Transport and retention of perfluorooctanoic acid (PFOA) in natural soils: Importance of soil organic matter and mineral contents, and solution ionic strength

2019 ◽  
Vol 225 ◽  
pp. 103477 ◽  
Author(s):  
Xueyan Lyu ◽  
Xing Liu ◽  
Yuanyuan Sun ◽  
Rong Ji ◽  
Bin Gao ◽  
...  
2012 ◽  
Vol 92 (1) ◽  
pp. 153-164
Author(s):  
Isabelle Turcotte ◽  
Sylvie A. Quideau

Turcotte, I. and Quideau, S. A. 2012. Phenolic profiles in natural and reconstructed soils from the oil sands region of Alberta. Can. J. Soil Sci. 92: 153–164. This research was conducted in the Athabasca oil sands reclamation area of northeastern Alberta, where land reclamation entails reconstruction of soil-like profiles using salvaged materials such as peat and mining by-products. Successful reclamation is in part dependent on the quality of the organic capping of these reconstructed soils. This study investigated organic matter composition between reconstructed and natural soils. Soil samples (0–10 cm) were taken from 45 plots to represent a range of reclaimed and undisturbed sites. The botanical origin of soil organic matter was characterised through cupric oxide oxidation, which yields lignin monomers hypothesized to reflect vegetation inputs and extent of decomposition based on time since reclamation. Additional soil organic matter parameters were obtained using acid hydrolysis, physical separation and ramped cross polarisation C-13 nuclear magnetic resonance techniques. Yields of vanillyl phenols, coumaryl phenols, p-hydroxy phenols, summed lignin phenols and total phenolic constituents were significantly higher in natural soils than in reconstructed soils. We suggest that there may be an accelerated decomposition of peat phenols in reconstructed soils, which would leave only those phenols representative of the vascular plant history accumulated in the initial peat profile.


2021 ◽  
Vol 9 (3) ◽  
pp. 294-304
Author(s):  
Zakaria Ait lhaj ◽  
◽  
Abdelmajid Zouahri ◽  
Oualid Abboussi ◽  
Hind Ibork ◽  
...  

Leaf mineral composition reflects the complex interaction between soil, climate, and plant genetic and epigenetic background in terms of organic and inorganic composition. The present study aimed to evaluate the effect of seven soil compositions on the mineral contents of Strawberry leaves (Arbutus unedo) under Moroccan conditions. The obtained results demonstrated a significant positive correlation between the soil nitrogen, phosphorus, and potassium levels and their levels in the Strawberry plant leaves. Also, a positive relation was reported between the soil organic matter and the level of manganese and phosphorus in leaves. Moreover, a significant negative correlation was demonstrated between the soil organic matter and the plant pH level. These correlations were confirmed by the principal component analysis (PCA) which demonstrated the presence of three principal components accounting for 54.42% of the total variations, reflecting the important proportions of the various patterns of mineral and organic traits among accessions. In PCA, the most discriminative traits were clustered in PC1 and PC2. These findings may highlight the specific mineral needs for the A. unedo plant for its optimal cultivation and subsequent domestication in Morocco.


1962 ◽  
Vol 54 (5) ◽  
pp. 470-470
Author(s):  
T. M. McCalla

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