Sentence examples for most soil properties from inspiring English sources

The variability of most soil properties is expressed at small scales.

The paired mean difference and the correlation matrix of most soil properties between the different erosion statuses also showed significant differences.

The analysis of variance highlighted significant differences for most soil properties across landscape position and soil depth except for organic carbon (OC), total nitrogen (TN), and total phosphorus.

Classification based on ECa significantly delineated most soil properties evaluated (0 0.3 and/or 0 1.2 m) and effectively reduced MS error (P ≤ 0.10).

In addition to changes in spatial patterns, most soil properties were elevated in the reclaimed soil, compared with the undisturbed soil.

Because most soil properties showed little variability for soils occurring in floodplains for all six rivers, botanical assessments will be needed to determine the magnitude of the role the properties have toward defining ecological sites.

Soil texture and pH were the most important soil properties in explaining variations in AGB, with stronger effects than soil nutrients.

Using coefficient of variation (CV) as criteria for expressing variability, Ca, TON, Mg, SOC and silt were most variable soil properties for the 0 20 cm depth.

The particle size fractions and relative bulk density were identified as most important soil properties for the prediction of shrinkage indices.

The objectives of the study were to find the most important soil properties that discriminated among eight New Zealand Soil Orders and determine relationships between Soil Orders and early tree growth rates for P. radiata and Cupressus lusitanica.

The most variable soil properties (CV > 0.38) were nitrogen (N), electric conductivity (ECd), exchangeable bases (ExBas), boron (B), calcium (Ca), potassium (K), magnesium (Mg), manganese (Mn) and phosphorus (P).