Nanoplastics interaction with feldspar and weathering originated secondary minerals (kaolinite and gibbsite) in the riverine environment

Author(s):  
Aniket Choudhary ◽  
Nitin Khandelwal ◽  
Nisha Singh ◽  
Ekta Tiwari ◽  
Zahid Ahmad Ganie ◽  
...  
2021 ◽  
Author(s):  
Ling Tan ◽  
Thomas Jones ◽  
Jianping Xie ◽  
Xinxing Liu ◽  
Gordon Southam

Abstract Weathering of the Merensky reef was enhanced under laboratory conditions by Fe- and S-oxidizing bacteria: Acidithiobacillus ferrooxidans, Acidithiobacillus thiooxidans, and Leptospirillum ferrooxidans. These bacteria preferentially colonized pyrrhotite and pyrite, versus pentlandite and chalcopyrite (all of which were common within the rock substrate), promoting weathering. Weathering of base metal sulfides resulted in the precipitation of Fe oxides, Fe phosphate, and elemental sulfur as secondary minerals. Fe pyroxene weathered readily under acidic conditions and resulted in mineral dissolution, while other silicates (orthopyroxene and plagio-clase) precipitated Fe phosphate spherules or coatings on their surface. The deterioration of the platinum group metal (PGM) matrix (base metal sulfides and silicates) and the occurrence of a platinum grain associated with platinum nanoparticles observed in the biotic thin sections demonstrate that biogeochemical acid weathering is an important step in the active release of intact PGM grains. A platinum grain embedded in secondary Fe oxides/phosphate that had settled by gravity within the weathering solution demonstrates that secondary minerals that formed during weathering of PGM-hosting minerals also represent targets in PGM exploration by trapping and potentially slowing PGM migration. Dispersion halos surrounding or occurring downstream from PGM occurrences will likely produce two physical target classes—i.e., grains and colloids—under surficial weathering conditions.


2021 ◽  
Vol 17 (1) ◽  
pp. 126-133
Author(s):  
Bogdan VOINESCU ◽  
Ionel POPESCU

Abstract: This approach proposes an analysis and a presentation of divers’ actions in the riverine area in order to combat the risks and the threats which can occur there, correlated with the features and the characteristics of the environment and with the objectives of the Navy. The identification of new insights and opportunities of involving the divers in this domain through concrete, focused actions having a maximum effect in the preservation of a security climate in the riverine area is the novelty of this approach. While analyzing the actual possibilities of divers’ actions in the riverine area, this article is pleading regarding the importance of using divers in this environment and it is structured on two directions. The actions of the military divers in the riverine area contain these directions that meet the national objectives regarding maintenance or getting the control over the main economic and military objectives concomitant with the research, capture or destruction of enemy`s forces. I am addressing this approach to the specialists and to those who are interested in divers’ way of actions in the riverine environment. Divers are an especially important tool among the whole range of military actions in the riverine area. The actions taken by divers usually offer depth to the campaign and they have a significant role in preserving the riverine area.


1967 ◽  
Author(s):  
David M. Lassaline ◽  
David A. Sloss Jr. ◽  
Warren J. Baker ◽  
Constanzio X. C. Miranda
Keyword(s):  

Author(s):  
Robert F. Keefer

Micronutrients needed by plants are Cu, Fe, Mn, Zn, B, Mo, Cl, Ni, Co, V, Si, and Na. The required amounts of each of these elements is very small but still essential for desirable plant growth and reproduction. These elements must be applied to soils cautiously for the range between deficient and toxic is very small. It is unwise to use a fertilizer containing all of these micronutrients. Any one of them may already be high enough in soils to cause toxicity from that particular element. If a micronutrient is suspected of being deficient, it would be wise to get soil tests and plant tissue tests to corroborate your suspicions. If a micronutrient is deficient, one should apply only the amount recommended but no more. Sometimes a toxicity of an element is more difficult to correct than a deficiency. Copper, iron, manganese, cobalt, and zinc can be present in soils as (a) several types of precipitates, (b) adsorbed onto the surface of soil particles, (c) present in primary minerals (rocks) and secondary minerals (clays), and (d) present as complex ring compounds. These forms may or may not be available to plants. Precipitates of Cu, Fe, Mn, or Zn often form in soils at high pH (after liming Fig. 14.1). This may occur in soils near buildings from the lime used in the mortar. Soil acids dissolve the lime into Ca++ or Mg++ that migrate into the soil raising the pH and cause these micronutrients to precipitate. Often an Fe deficiency is evident, particularly on acid-loving plants, such as azaleas, rhododendrons, or hollies. If this is extensive, the soil near the buildings may need to be replaced. With limited areas, the soil can be acidified by adding elemental S near the plants affected. The elements Cu, Fe, Mn, and Zn can exist as soluble forms or precipitates, depending on the pH of the soil. The soluble forms as cations are present when soils have poor internal drainage (poorly drained soils), whereas the oxides of these elements are present where the soil is well aerated.


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