Loading ...
of a range of dissolved salts , such as NaCl(passive) is composedThe soil solution of saline soils
Another consequence of climate change ... the prolonged drought in Australiaresultedin high saline soil
industrial agricultural practices(passive) caused byhigh saline soils or impoverished soils
of a range of dissolved salts , such as NaCl , Na2SO4 , MgSO4 , CaSO4 , MgCl2 , KCl , and Na2CO3 , each of which contribute to salinity stress(passive) is composedThe soil solution in saline soils
a high water table too close to the soil surface(passive) are caused bySoil Saline soils
Indiscriminate and unscientific irrigationresultedin marshy land and saline soils
also(passive) are ... causedSalt affected soils
In dry regions , salts may accumulate over timeleadingto naturally saline soils
excess accumulation of salts(passive) are caused bySalt affected soils
In dry regions salts may accumulateleadingto naturally saline soils
Salts may accumulate in dry regionsleadingto naturally saline soils
Groundwater ... dissolved saltscausesaline - affected land
by human activities and natural factors(passive) caused bysoil salinity
by the water(passive) caused bySoil salinity
the application of irrigation water that is high in dissolved salts , particularly sodium , chlorine , and boron(passive) is often caused bySoil salinity
dissolved saltscausesaline - affected land
also(passive) can ... be causedSoil salinity
by natural(passive) caused bysoil salinity
by climate change associated with rising sea level(passive) caused bySoil salinity
by the concentration and composition of dissolved salts(passive) is influenced bysoil salinity
by winter road maintenance using salt ( NaCl(passive) caused bysoil salinity
often(passive) is ... causedSalinity of the soil
2 ) additional layers of informationcan influencesoil salinity
by John C. Cochrane(passive) designed bySaline Countywas
the main factorinfluencingsoil salinity
by rising sea - levels and storm surges(passive) caused bysoil salinity
poor - quality irrigation water , lack of precipitation and capillary wicking from a high water table(passive) can be caused bySoil salinity
Applications of saline and/or sodic water without adequate leaching or in the presence of a high water table will increase soil EC over timeeventually resultingin saline soil
water table will increase soil EC over timeeventually resultingin saline soil
growth habitresultingfrom saline soil
by deicers(passive) caused bysaline soil
Even more detrimental , seawater mixed back in along the new rivercausedthe soil to have saline in it
saltsleadsto reh ( saline soils
A common problem of coastal and mountain regionsresultsaline soils
by seawater intrusions(passive) caused bysaline groundwater
by rising seas(passive) caused bysaltier soils
rising seas(passive) caused bysaltier soils
CO2 storage(passive) caused bysaline aquifers
of porous rock , filled with brine(passive) are composedsaline aquifers
a dynamic situation(passive) is caused bySaline seep
boron toxicityto causeboron toxicity
a white efflorescence on the surfacecausesa white efflorescence on the surface
in poorresultin poor
poor plant growthcausepoor plant growth
in less soil organic carbon ( SOCresultingin less soil organic carbon ( SOC
in a strong presence of this invasive species along stretches of sandy , semiarid regionshas resultedin a strong presence of this invasive species along stretches of sandy , semiarid regions
Salt stress(passive) caused bySalt stress
the problems(passive) caused bythe problems
significantly to the OC storage in the semiarid soils of the Kulunda steppecontributesignificantly to the OC storage in the semiarid soils of the Kulunda steppe
to saline groundwater ... Fig . 7.19leadsto saline groundwater ... Fig . 7.19
by different strains of cyanobacteriainfluencedby different strains of cyanobacteria
bare areas(passive) caused bybare areas
problems(passive) caused byproblems
problems(passive) caused byproblems
stunted plant growth , lower yieldcausesstunted plant growth , lower yield
several difficulties in the irrigationcausesseveral difficulties in the irrigation
ion stress(passive) caused byion stress
osmotic stress(passive) caused byosmotic stress
high sodium levelshave causedhigh sodium levels
to an increase in the soil respiration , microbiological activity , cation exchange capacity , and activity of the enzymes LiP and Lacledto an increase in the soil respiration , microbiological activity , cation exchange capacity , and activity of the enzymes LiP and Lac
up to 93 % yield loss in tefcausesup to 93 % yield loss in tef
problems(passive) caused byproblems
groundwater pollutioncausinggroundwater pollution
a variety of side effects which are dependent on the patientcan causea variety of side effects which are dependent on the patient
to salinizationleadingto salinization
major problems for farmers as they halt the movement of water , preventing uptake by crops , making production non - existentcausemajor problems for farmers as they halt the movement of water , preventing uptake by crops , making production non - existent
the long term use of chemical fertilizers harm(passive) caused bythe long term use of chemical fertilizers harm
the long term use of chemical fertilizers harm(passive) caused bythe long term use of chemical fertilizers harm
from irrigationresultfrom irrigation
chemical fertilizers harm(passive) caused bychemical fertilizers harm
usuallyresultusually
GPR penetration(passive) caused byGPR penetration
usuallydo ... causeusually
less than 0.2 % of river discharge , but 0.04 to 39 % of major ion concentrations in the rivers , with highest contributions under winter low - flow conditionscontributedless than 0.2 % of river discharge , but 0.04 to 39 % of major ion concentrations in the rivers , with highest contributions under winter low - flow conditions
less than 0.2 % of river discharge ... but 0.04?39 % of major ion concentrations in the rivers , with highest contributions under winter low - flow conditionscontributedless than 0.2 % of river discharge ... but 0.04?39 % of major ion concentrations in the rivers , with highest contributions under winter low - flow conditions
to the salinization of shallow groundwaterleadingto the salinization of shallow groundwater
from industry sourcesoriginatingfrom industry sources
23?39 % of average monthly Cl flux and 18?32 % of average monthly Na fluxcontributed23?39 % of average monthly Cl flux and 18?32 % of average monthly Na flux
back from the waterfrontsetback from the waterfront
precipitationcausingprecipitation