Sentence examples for sediment loam from inspiring English sources

The surface geology moving inland is sand-rich sediment, loam formations, mud-rich sediment, sand, and then loam formations, with the strata formed by the weathering of volcanic ash deposits in the terrestrial area (Fig. 8a; right).

Our laboratory determined sorption differences between tylosin A and B in loam sediment at an initial concentration of 50 μg/mL equilibrated between sediment and aqueous phase for 24 h.

Similarly, the loam sediment exhibits some non-linearity (npH5 = 1.15, npH7 = 1.18, npH9 = 1.19), but to a lower extent.

The higher clay content in the loam sediment has a weaker buffering capacity relative to OM [47].

Our experimental values indicate that tylosin sorption (Table 3) is linear over 3 orders of magnitude in the sandy loam sediment at pH 5 and 7 (npH5 = 0.993, npH7 = 1.05).

The factors and levels were (i) sediment types (clay loam, clayey and sandy); (ii) different inoculums (Sphingomonas sp., a mixture of Sphingomonas sp. and Mycobacterium sp., and without inoculum); (iii) presence of other PAHs (fluorene, pyrene, and none); and (iv) different salinities (5, 15 and 25 ppt).

The terracing greatly reduced surface water flow through the entrapment of sandy loam sediments behind it.

The sorption isotherm we determined for sulfamethazine (Figure 2) illustrates that Kd generally decreases with increase in pH for both loamy sand and loam sediments.

Two different plant species were tested, Lolium perenne and Trifolium repens, after 2 and 4 months of plant growth and for 2 different incoming silty-loam sediment concentrations.

At Heimdaljordet, typically laminated intertidal silty clay loam sediments were sealed by beach sands, into which, for example, a boat grave was dug.

Soils were comprised of nutrient poor sandy chestnut soils on sand and loam sediments (see Table S1 for soil chemical properties).