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Marcos Paradelo Perez

Bio: Marcos Paradelo Perez is an academic researcher from University of Greenwich. The author has contributed to research in topics: Alkali soil & Bioavailability. The author has an hindex of 1, co-authored 1 publications receiving 1 citations.

Papers
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TL;DR: In this article, the influence of three commonly used fertilizers (Di-ammonium Phosphate (DAP), Urea, and cow-manure) on the bioavailability of soil fluoride in an alkaline soil was investigated.

10 citations


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29 Nov 2021
TL;DR: In this article, a review of biological processes for fluoride remediation, i.e., bioaccumulation in plants and microbially assisted systems, is presented, which recommends the practical applicability and sustainability of microbial bioremediation of fluoride in different environments.
Abstract: Fluoride is widely found in soil–water systems due to anthropogenic and geogenic activities that affect millions worldwide. Fluoride ingestion results in chronic and acute toxicity, including skeletal and dental fluorosis, neurological damage, and bone softening in humans. Therefore, this review paper summarizes biological processes for fluoride remediation, i.e., bioaccumulation in plants and microbially assisted systems. Bioremediation approaches for fluoride removal have recently gained prominence in removing fluoride ions. Plants are vulnerable to fluoride accumulation in soil, and their growth and development can be negatively affected, even with low fluoride content in the soil. The microbial bioremediation processes involve bioaccumulation, biotransformation, and biosorption. Bacterial, fungal, and algal biomass are ecologically efficient bioremediators. Most bioremediation techniques are laboratory-scale based on contaminated solutions; however, treatment of fluoride-contaminated wastewater at an industrial scale is yet to be investigated. Therefore, this review recommends the practical applicability and sustainability of microbial bioremediation of fluoride in different environments.

8 citations

Journal ArticleDOI
TL;DR: Zhang et al. as discussed by the authors investigated the fluorine distribution and pollution level in soil in soda saline-alkali soil areas of western Jilin Province and found that rice planting increased the content of macroaggregates with diameters >2 and 2-0.25 mm.

6 citations

Journal ArticleDOI
TL;DR: In this article , the effects of soil fluoride on morpho-physiological growth characteristics of wheat, soil F contents, and bioavailability and uptake of F, phosphorus (P), sulphur (S), potassium (K), calcium (Ca), magnesium (Mg), aluminium (Al), iron (Fe), manganese (Mn), silicon (Si) and zinc (Zn) by wheat were investigated.

5 citations

Journal ArticleDOI
TL;DR: Wang et al. as mentioned in this paper used the hazard index (HI) to assess exposure risk from multiple exposure routes, and the results revealed that there is considerable F contamination in soil and crops in the study area.

4 citations

Journal ArticleDOI
TL;DR: In this article , the efficacy of fermented seaweed (Eucheuma cottonii) on the remediation of fluoride-contaminated soil was investigated and the soil was amended with either 1.25, 3.0, or 5.0% (w/w) FSW, parallel with the controls (0%).
Abstract: This study investigated the efficacy of fermented seaweed (Eucheuma cottonii) on the remediation of fluoride-contaminated soil. The soil was amended with either 1.25, 3.0, or 5.0% (w/w) fermented seaweed (FSW), parallel with the controls (0%). The amendment improved the physicochemical properties of the soil particularly pH regulated from strong alkaline (9.3) to neutral (7.0) which is essential for germination, crop growth, and yield. The amount of water soluble-fluoride (Ws-F) dropped from 81.7 ± 3.1 mg/kg to 42.7 ± 2.4, 33.7 ± 1.2, 19.6 ± 0.9, and 12 ± 1.3 mg/kg following 0, 1.25, 3, and 5% amendment dosage, respectively. Most of the Ws-F was converted into exchangeable fluoride (Ex-F) and to fluoride-bound to iron and manganese (Fe/Mn-F). Furthermore, the amendment also enhanced microbial mass and diversity in the soil. The FSW contains organic acids which participate in ionic bonding with the multivalent cations in the soil. The formed compound participates in ion exchange with clay or with anionic adsorption to positively charged clay sites at the edges. This interaction is further essential for enhancing the fluoride holding capacity of the soil. The use of seaweed reduced the bioavailability of fluoride in the agricultural soils and had positive effects on promoting soil fertility. However, further studies to observe its effects on crop performance is of significance.

2 citations