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Changes in soil properties are probably due to the presence of a continuous vegetation cover that enhances organic matter accumulation, water infiltration, sodium leaching and subsequently soil development.
Subsequently, soil was incubated using the standard incubation procedure as described above, but without the addition of concentrated root exudates.
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Subsequently, soils were extensively and accurately mixed by stirring with a spoon, and then transferred to glass beakers which were subsequently sealed by Parafilm®.
Subsequently, the soil was grubbed and then ploughed in the next spring.
Subsequently the soil was wet sieved to < 500 μm to recover granules and the granules were air-dried.
Subsequently, the soil was then air dried and mixed with different amounts of (d < 2 mm) wheat straw and alfalfa straw (0 and 5%% w/w) separately; afterward, the samples were mixed with different amounts of nanozeolite (0, 10, and 30%% w/w) and then were kept in field capacity moisture content and lab condition.
Subsequently, the soil was carefully shaken and washed off the roots of each plant.
These putative suppressors were first transferred to cytokinin-free media to recover, and subsequently to soil for self-pollination.
Small, ice-scoured hollows and small moraines (ridges of glacial debris) attest to those events, while over rather wider areas frost-shattered rocks that subsequently caused soils to flow down-slope (solifluction) have helped shape the surface.
Soil moisture levels subsequently increased and soils remained wetter for longer and were thus more prone to mass wasting (Pearce et al., 1987).
WWTP sludges, enriched with Ag and ZnO ENPs or their corresponding soluble metal salts during anaerobic digestion and subsequently mixed with soil (targeting a final concentration of 1400 and 140 mg/kg for Zn and Ag, respectively), were subjected to 6 months of ageing and leaching in lysimeter columns outdoors.
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