Low carbon futures: assessing the status of decarbonisation efforts at universities within a 2050 perspective.

Background: The implementation of sustainability at universities means that they can also play a key role in the transition to a low carbon economy, and in assisting global efforts towards decarbonisation. Yet, not all of them have so far fully engaged in this area. This paper reviews the state of the art on trends in decarbonisation, and outlines the need for decarbonisation efforts at universities. It also reports on a survey aimed at ascertaining the extent to which universities in a sample of 40 countries across the various geographical regions are engaged in carbon reduction efforts, identifying the challenges faced. Results: The study has shown that the literature on the topic has been evolving over time and that increasing a given university's energy supply from renewable energy sources has been the cornerstone of university-based climate action plans. The study also indicates that even though several universities are concerned with their carbon footprint and actively seeking ways to reduce it, there are some institutional obstacles that need to be overcome. Conclusions: A first conclusion which can be drawn is that efforts on decarbonisation are becoming more popular, with a special focus being placed on the use of renewable energy. Also, the study has shown that, from the range of efforts being made towards decarbonisation, many universities are setting up a team with carbon management responsibilities, have Carbon Management Policy Statements, and review them. The paper points towards some measures which may be deployed, so as to allow universities to take better advantage of the many opportunities an engagement in decarbonisation initiatives offers to them.

Rapid carbon accumulation at a saltmarsh restored by managed realignment exceeded carbon emitted in direct site construction.

Increasing attention is being paid to the carbon sequestration and storage services provided by coastal blue carbon ecosystems such as saltmarshes. Sites restored by managed realignment, where existing sea walls are breached to reinstate tidal inundation to the land behind, have considerable potential to accumulate carbon through deposition of sediment brought in by the tide and burial of vegetation in the site. While this potential has been recognised, it is not yet a common motivating factor for saltmarsh restoration, partly due to uncertainties about the rate of carbon accumulation and how this balances against the greenhouse gases emitted during site construction. We use a combination of field measurements over four years and remote sensing to quantify carbon accumulation at a large managed realignment site, Steart Marshes, UK. Sediment accumulated rapidly at Steart Marshes (mean of 75 mm yr-1) and had a high carbon content (4.4% total carbon, 2.2% total organic carbon), resulting in carbon accumulation of 36.6 t ha-1 yr-1 total carbon (19.4 t ha-1 yr-1 total organic carbon). This rate of carbon accumulation is an order of magnitude higher than reported in many other restored saltmarshes, and is somewhat higher than values previously reported from another hypertidal system (Bay of Fundy, Canada). The estimated carbon emissions associated with the construction of the site were ~2-4% of the observed carbon accumulation during the study period, supporting the view that managed realignment projects in such settings may have significant carbon accumulation benefits. However, uncertainties such as the origin of carbon (allochthonous or autochthonous) and changes in gas fluxes need to be resolved to move towards a full carbon budget for saltmarsh restoration.

SARS-CoV-2 driving rapid change in adult cystic fibrosis services: the role of the clinical nurse specialist.

Cystic fibrosis (CF) is a genetic, life-limiting disease without a cure; treatment is complex and lifelong. Respiratory failure is the most common cause of death; however, gastrointestinal disease, diabetes and liver disease are common comorbidities. Coronavirus disease (COVID-19) rapidly changed healthcare services across the globe, including redeployment of healthcare professionals. This adult CF service was challenged to continue a patient facing service within severe staffing and structural limitations.Not only were many members of the CF multidisciplinary team (MDT) redeployed at the start of the first wave, but also both the CF and ambulatory care wards were closed. Fortunately, the CF clinical nurse specialists (CF-CNSs) remained in their role. Rapid change and adaptation of the CF service was required to ensure that patients did not feel abandoned and access to treatment remained available. The role of the CF-CNS was therefore pivotal in this change.The aim of this project was to use quality improvement methodology to plan an emergency service allowing a reintroduction of ambulatory care services. Success was measured by the number of patients clinically reviewed with or without intervention, and the reasons for patients contacting the CF-CNS via email and phone were recorded.In weeks 1 and 2 of the emergency service, the CF-CNSs triaged patients by phone, then reviewed face-to-face when necessary. This first step allowed the CF-CNSs to start two patients on home intravenous antibiotics. This service continued to be developed over the following 12 weeks, leading to a total of 36 patient attendances. In March 2020, n=1187 patients made contact (mostly COVID-19, unwell and medication related), in April n=904 and May n=870 (blood test results, unwell and medication related).The motivation of the CF-CNSs was pivotal to the success of this initiative with the CF MDT available to provide some support and advice. It concluded at week 12, which then saw the opening of the formal ambulatory care ward and returning redeployed ward staff.

Seeing a deep ocean CO2 enrichment experiment in a new light: laser raman detection of dissolved CO2 in seawater.

We used a newly developed in situ laser Raman spectrometer (LRS) for detection of elevated levels of dissolved CO2 in seawater. The experiment was carried out at 500 m depth, 6 degrees C, to examine new protocols for detection of CO2-enriched seawater emanating from a liquid CO2 source in the ocean, and to determine current detection limits under field conditions. A system of two interconnected 5 L chambers was built, with flow between them controlled by a valve and pump system, and this unit was mounted on an ROV. The first chamber was fitted with a pH electrode and the optical probe of the LRS. In the second chamber approximately 580 mL of liquid CO2 was introduced. Dissolution of CO2 across the CO2-seawater interface then occurred, the valves were opened, and a fixed volume of low-pH/CO2-enriched seawater was transferred to the first chamber for combined pH/Raman sensing, where we estimate a mean dissolution rate of approximately 0.5 (micromol/cm2)/s. This sequence was repeated, resulting in measurement of a progressively CO2 enriched seawater sample. The rapid in-growth of CO2 was readily detected as the Fermi dyad of the dissolved state with a detection limit of approximately 10 mM with spectral acquisition times of 150 s. The detection of background levels of CO2 species in seawater (approximately 2.2 mM, dominantly HCO3-) will require an improvement in instrument sensitivity by a factor of 5-10, which could be obtained by the use of a liquid core waveguide.