Impact of basidiomycete fungi on the wettability of soil contaminated with a hydrophobic polycyclic aromatic hydrocarbon

Soil water repellency and micro-aggregate fractions in response to crop growth periods in a sloping cropland subjecting to long-term fertilization management

Fertilization management and crop growth can affect soil water repellency (SWR) through altering other soil properties such as micro-aggregate, soil organic carbon (SOC) and total nitrogen (TN). However, the extents and magnitudes of these effects remain unclear. This study aimed to determine the effects of different crop growth periods and long-term fertilization managements on SWR and selected soil physicochemical properties and their linkages. Soil samples were collected from agricultural plots experiencing different maize growth periods (ES, elongation stage; TS, tasseling stages; FS, filling stage; and MS, maturity stage) and fertilization managements (CK, no fertilizer with downslope cultivation; T1, combined manure and chemical fertilizers with downslope cultivation; T2, chemical fertilizer with downslope cultivation; T3, 1.5-fold chemical fertilizer with downslope cultivation; T4, chemical fertilizer with contour cultivation) in a representative sloping cropland with Entisols, southwest China. SWR, micro-aggregate fractions, and other physiochemical properties like soil organic carbon (SOC) and total nitrogen (TN) were determined. Results showed that SWR increased by 64.93% in T1 than in CK, and fertilization managements (i.e., T1, T2, T3, and T4) markedly increased soil 1000-250 μm fraction by 34.50-50.74% and reduced 250-50 μm fraction by 22.95-48.87% than CK did. SWR was 27.35%-78.74% higher in ES than that in other growth periods. The highest soil 250-50 fractions (30.80%) and the lowest <50 μm fractions (43.95%) both appeared in TS. SOC was both differed by fertilization management and growth period, while TN was only affected by the former. SWR was predicted well by TN alone. Our results indicate that long-term fertilizer application enhances SWR and have great significance for optimizing sustainable agricultural management in the similar sloping croplands.

Wildfire effects on lipid composition and hydrophobicity of bulk soil and soil size fractions under Quercus suber cover (SW-Spain)

Soil water repellency (hydrophobicity) prevents water from wetting or infiltrating soils, triggering changes in the ecosystems. Fire may develop, enhance or destroy hydrophobicity in previously wettable or water-repellent soils. Soil water repellency is mostly influenced by the quality and quantity of soil organic matter, particularly the lipid fraction. Here we report the results of a study on the effect of fire on the distribution of soil lipids and their role in the hydrophobicity grade of six particle size fractions (2-1, 1-0.5, 0.5-0.25, 0.25-0.1, 0.1-0.05 and <0.05mm) of an Arenosol under Quercus suber canopy at the Doñana National Park (SW-Spain). Hydrophobicity was determined using water drop penetration time test. Field emission scanning electron microscopy (FESEM) was used to assess the presence and morphology of the inorganic and organic soil components in the particle size fractions. Soil lipids were Soxhlet extracted with a dichloromethane-methanol mixture. Fatty acids (FAs) and neutral lipids were separated, derivatized, identified and quantified by gas chromatography/mass spectrometry and gas chromatography/flame ionization detection. The hydrophobicity values of soil samples and fractions were statistically different (P < 0.05), for both, the unburnt and burnt soils, and particle size fractions. All samples displayed a similar distribution of FAs, straight-chain saturated acids in the C₁₄-C₃₂ range, and neutral lipids (n-alkan-1-ols, n-alkanes), only differing in their relative abundances. Among possible biogeochemical mechanisms responsible for the changes in soil lipids, the observed depletion of long chain FAs (C_≥24) in the coarse fraction is best explained by thermal cracking caused by the heat of the fire. The enrichment of long chain FAs observed in other fractions suggests possible exogenous additions of charred, lipid-rich, material, like cork suberin or other plant-derived macromolecules (cutins). Principal component analysis was used to study the relationships between hydrophobicity with soil organic matter and its different components. Extractable organic matter (EOM) and specifically long chain FAs content were positively correlated to soil hydrophobicity. Therefore, the latter could be used as biomarkers surrogated to hydrophobicity in sandy soils.