =
the open cell(passive) caused bythe open cell
spacing ... while ground water level , quality and transmissivity are critical to ISR projectswill ... influencespacing ... while ground water level , quality and transmissivity are critical to ISR projects
a leak and make it unusable for holding pressure in marine applicationswould causea leak and make it unusable for holding pressure in marine applications
the storage and movement of groundwater influencethe storage and movement of groundwater
from precipitation of ferroan calcite ( Cresultingfrom precipitation of ferroan calcite ( C
in a mass of water storage , which is primarily derived from weak and fractured adjacent coal beds and formationsresultingin a mass of water storage , which is primarily derived from weak and fractured adjacent coal beds and formations
rapid rainwater evaporation and infiltrationcausingrapid rainwater evaporation and infiltration
an ideal setting for initial reaction of CO2createan ideal setting for initial reaction of CO2
to a reduction in the unconfined compressive strength of the cores under studyleadingto a reduction in the unconfined compressive strength of the cores under study
into improved specific capacitiesresultinginto improved specific capacities
from water - rock reactionsresultingfrom water - rock reactions
in increased entry of LNAPL into the rock matrixwill resultin increased entry of LNAPL into the rock matrix
from of a number of hydrogeologic factorsresultfrom of a number of hydrogeologic factors
drainageinfluencedrainage
the boiling rate(passive) caused bythe boiling rate
in a mass of groundwater storage , which causes a threat of groundwater inrush hazard to the safety of coal minesresultingin a mass of groundwater storage , which causes a threat of groundwater inrush hazard to the safety of coal mines
in high production ratesresultsin high production rates
from oolitic depositionresultingfrom oolitic deposition
in better well deliverabilityresultingin better well deliverability
in little or no surface runoffresultingin little or no surface runoff
to reducing reservoir qualityledto reducing reservoir quality
to flow restrictionsleadsto flow restrictions
to the imminent collapse of the Nigeria power sectoris gradually leadingto the imminent collapse of the Nigeria power sector