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However, the increase was only by 45% in soil 1.
The most significant CBZ biodegradation occurred in soil 1 under aerobic conditions.
However, N application promoted significant tissue K concentration in soil 1.
Soil 1 had a long history of irrigated urban vegetable production using polluted river water.
While soil 1 and 2 do not differ in their clay content (around 7 8%) they differ significantly in the silt/sand ratio with 74/19 (soil 1) to 38/54 (soil 2).
Despite same clay content soil 1 showed significantly higher levels of exchangeable cations is thus a result of the several times higher carbon content of soil 1 (1.9%) compared to soil 2 (0.3%).
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Little information has been gathered about T. gondii detection in water and soil [ 1, 4, 7, 13, 17, 27, 28, 30, 36, 38].
All this activity makes the rhizosphere, the most dynamic environment in soil [1].
Also, in this aggregate size class, the amounts of OC increased from 10%% nanozeolite 3.27 (g Kg soil −1 ) and zeolite 2.91 (g Kg soil −1 ) in (10 % zeolitic materials plus 5%% alfalfa straw) treatment to 30%% nanozeolite 3.93 (g Kg soil −1 ) and zeolite 3.54 (g Kg soil −1 ) in (30%% zeolitic materials plus 5%% alfalfa straw) treatment.
The amount of OC increased from 2.16 (g Kg soil −1 ) in control to 3.93 and 3.54 (g Kg soil −1 ) in compound A and compound B, respectively, in aggregate size fraction (>2 mm).
Silty sand mixed with lateritic soil (1 1 by volume) sourced from Phitsanulok is used as backfill material.
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