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Habib S, Talhami M, Hassanein A, Mahdi E, Al-Ejji M, Hassan MK, Altaee A, Das P, Hawari AH. Advances in functionalization and conjugation mechanisms of dendrimers with iron oxide magnetic nanoparticles. NANOSCALE 2024. [PMID: 38967017 DOI: 10.1039/d4nr01376j] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 07/06/2024]
Abstract
Iron oxide magnetic nanoparticles (MNPs) are crucial in various areas due to their unique magnetic properties. However, their practical use is often limited by instability and aggregation in aqueous solutions. This review explores the advanced technique of dendrimer functionalization to enhance MNP stability and expand their application potential. Dendrimers, with their symmetric and highly branched structure, effectively stabilize MNPs and provide tailored functional sites for specific applications. We summarize key synthetic modifications, focusing on the impacts of dendrimer size, surface chemistry, and the balance of chemical (e.g., coordination, anchoring) and physical (e.g., electrostatic, hydrophobic) interactions on nanocomposite properties. Current challenges such as dendrimer toxicity, control over dendrimer distribution on MNPs, and the need for biocompatibility are discussed, alongside potential solutions involving advanced characterization techniques. This review highlights significant opportunities in environmental, biomedical, and water treatment applications, stressing the necessity for ongoing research to fully leverage dendrimer-functionalized MNPs. Insights offered here aim to guide further development and application of these promising nanocomposites.
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Affiliation(s)
- Salma Habib
- Department of Mechanical and Industrial Engineering, Qatar University, 2713 Doha, Qatar
- Department of Civil and Environmental Engineering, College of Engineering, Qatar University, PO Box 2713, Doha, Qatar.
| | - Mohammed Talhami
- Department of Civil and Environmental Engineering, College of Engineering, Qatar University, PO Box 2713, Doha, Qatar.
| | - Amani Hassanein
- Department of Civil and Environmental Engineering, College of Engineering, Qatar University, PO Box 2713, Doha, Qatar.
| | - Elsadig Mahdi
- Department of Mechanical and Industrial Engineering, Qatar University, 2713 Doha, Qatar
| | - Maryam Al-Ejji
- Center for Advanced Materials, Qatar University, PO Box 2713, Doha, Qatar
| | - Mohammad K Hassan
- Center for Advanced Materials, Qatar University, PO Box 2713, Doha, Qatar
| | - Ali Altaee
- School of Civil and Environmental Engineering, University of Technology Sydney, 15 Broadway, Ultimo, NSW 2007, Australia
| | - Probir Das
- Algal Technologies Program, Center for Sustainable Development, College of Arts and Sciences, Qatar University, 2713, Doha, Qatar
| | - Alaa H Hawari
- Department of Civil and Environmental Engineering, College of Engineering, Qatar University, PO Box 2713, Doha, Qatar.
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Kim M, Lopez-Canfin C, Lázaro R, Sánchez-Cañete EP, Weber B. Unravelling the main mechanism responsible for nocturnal CO 2 uptake by dryland soils. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 926:171751. [PMID: 38503391 DOI: 10.1016/j.scitotenv.2024.171751] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/17/2023] [Revised: 02/21/2024] [Accepted: 03/14/2024] [Indexed: 03/21/2024]
Abstract
Soil respiration, or CO2 efflux from soil, is a crucial component of the terrestrial carbon cycle in climate models. Contrastingly, many dryland soils absorb atmospheric CO2 at night, but the exact mechanisms driving this uptake are actively debated. Here we used a mechanistic model with heuristic approaches to unravel the underlying processes of the observed patterns of soil-atmosphere CO2 fluxes. We show that the temperature drop during nighttime is the main driver of CO2 uptake by increasing CO2 solubility and local water pH of a thin water film on soil particle surfaces, providing favourable conditions for carbonate precipitation. Our data demonstrate that the nocturnal inorganic carbon absorption is a common soil process, but often offset by biological CO2 production. The uptake rates can be impacted by different successional stages of biocrusts that consume or produce CO2 and modify the pH of the soil water film, which can be maintained by non-rainfall water inputs, such as pore space condensation. Annual estimates of nocturnal carbon uptake, based on in situ continuous measurements at the soil level in drylands are still very scarce, but fluxes of up to several tens of g C m-2 y-1 have been reported, potentially accounting for a considerable fraction of the global residual terrestrial carbon sink.
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Affiliation(s)
- Minsu Kim
- Institute of Biology, University of Graz, Graz, Austria.
| | - Clément Lopez-Canfin
- Department of Applied Physics, University of Granada (UGR), Granada, Spain; Department of Plant and Soil Sciences, University of Delaware, Newark, DE, USA
| | - Roberto Lázaro
- Department of Desertification and Geo-Ecology, Experimental Station of Arid Zones (EEZA-CSIC), Almería, Spain
| | - Enrique P Sánchez-Cañete
- Department of Applied Physics, University of Granada (UGR), Granada, Spain; Inter-University Institute for Earth System Research (IISTA-CEAMA), Granada, Spain
| | - Bettina Weber
- Institute of Biology, University of Graz, Graz, Austria; Multiphase Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
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Andrews HM, Krichels AH, Homyak PM, Piper S, Aronson EL, Botthoff J, Greene AC, Jenerette GD. Wetting-induced soil CO 2 emission pulses are driven by interactions among soil temperature, carbon, and nitrogen limitation in the Colorado Desert. GLOBAL CHANGE BIOLOGY 2023; 29:3205-3220. [PMID: 36907979 DOI: 10.1111/gcb.16669] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/26/2022] [Accepted: 01/20/2023] [Indexed: 05/03/2023]
Abstract
Warming-induced changes in precipitation regimes, coupled with anthropogenically enhanced nitrogen (N) deposition, are likely to increase the prevalence, duration, and magnitude of soil respiration pulses following wetting via interactions among temperature and carbon (C) and N availability. Quantifying the importance of these interactive controls on soil respiration is a key challenge as pulses can be large terrestrial sources of atmospheric carbon dioxide (CO2 ) over comparatively short timescales. Using an automated sensor system, we measured soil CO2 flux dynamics in the Colorado Desert-a system characterized by pronounced transitions from dry-to-wet soil conditions-through a multi-year series of experimental wetting campaigns. Experimental manipulations included combinations of C and N additions across a range of ambient temperatures and across five sites varying in atmospheric N deposition. We found soil CO2 pulses following wetting were highly predictable from peak instantaneous CO2 flux measurements. CO2 pulses consistently increased with temperature, and temperature at time of wetting positively correlated to CO2 pulse magnitude. Experimentally adding N along the N deposition gradient generated contrasting pulse responses: adding N increased CO2 pulses in low N deposition sites, whereas adding N decreased CO2 pulses in high N deposition sites. At a low N deposition site, simultaneous additions of C and N during wetting led to the highest observed soil CO2 fluxes reported globally at 299.5 μmol CO2 m-2 s-1 . Our results suggest that soils have the capacity to emit high amounts of CO2 within small timeframes following infrequent wetting, and pulse sizes reflect a non-linear combination of soil resource and temperature interactions. Importantly, the largest soil CO2 emissions occurred when multiple resources were amended simultaneously in historically resource-limited desert soils, pointing to regions experiencing simultaneous effects of desertification and urbanization as key locations in future global C balance.
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Affiliation(s)
- Holly M Andrews
- Department of Evolution, Ecology, and Organismal Biology, University of California, Riverside, California, USA
| | - Alexander H Krichels
- Department of Environmental Sciences, University of California, Riverside, California, USA
- Center for Conservation Biology, University of California, Riverside, California, USA
| | - Peter M Homyak
- Department of Environmental Sciences, University of California, Riverside, California, USA
| | - Stephanie Piper
- Department of Botany and Plant Sciences, University of California, Riverside, California, USA
| | - Emma L Aronson
- Department of Microbiology and Plant Pathology, University of California, Riverside, California, USA
| | - Jon Botthoff
- Center for Conservation Biology, University of California, Riverside, California, USA
| | - Aral C Greene
- Department of Environmental Sciences, University of California, Riverside, California, USA
| | - G Darrel Jenerette
- Center for Conservation Biology, University of California, Riverside, California, USA
- Department of Botany and Plant Sciences, University of California, Riverside, California, USA
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