我国钢渣碳汇的量化分析

在全球温室气体浓度升高的背景下,如何减少碳排放、增加碳吸收是当前应对气候变化研究的热点.本研究基于我国1963—2016年粗钢产量,采用温室气体清单指南编制方法,建立了钢渣碳汇核算方法,核算了我国1963—2016年钢渣碳汇量,并进行了不确定性分析.结果表明: 1963—2016年间,我国钢渣的年碳汇量总体呈上升趋势,从3.75×10³ t C增加至1359.32×10³ t C.1963—2016年间我国钢渣累积碳汇量为15×10⁶ t C,钢渣碳汇的总不确定性约为±30.4%.钢渣年碳汇量由当年产钢渣碳汇量和历年产钢渣碳汇量两部分组成.由于钢渣结构致密,年碳化速率较小,导致1963—2016年间当年产钢渣碳汇量较小,占钢渣碳汇总量的37%;历年产钢渣碳汇量较大,占钢渣碳汇总量的63%.虽然钢渣年碳汇量不大,但长期累积碳汇量非常可观,其碳汇作用不容忽视.今后研究应细化不同环境条件下钢渣碳化速率,降低钢渣碳汇核算的不确定性;推动以钢渣为原材料的碳捕集与封存技术发展,增加有效碳汇,为我国应对气候变化国际谈判提供科技支撑.     

Leaching of Mercury from Carbonated and Non-Carbonated Cement-Solidified Dredged Sediments

This study investigated traditional cement-based and non-conventional (using accelerated carbonation) solidification/stabilization to treat 2 dredged sediments contaminated with mercury from two different locations in UK. Canal and estuarine-derived sediments were mixed with blended binders and powdered activated carbon. Fresh mixtures of sediment and cement were exposed to gaseous carbon dioxide and were allowed to carbonate for fixed time periods, after which they were cured for 28 days. Following curing, samples were leach tested to evaluate the fixation of mercury in the treated products. The results obtained indicated that both conventional and accelerated carbonated treatments were capable of reducing the concentration of mercury in the eluates to acceptable limits.     

Lessons from two high CO2 worlds – future oceans and intensive aquaculture

Exponentially rising CO₂ (currently ~400 μatm) is driving climate change and causing acidification of both marine and freshwater environments. Physiologists have long known that CO₂ directly affects acid–base and ion regulation, respiratory function and aerobic performance in aquatic animals. More recently, many studies have demonstrated that elevated CO₂ projected for end of this century (e.g. 800–1000 μatm) can also impact physiology, and have substantial effects on behaviours linked to sensory stimuli (smell, hearing and vision) both having negative implications for fitness and survival. In contrast, the aquaculture industry was farming aquatic animals at CO₂ levels that far exceed end‐of‐century climate change projections (sometimes >10 000 μatm) long before the term ‘ocean acidification’ was coined, with limited detrimental effects reported. It is therefore vital to understand the reasons behind this apparent discrepancy. Potential explanations include 1) the use of ‘control’ CO₂ levels in aquaculture studies that go beyond 2100 projections in an ocean acidification context; 2) the relatively benign environment in aquaculture (abundant food, disease protection, absence of predators) compared to the wild; 3) aquaculture species having been chosen due to their natural tolerance to the intensive conditions, including CO₂ levels; or 4) the breeding of species within intensive aquaculture having further selected traits that confer tolerance to elevated CO₂. We highlight this issue and outline the insights that climate change and aquaculture science can offer for both marine and freshwater settings. Integrating these two fields will stimulate discussion on the direction of future cross‐disciplinary research. In doing so, this article aimed to optimize future research efforts and elucidate effective mitigation strategies for managing the negative impacts of elevated CO₂ on future aquatic ecosystems and the sustainability of fish and shellfish aquaculture.     

Mineral Carbonation as the Core of an Industrial Symbiosis for Energy‐Intensive Minerals Conversion

The longer term sustainability of the minerals sector may hinge, in large part, on finding innovative solutions to the challenges of energy intensity and carbon dioxide (CO₂) management. This article outlines the need for large‐scale “carbon solutions” that might be shared by several colocated energy‐intensive and carbon‐intensive industries. In particular, it explores the potential for situating a mineral carbonation plant as a carbon sink at the heart of a minerals and energy complex to form an industrial symbiosis. Several resource‐intensive industries can be integrated synergistically in this way, to enable a complex that produces energy and mineral products with low net CO₂ emissions. An illustrative hypothetical case study of such a system within New South Wales, Australia, has been constructed, on the basis of material and energy flows derived from Aspen modeling of a serpentine carbonation process. The synergies and added value created have the potential to significantly offset the energy and emission penalties and direct costs of CO₂ capture and storage. This suggests that greenfield minerals beneficiation and metals refining plants should consider closer integration with the power production and energy provision plants on which they depend, together with a carbon solution, such as mineral carbonation, as a critical element of such integration. Other sustainability considerations are highlighted.     

Red Algae (Eucheuma muricatum) Mucilage- Complex Formation and Mechanism

Eucheuma muricatum mucilage which was extracted and purified after irradiation of the seaweed with γ-ray of ⁶⁰Co formed a complex with , and exhibited a new absorption band at 555 nm. The absorbancy observed at that time depended on the concentration of urea and on the temperature. The curves representing relations between absorbancy at 555 nm and the above factors have two inflection points. The fact that their inflection points shift toward the lower temperature side with the increase in urea concentration suggests that the coloring phenomenon may relate closely to the transition of the mucilage. It was also found that the absorbancy at 555 nm depended on the content of pyruvic acid residue in the same mucilages, the absorbancy decreased with the increase pyruvic acid residues, and that the steric hindrance caused by a sugar residue of large demension affected the stable from containing viscous polysaccharide.     

Trends,application and future prospectives of microbial carbonic anhydrase mediated carbonation process for CCUS

Summary

Growing industrialization and the desire for a better economy in countries has accelerated the emission of greenhouse gases (GHGs), by more than the buffering capacity of the earth's atmosphere. Among the various GHGs, carbon dioxide occupies the first position in the anthroposphere and has detrimental effects on the ecosystem. For decarbonization, several non‐biological methods of carbon capture, utilization and storage (CCUS) have been in use for the past few decades, but they are suffering from narrow applicability. Recently, CO₂ emission and its disposal related problems have encouraged the implementation of bioprocessing to achieve a zero waste economy for a sustainable environment. Microbial carbonic anhydrase (CA) catalyses reversible CO₂ hydration and forms metal carbonates that mimic the natural phenomenon of weathering/carbonation and is gaining merit for CCUS. Thus, the diversity and specificity of CAs from different micro‐organisms could be explored for CCUS. In the literature, more than 50 different microbial CAs have been explored for mineral carbonation. Further, microbial CAs can be engineered for the mineral carbonation process to develop new technology. CA driven carbonation is encouraging due to its large storage capacity and favourable chemistry, allowing site‐specific sequestration and reusable product formation for other industries. Moreover, carbonation based CCUS holds five‐fold more sequestration capacity over the next 100 years. Thus, it is an eco‐friendly, feasible, viable option and believed to be the impending technology for CCUS. Here, we attempt to examine the distribution of various types of microbial CAs with their potential applications and future direction for carbon capture. Although there are few key challenges in bio‐based technology, they need to be addressed in order to commercialize the technology.     

Bioleaching of Lizardite by Magnesium- and Nickel-Resistant Fungal Isolate from Serpentinite Soils—Implication for Carbon Capture and Storage

The major goal of this study was to evaluate the potential of fungal species indigenous to mine tailing soils in accelerating Mg release from lizardite (a polymorph of serpentine) at ambient T/P conditions. We characterized the culturable fungal isolates at three sampling sites representative of different degrees of mineral weathering by isolating the genomic subunits and internal transcribed spacer (ITS) rRNA genes using PCR and sequencing of cloned fragments. We chose the specific strain primarily identified as Talaromyces sp. for the further experiments with lizardite because of this strain's remarkable tolerance to high [Mg²⁺] (1 mol·L^?1) and [Ni²⁺] (10 mM·L^?1) levels in the screening test and its ubiquity in the most severely weathered samples. Results of dissolution experiments revealed that both magnesium-release rate and efficiency were significantly increased (e.g., by a factor of up to 15) in the presence of fungal cells than those in the abiotic controls. The enhanced dissolution of lizardite was mainly attributed to the fungal production of organic acids including oxalic acid, gluconic acid, formic acid, and fumaric acid added to the solution. The proton-promoted dissolution, however, was indicated not to be the only mechanism for fungus-lizardite interactions as much lesser Mg (in wt.%) was recovered in the abiotic system where the solution pH was constantly adjusted to match that of the fungal system. We also explored the dependence of fungal dissolution (of lizardite) on temperature and mineral particle sizes. In particular, we found that up to ～ 50 wt.% of Mg was released from mineral particles of ～ 50 μm within 30 days at 38°C, ～ 26% and 8% higher than that at 18°C and 28°C, respectively. At the same temperature of 28°C, the Mg-release efficiency increased from 12.2 wt% for particles of ～ 270 μm to 38.4 wt% for those of ～100 μm although no apparent difference was recognized when the particle size decreased below 100 μm. The nonlinear correlation of dissolution rates with particle surface areas suggested that the dissolution process was controlled by mineral surface-structural modification along with Mg release and by fungal cells’ interaction with these surface structures. An amorphous layer of Mg-depleted silica was detected at the reacted mineral surface by scanning electron microscopy (SEM) and Fourier transform infrared spectroscopy (FTIR). Formation of glushinskite (MgC₂O₄·2H₂O) was also observed when oxalate was accumulated to certain concentrations in the solution. Overall, this study showed that the isolated Talaromyces sp. was a promising bioagent to improve the efficacy of cation release from serpentine minerals for the purpose of carbon sequestration and resource recovery.     

Membrane technology in microalgae cultivation and harvesting: A review

Membrane processes have long been applied in different stages of microalgae cultivation and processing. These processes include microfiltration, ultrafiltration, dialysis, forward osmosis, membrane contactors and membrane spargers. They are implemented in many combinations, both as a standalone and as a coupled system (in membrane biomass retention photobioreactors (BR-MPBRs) or membrane carbonation photobioreactors (C-MPBRs). To provide sufficient background on these applications, an overview of membrane materials and membrane processes of interest in microalgae cultivation and processing is provided in this work first. Afterwards, discussion about specific aspects of membrane applications in microbial cultivation and harvesting is provided, including membrane fouling. Many of the membrane processes were shown to be promising options in microalgae cultivation. Yet, significant process optimizations are still required when they are applied to enable microalgae biomass bulk production to become competitive as a raw material for biofuel production. Recent developments of the coupled systems (BR-MPBR and C-MPBR) bring significant promises to improve the volumetric productivity of a cultivation system and the efficiency of inorganic carbon capture, respectively.     

Production of Honbushi-like Flavor by the Fermentation of Nijiru

It takes about 2 months for the molding process of Katsuobushi (dried bonito) production. A model of a short-term system for the molding process was desirable for the efficient selection of useful fungi for Katsuobushi production by evaluating the flavor change in the model system.

A liquid culture system using Nijiru (waste fluid of Katsuobushi sterilization), which is obtained from the Kezuribushi (sliced Katsuobushi) manufacturing process and contains abundant phenolic compounds of smoke tar, was found to be suitable for the short-term evaluation of a 10 day culture.