Investigation on the potential of eco-friendly bio-char for amendment in serpentine soils and immobilization of heavy metals contaminants: a review

Author(s):  
Arvind Kumar ◽  
Duraisamy Ramamoorthy ◽  
Naveen Kumar ◽  
Ravikant Verma ◽  
Agam Kumar ◽  
...  
2015 ◽  
Vol 63 (2) ◽  
pp. 47 ◽  
Author(s):  
S. Majid Ghaderian ◽  
Rasoul Ghasemi ◽  
Faeze Hajihashemi

Serpentine soils are often characterised by high concentrations of heavy metals, high plant diversity and endemism, and, in some cases, the presence of plants that hyperaccumulate nickel (Ni). Nickel uptake by hyperaccumulator plants could potentially be affected by other heavy metals in serpentine soils, such as manganese (Mn), which competes for uptake at roots. The present study investigated interactions between Ni and Mn in metal uptake, translocation and storage in a serpentine-endemic Ni-hyperaccumulator plant, Alyssum bracteatum (Brassicaceae), native to western Iran. The results based on a factorial treatment of seedlings using Ni and Mn and elemental analyses showed that whole shoot and root Ni concentrations were inversely correlated with Mn in the growing medium. Likewise, whole shoot and root Mn concentrations were inversely correlated with Ni in the medium, suggesting competition between Ni and Mn for uptake at roots. No evidence was found for competition between Ni and Mn for translocation between the roots and shoot.


Soil Systems ◽  
2021 ◽  
Vol 5 (2) ◽  
pp. 34
Author(s):  
George A. Meindl ◽  
Mark I. Poggioli ◽  
Daniel J. Bain ◽  
Michael A. Colón ◽  
Tia-Lynn Ashman

Serpentine soils are a stressful growing environment for plants, largely due to nutrient deficiencies and high concentrations of toxic heavy metals (e.g., Ni). Plants have evolved various adaptations for tolerating these extreme environments, including metal hyperaccumulation into above-ground tissues. However, the adaptive significance of metal hyperaccumulation is a topic of debate, with several non-mutually-exclusive hypotheses under study. For example, the inadvertent uptake hypothesis (IUH) states that heavy metal accumulation is a consequence of an efficient nutrient-scavenging mechanism for plants growing in nutrient-deficient soils. Thus, it is possible that metal hyperaccumulation is simply a byproduct of non-specific ion transport mechanisms allowing plants to grow in nutrient-deficient soils, such as serpentine soils, while simultaneously tolerating other potentially toxic heavy metals. Furthermore, some nutrient needs are tissue-specific, and heavy metal toxicity can be more pronounced in reproductive tissues; thus, studies are needed that document nutrient and metal uptake into vegetative and reproductive plant tissues across species of plants that vary in the degree to which they accumulate soil metals. To test these ideas, we grew nine plant species that are variously adapted to serpentine soils (i.e., Ni-hyperaccumulating endemic, non-hyperaccumulating endemic, indicator, or indifferent) in a common garden greenhouse experiment. All species were grown in control soils, as well as those that were amended with the heavy metal Ni, and then analyzed for macronutrient (Ca, Mg, K, and P), micronutrient (Cu, Fe, Zn, Mn, and Mo), and heavy metal (Cr and Co) concentrations in their vegetative and reproductive organs (leaves, anthers, and pistils). In accordance with the IUH, we found that hyperaccumulators often accumulated higher concentrations of nutrients and metals compared to non-hyperaccumulating species, although these differences were often organ-specific. Specifically, while hyperaccumulators accumulated significantly more K and Co across all organs, Cu was higher in leaves only, while Mn and Zn were higher in anthers only. Furthermore, hyperaccumulators accumulated significantly more Co and Mo across all organs when Ni was added to the soil environment. Our work provides additional evidence in support of the IUH, and contributes to our understanding of serpentine adaptation in plants.


2016 ◽  
Vol 18 (1) ◽  
pp. 214-222 ◽  

<p>Ultramafics represent magmatic or metamorphic rocks which are characterized by high concentrations of Mg, Fe, Ni, Cr and Co and low concentrations of Ca, and K. Serpentine soils are weathered products of a range of ultramafic rocks composed of ferromagnesian silicates. The aim of this study was to determine the content of heavy metals in some of serpentine soils of Kosovo and heavy metals uptake by entire associated flora. Furthermore, another objective of this study was finding out bioavailable Ca/Mg relationship, which is very important indicator for plants&rsquo; development. The sampling was conducted in June 2014. A total of three serpentine areas have been surveyed and 7 soil samples have been taken in various depths of soil profiles. Those samples were analyzed for total Ca, Cd, Co, Cr, Cu, Mn, Ni, Pb, Fe and Zn. Results showed that each site exhibited a high concentration of at least one metal. The maximum concentrations of metals in soils Dry Matter (DM) were 108.9 mg kg<sup>-1</sup> Cd, 95.8 mg kg<sup>-1</sup> Co, 1206 mg kg<sup>-1</sup> Cr, 24 mg kg<sup>-1</sup> Cu, 2570 mg kg<sup>-1</sup> Ni, 21.7 mg kg<sup>-1</sup> Pb, 39 mg kg<sup>-1</sup> Zn, and 51563 mg kg<sup>- </sup>Fe. The serpentine soils at all sites were characterized by elevated levels of heavy metals, which showed typical properties of ultramafic environments. Nickel Total at studied areas varied between 1543 and 2570 mg kg<sup>-1</sup>, while the highest Ni concentration was found in aerial part of Alyssum markgrafii (4038 mgkg<sup>-1</sup>),</p> <div> <p>Based on our findings on the field we concluded that there is a close relationship between the quantity of Ni in soil and Ni uptake in plants.</p> </div> <p>&nbsp;</p>


2015 ◽  
Vol 63 (2) ◽  
pp. 78 ◽  
Author(s):  
Anzhelika Yu. Teptina ◽  
Alexander G. Paukov

Cool temperate regions have a limited number of species able to accumulate nickel (Ni) and other heavy metals in above-ground tissues. Our study was conducted in order to find accumulators of Ni on serpentine soils in the Middle and Southern Urals. Above-ground tissues of plants as well as soil samples were collected in 10 ultramafic massifs. Our results confirmed hyperaccumulation activity of Alyssum obovatum (C.A.Mey.) Turcz. Three species that appeared to be hemi-accumulators of Ni are Alyssum litvinovii Knjaz., Alyssum tortuosum Willd. and Noccaea thlaspidioides (Pall.) F.K.Mey. All these species are facultative accumulators/hyperaccumulators and exhibit different concentrations of Ni under a range of soil conditions. The highest Ni concentration was found in A. obovatum in Krakinskiy massif (6008 μg·g–1 dry mass), A. tortuosum (1789 μg·g–1) and A. litvinovii (160 μg·g–1) in Khabarninskiy massif, and N. thlaspidioides (741 μg·g–1) in Sugomakskiy massif (Southern Urals). Regression analysis shows statistically significant dependence of Ni concentrations in soil and tissue of both A. obovatum and A. tortuosum. The latter shows a dramatically high difference in the level of accumulation that varies from excluder to 20 μg g–1 Ni to hyperaccumulator levels, suggesting the existence of genetically distinct populations with the ability to vary their accumulation of Ni.


2021 ◽  
Vol 42 ◽  
pp. e67609
Author(s):  
Marina Mota-Merlo ◽  
Vanessa Martos

The so-called hyperaccumulator plants are capable of storing hundred or thousand times bigger quantities of heavy metals than normal plants, which makes hyperaccumulators very useful in fields such as phytoremediation and phytomining. Among these plants there are many serpentinophytes, i.e., plants that grow exclusively on ultramafic rocks which produce soils with a great proportion of heavy metals. Even though there are multiple classifications, the lack of consensus regarding which parameters to use to determine whether a plant is a hyperaccumulator, as well as the arbitrariness of stablished thresholds, bring about the need to propose more objective criteria. To this end, plant mineral composition data from different vegetal species were analysed using machine learning techniques. Three complementary case studies were established. Firstly, plants were classified in three types of soils: dolomite, gypsum and serpentine. Secondly, data about normal and hyperaccumulator plant Ni composition were analysed with machine learning to find differentiated subgroups. Lastly, association studies were carried out using data about mineral composition and soil type. Results in the classification task reach a success rate over 75%. Clustering of plants by Ni concentration in parts per million (ppm) resulted in four groups with cut-off points in 2.25, 100 (accumulators) and 3000 ppm (hyperaccumulators). Associations with a confidence level above 90% were found between high Ni levels and serpentine soils, as well as between high Ni and Zn levels and the same type of soil. Overall, this work demonstrates the potential of machine learning to analyse data about plant mineral composition. Finally, after consulting the red list of the IUCN and those of countries with high richness in hyperaccumulator species, it is evident that a greater effort should be made to establish the conservation status of this type of flora.


2020 ◽  
Vol 231 (4) ◽  
Author(s):  
Anesa Ahatović ◽  
Jasmina Čakar ◽  
Mirel Subašić ◽  
Mujo Hasanović ◽  
Senad Murtić ◽  
...  

Author(s):  
Nishanta Rajakaruna ◽  
Robert S. Boyd

Serpentine soils are weathered products of a range of ultramafic rocks composed of ferromagnesian silicates. Serpentine more accurately refers to a group of minerals, including antigorite, chrysotile, and lizardite, in hydrothermally altered ultramafic rocks. Common ultramafic rock types include peridotites (dunite, wehrlite, harzburgite, lherzolite) and the secondary alteration products formed by their hydration within the Earth’s crust, including serpentinite, the primary source of serpentine soil. Serpentine soils are generally deficient in plant essential nutrients such as nitrogen, phosphorus, potassium, and sulfur; have a calcium-to-magnesium (Ca:Mg) molar ratio of less than 1; and have elevated levels of heavy metals such as nickel, cobalt, and chromium. Although physical features of serpentine soils can vary considerably from site to site and within a site, serpentine soils are often found in open, steep landscapes with substrates that are generally shallow and rocky, often with a reduced capacity for moisture retention. Due to the intense selective pressure generated by such stressful edaphic conditions, serpentine soils promote speciation and the evolution of serpentine endemism, contributing to unique biotas worldwide, including floras with high rates of endemism and species with disjunct distributions. The biota of serpentine soils has contributed greatly to the development of ecological and evolutionary theory, as well as to the study of the genetics of adaptation and speciation. Plants growing on serpentine soils also provide genetic material for phytoremediation and phytomining operations. Habitats with serpentine soils are undergoing drastic changes due to ever-expanding development, deforestation, mining for heavy metals and asbestos, exotic-species invasions, climate change, and atmospheric deposition of previously limiting nutrients such as nitrogen. Such changes can have drastic impacts on serpentine floras and affect bacteria, fungi, and fauna associated with serpentine plants and soils. Habitats with serpentine soils provide ample opportunities for conservation- and restoration-oriented research directed at finding ways to better manage these biodiversity hotspots.


Author(s):  
Randall W. Smith ◽  
John Dash

The structure of the air-water interface forms a boundary layer that involves biological ,chemical geological and physical processes in its formation. Freshwater and sea surface microlayers form at the air-water interface and include a diverse assemblage of organic matter, detritus, microorganisms, plankton and heavy metals. The sampling of microlayers and the examination of components is presently a significant area of study because of the input of anthropogenic materials and their accumulation at the air-water interface. The neustonic organisms present in this environment may be sensitive to the toxic components of these inputs. Hardy reports that over 20 different methods have been developed for sampling of microlayers, primarily for bulk chemical analysis. We report here the examination of microlayer films for the documentation of structure and composition.Baier and Gucinski reported the use of Langmuir-Blogett films obtained on germanium prisms for infrared spectroscopic analysis (IR-ATR) of components. The sampling of microlayers has been done by collecting fi1ms on glass plates and teflon drums, We found that microlayers could be collected on 11 mm glass cover slips by pulling a Langmuir-Blogett film from a surface microlayer. Comparative collections were made on methylcel1ulose filter pads. The films could be air-dried or preserved in Lugol's Iodine Several slicks or surface films were sampled in September, 1987 in Chesapeake Bay, Maryland and in August, 1988 in Sequim Bay, Washington, For glass coverslips the films were air-dried, mounted on SEM pegs, ringed with colloidal silver, and sputter coated with Au-Pd, The Langmuir-Blogett film technique maintained the structure of the microlayer intact for examination, SEM observation and EDS analysis were then used to determine organisms and relative concentrations of heavy metals, using a Link AN 10000 EDS system with an ISI SS40 SEM unit. Typical heavy microlayer films are shown in Figure 3.


1993 ◽  
Vol 88 (3) ◽  
pp. 522-529 ◽  
Author(s):  
Udo W. Stephan ◽  
Gunter Scholz
Keyword(s):  

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