The inhibition of soil urease activity by the accumulation of soluble salts
in a coastal region of the Sultanate of Oman susceptible to salinization w
as investigated. Soil transects around six individual date paints (Phoenix
dactylifera L.) growing on commercially managed farms were intensively samp
led and assayed for soil urease activity. Activities ranged from 0.10 to 39
.85 mu g NH4+ released g(-1) soil h(-1) at 37 degrees C. Soil collected fro
m within 70 cm of the palms had a higher urease activity than soil from a d
istance > 1.5 m. Multiple I egression analysis showed that more than 75% of
the variance in soil urease activity was accounted for by soil physicochem
ical properties, except in sandy soils low in organic carbon (C). The soil
properties most closely associated with urease activity were soil organic C
, salinity, and texture. A scattergram of urease activity against salinity
showed high variability in activity at low salinities (<0.5 dS m(-1) in 1:5
soil to water extracts) and severe inhibition at salinity values >12 dS m(
-1). In nonsaline soils, variation in urease activity was closely associate
d with variations in organic C and clay contents, whereas at saline conditi
ons, only soil salinity was significantly associated with urease activity.