Cryogenic carbon capture

Cryogenic Carbon Capture™ (CCC) removes CO2 from flue gas in a bolt on retrofittable, cost-effective, and energy-efficient process. The process also provides grid-level energy storage capable of storing and releasing energy at hundreds of megawatt rates at high efficiency and minimal cost beyond the costs of the carbon capture technology. The energy storage can level daily load fluctuations and responds to intermittent power sources on time scales comparable to solar and wind farms. The technology cools flue gases to their condensation (desublimation) point forming solid CO2, separates the solids from the residual gases, pressurizes the solids, and reheats both streams to room temperature. The process produces two nominally ambient-temperature streams: liquid CO2 at about 150 bar and the light gases at ambient pressure. Essentially all of the sensible heating occurs through energy integration. The technology primary advantages include (a) consumes minimal energy for CO2 capture (appx. 0.7 GJe/tonne CO2 for typical coal flue gas) (b) costs relatively little (2.5 cents/kWh or less increase in COE) (c) retrofits existing plants with virtually no upstream modification (d) removes essentially all other pollutants except CO, including SOx, NOx, Hg, PMxx, and HC; (e) requires no additional cooling water; (f) requires no steam or other resources from the process other than electrical power Fully integrated versions of the technology at up to 1 tonne of CO2/day have operated on fuels including subbituminous coal, bituminous coal, natural gas, biomass, municipal waste and tires and at sites that include utility power plants, cement kilns, heat plants, and pilot-scale research combustors. This presentation summarizes the technology, field test results, and development plans for this technology. Further information is available at www.sesinnovation.com

Restoration of the Nisqually River Delta and increased rearing opportunities for salmonids

Estuarine wetlands in the Salish Sea provide important rearing habitat for migrating juvenile Pacific salmon, contributing to their overall productivity and ocean survival. Substantial loss of historical estuarine habitat in the Salish Sea due to diking, draining and development has contributed to the decline of Pacific salmon populations (Oncorhynchus spp.). The return of tidal inundation through a series of dike removals to 364 hectares of the Nisqually River Delta (Olympia, Washington, USA) represents one of the most significant advances to date towards the recovery of the threatened Nisqually Fall Chinook stock. Our objective was to assess the collective Nisqually Delta restorations in terms of increased rearing opportunity for juvenile salmon. Metrics consisted of physical conditions that allow juvenile salmon to access the estuarine restorations such as delta connectivity, full tidal inundation and channel development. Unlike most studies, we put these physical metrics in terms of juvenile Chinook by constraining our inundation model to outmigration season (Mar – Aug) and those tidal depths supporting juvenile Chinook (\u3e 0.4 m). We used these criteria, verified by presence of juvenile salmonids in three restored and two reference tidal channels, to measure the change in opportunity potential from pre-restoration to post-restoration condition for juvenile Chinook to access and rear in the Nisqually estuary. We found landscape connectivity to be strongly tied to tidal height and increased throughout the estuary with dike removal. Tidal channel development was most rapid in the first and second year post-restoration; with channel outlets widening and deepening to accommodate restored tidal prisms. Chum salmon, natural origin Chinook and hatchery origin Chinook salmon accessed all three restored marshes within two years post-restoration, although responses varied among years, marshes and salmon species. These results suggest that the Nisqually Delta restorations are providing increased rearing opportunity for juvenile salmon

Identification of Bone Marrow Cell Subpopulations Associated With Improved Functional Outcomes in Patients With Chronic Left Ventricular Dysfunction: An Embedded Cohort Evaluation of the FOCUS-CCTRN Trial

In the current study, we sought to identify bone marrow-derived mononuclear cell (BM-MNC) subpopulations associated with a combined improvement in left ventricular ejection fraction (LVEF), left ventricular end-systolic volume (LVESV), and maximal oxygen consumption (VO2 max) in patients with chronic ischemic cardiomyopathy 6 months after receiving transendocardial injections of autologous BM-MNCs or placebo. For this prospectively planned analysis, we conducted an embedded cohort study comprising 78 patients from the FOCUS-Cardiovascular Cell Therapy Research Network (CCTRN) trial. Baseline BM-MNC immunophenotypes and progenitor cell activity were determined by flow cytometry and colony-forming assays, respectively. Previously stable patients who demonstrated improvement in LVEF, LVESV, and VO2 max during the 6-month course of the FOCUS-CCTRN study (group 1, n = 17) were compared to those who showed no change or worsened in one to three of these endpoints (group 2, n = 61) and to a subset of patients from group 2 who declined in all three functional endpoints (group 2A, n = 11). Group 1 had higher frequencies of B-cell and CXCR4(+) BM-MNC subpopulations at study baseline than group 2 or 2A. Furthermore, patients in group 1 had fewer endothelial colony-forming cells and monocytes/macrophages in their bone marrow than those in group 2A. To our knowledge, this is the first study to show that in patients with ischemic cardiomyopathy, certain bone marrow-derived cell subsets are associated with improvement in LVEF, LVESV, and VO2 max at 6 months. These results suggest that the presence of both progenitor and immune cell populations in the bone marrow may influence the natural history of chronic ischemic cardiomyopathy-even in stable patients. Thus, it may be important to consider the bone marrow composition and associated regenerative capacity of patients when assigning them to treatment groups and evaluating the results of cell therapy trials

The \u3cem\u3eChlamydomonas\u3c/em\u3e Genome Reveals the Evolution of Key Animal and Plant Functions

Chlamydomonas reinhardtii is a unicellular green alga whose lineage diverged from land plants over 1 billion years ago. It is a model system for studying chloroplast-based photosynthesis, as well as the structure, assembly, and function of eukaryotic flagella (cilia), which were inherited from the common ancestor of plants and animals, but lost in land plants. We sequenced the ∼120-megabase nuclear genome of Chlamydomonas and performed comparative phylogenomic analyses, identifying genes encoding uncharacterized proteins that are likely associated with the function and biogenesis of chloroplasts or eukaryotic flagella. Analyses of the Chlamydomonas genome advance our understanding of the ancestral eukaryotic cell, reveal previously unknown genes associated with photosynthetic and flagellar functions, and establish links between ciliopathy and the composition and function of flagella

Progressing from multidisciplinary to interdisciplinary restoration science: monitoring and applied studies on the Nisqually River Delta

Restoration science is often described as an ultimate test of ecological theory; assessing the value of restoration actions is challenged by difficulties in measuring complex interactions between restored physical processes and the response of biological resources. Yet, demonstrating the value of restoration is a key to sustaining future public investment, especially in light of uncertainty of future climate change effects. At the Nisqually River Delta, a restoration partnership between the U. S. Fish and Wildlife Service Nisqually National Wildlife Refuge (Refuge), the Nisqually Indian Tribe (Tribe), and Ducks Unlimited culminated in re-established tidal flow to 360 ha of historic floodplain and delta representing the largest estuarine restoration in the Pacific Northwest. Restoration of this large delta was expected to result in a substantial improvement in ecological functions and services in southern Puget Sound. The goal of our scientific team, led by the U. S. Geological Survey (USGS) for the project partners, was to assess the biophysical response to restoration. Science objectives were built into a monitoring framework to include hydrodynamics, geomorphology, sedimentation and nearshore processes with vegetation, invertebrate food resources, waterbird, and fisheries. Our science partners included the U. S. Geological Survey, Refuge, Tribe, non-governmental organizations, and universities representing several disciplines. Funding the science was challenging, since as with most wetland restoration projects, adequate funds are rarely included in costs. Instead, the managers and scientists worked together to raise funds through special funds and competitive grants including addressing climate change. With this funding model, a major challenge for the team was communicating and sustaining a vision to make separate multidisciplinary efforts into unified interdisciplinary science. Here, we use lessons learned from early results of the Nisqually River Delta restoration to discuss restoration science in planning processes, funding costs and approaches, monitoring versus applied studies, and advancing interdisciplinary findings from multidisciplinary efforts

The Redshift Evolution of the Mean Temperature, Pressure, and Entropy Profiles in 80 SPT-Selected Galaxy Clusters

We present the results of an X-ray analysis of 80 galaxy clusters selected in the 2500 deg2 South Pole Telescope survey and observed with the Chandra X-ray Observatory. We divide the full sample into subsamples of ∼20 clusters based on redshift and central density, performing a joint X-ray spectral fit to all clusters in a subsample simultaneously, assuming self-similarity of the temperature profile. This approach allows us to constrain the shape of the temperature profile over 0 R500) regions than their low-z (0.3 < z < 0.6) counterparts. Combining the average temperature profile with measured gas density profiles from our earlier work, we infer the average pressure and entropy profiles for each subsample. Confirming earlier results from this data set, we find an absence of strong cool cores at high z, manifested in this analysis as a significantly lower observed pressure in the central 0.1R500 of the high-z cool-core subset of clusters compared to the low-z cool-core subset. Overall, our observed pressure profiles agree well with earlier lower-redshift measurements, suggesting minimal redshift evolution in the pressure profile outside of the core. We find no measurable redshift evolution in the entropy profile at r . 0.7R500 – this may reflect a long-standing balance between cooling and feedback over long timescales and large physical scales. We observe a slight flattening of the entropy profile at r & R500 in our high-z subsample. This flattening is consistent with a temperature bias due to the enhanced (∼3×) rate at which group-mass (∼2 keV) halos, which would go undetected at our survey depth, are accreting onto the cluster at z ∼ 1. This work demonstrates a powerful method for inferring spatially-resolved cluster properties in the case where individual cluster signal-to-noise is low, but the number of observed clusters is high.Physic

Coming Together to Toast and Feed the Dead in the Cotahuasi Valley of Peru

There has been little discussion on the macrobotanical remains from Andean Middle Horizon sites. In this article, we present macrobotanical data from archaeological excavations at Tenahaha, a small mortuary center in the Cotahuasi Valley of Peru. While the people who attended Tenahaha may not have definitively been Wari, evidence suggests that they were likely influenced by the Wari. Our analysis revealed new insights into site use and the distribution of botanical staples during the Andean past. People used plants differently across time and how people chose to utilize plant resources from their environment provides insights into cultural practices. The local plant staples of quinoa (Chenopodium quinoa) and maize (Zea mays) were found in high densities in concentrated areas of the site. In addition, local plants such as Echinocactus (Echinocactus sp.), tubers (e.g., Solanum sp.), and the Peruvian peppertree (Schinus molle) were recovered in abundance. These remains provide insights into past public ceremonies and how the inhabitants used different areas of the site. The occurrence of sprouted maize and the fruit of peppertree in certain areas of the site seems to indicate ritual and/or ceremonial use of chicha during the Middle Horizon (AD 600–1050). The analysis of these macrobotanical remains provides a glimpse into the importance placed on bringing people together to commemorate the dead by Ancient Andean Peoples.</p

Evaluation of three field-based methods for quantifying soil carbon

Citation: Izaurralde, Roberto C., Charles W. Rice, Lucian Wielopolski, Michael H. Ebinger, James B. Reeves Iii, Allison M. Thomson, Ronny Harris, et al. “Evaluation of Three Field-Based Methods for Quantifying Soil Carbon.” PLOS ONE 8, no. 1 (January 31, 2013): e55560. https://doi.org/10.1371/journal.pone.0055560.Three advanced technologies to measure soil carbon (C) density (g C mˉ²) are deployed in the field and the results compared against those obtained by the dry combustion (DC) method. The advanced methods are: a) Laser Induced Breakdown Spectroscopy (LIBS), b) Diffuse Reflectance Fourier Transform Infrared Spectroscopy (DRIFTS), and c) Inelastic Neutron Scattering (INS). The measurements and soil samples were acquired at Beltsville, MD, USA and at Centro International para el Mejoramiento del Maı´z y el Trigo (CIMMYT) at El Bata´n, Mexico. At Beltsville, soil samples were extracted at three depth intervals (0–5, 5–15, and 15–30 cm) and processed for analysis in the field with the LIBS and DRIFTS instruments. The INS instrument determined soil C density to a depth of 30 cm via scanning and stationary measurements. Subsequently, soil core samples were analyzed in the laboratory for soil bulk density (kg mˉ³), C concentration (g kgˉ¹) by DC, and results reported as soil C density (kg mˉ²). Results from each technique were derived independently and contributed to a blind test against results from the reference (DC) method. A similar procedure was employed at CIMMYT in Mexico employing but only with the LIBS and DRIFTS instruments. Following conversion to common units, we found that the LIBS, DRIFTS, and INS results can be compared directly with those obtained by the DC method. The first two methods and the standard DC require soil sampling and need soil bulk density information to convert soil C concentrations to soil C densities while the INS method does not require soil sampling. We conclude that, in comparison with the DC method, the three instruments (a) showed acceptable performances although further work is needed to improve calibration techniques and (b) demonstrated their portability and their capacity to perform under field conditions