Food Waste

My project talks about the high amounts of food waste in America and around the word. It talks about problems that food waste causes, causes of food waste, and recommendations on how to slow down food waste

Erythrocyte transketolase activity coefficient (ETKAC) assay protocol for the assessment of thiamine status

Abstract: Vitamin B1 (thiamine) is an essential nutrient that acts as a cofactor for a number of metabolic processes, particularly in energy metabolism. Symptoms of classic thiamine deficiency are recognized as beriberi, although clinical symptoms are nonspecific and recognition of subclinical deficiency is difficult. Therefore, reliable biomarkers of thiamine status are required. Thiamine diphosphate is a cofactor for transketolase, including erythrocyte transketolase (ETK). The ETK activity assay as an indirect, functional marker of thiamine status has been used for over 50 years. The ETK activity assay provides a sensitive and specific biomarker of thiamine status; however, there is a lack of consensus over the cutoffs for deficiency, partly due to a lack of assay harmonization. Here, we provide a step‐by‐step protocol for the measurement of ETK activity and the calculation of the ETK activity coefficient, including detailed explanations of equipment and chemicals required and guidance for quality control procedures. Harmonization of the protocol will provide the basis for the development of internationally recognized cutoffs for thiamine insufficiency. The establishment of quality control materials and a quality assurance scheme are recommended to provide reliability. This will ensure that the ETK activity assay remains an important method for the assessment of thiamine status

Carbon dioxide generation and drawdown during active orogenesis of siliciclastic rocks in the Southern Alps, New Zealand

C.D.M. was supported by NERC CASE PhD studentship award NE/G524160/1 (GNS Science, NZ, CASE partner). D.A.H.T. acknowledges support from research grants NE/H012842/1 and NE/J022128/1 and a Royal Society Wolfson Research Merit Award (WM130051). S.C.C. was funded under GNS Science's “Impacts of Global Plate Tectonics in and around New Zealand Programme” (PGST Contract CO5X0203). J.C.A. was supported by NSF OCE1334758. We also thank Matthew Cooper, Andy Milton, Darryl Green and Lora Wingate for laboratory assistance. We thank Mike Bickle for editorial advice and comments, and reviews from two anonymous reviewers that improved this manuscript.Peer reviewedPublisher PD

Crop Updates 2008 - Cereals

This session covers twenty four papers from different authors: WHEAT AGRONOMY 1. Wheat variety performance in the Northern Agricultural Region in 2007, Christine Zaicou, Department of Agriculture and Food 2. Wheat variety performance on the Central Agricultural Region in 2007, Shahajahan Miyan, Department of Agriculture and Food 3. Response of wheat varieties to sowing time in the Great Southern and Lakes Region in 2007, Brenda Shackley and Steve Penny, Department of Agriculture and Food 4. Wheat variety performance in the South Coastal Region in 2007, Sarah Ellis, Department of Agriculture and Food 5. Flowering dates of wheat varieties in Western Australia in 2007, Darshan Sharma, Brenda Shackley and Christine Zaicou, Department of Agriculture and Food BARLEY AGRONOMY 6. Barley variety options for Western Australia, Blakely Paynter, Andrea Hills and Jeff Russell, Department of Agriculture and Food 7. Vlaming A – the newest malting barley variety, Blakely Paynter, Jeff Russell and Andrea Hills, Department of Agriculture and Food 8. Barley yields higher in wide rows with stubble retained in a very dry season at Merredin, Glen Riethmuller, Bill Bowden and Paul Blackwell, Department of Agriculture and Food HERBICIDE TOLERANCE 9. Herbicide tolerance of current/new wheat varieties, Dr Harmohinder Dhammu, Department of Agriculture and Food 10. Herbicide tolerance of new oat varieties, Dr Harmohinder Dhammu, Vince Lambert, and Chris Roberts,Department of Agriculture and Food NUTRITION 11. Managing nitrogen inputs in malting barley, Andrea Hills and Blakely Paynter, Department of Agriculture and Food 12. Decision tools for optimal N on cereal crops, David and Sally Cox, Jeremy Lemon* and Andrea Hills*, *Department of Agriculture and Food 13. Wheat varieties respond differently to potassium application on potassium responsive soils, Paul Damon and Zed Rengel, Faculty of Natural and Agricultural Sciences, University of Western Australia DISEASES 14. Leaf disease management in continuous barley in the northern and central grainbelt of WA, Geoff Thomas, Ciara Beard, Anne Smith, Kith Jayasena and Sean Kelly, Department of Agriculture and Food 15. Temperature and moisture requirements of leaf, stem and stripe rusts of wheat, Geoff Thomas, Rob Loughman and Bill MacLeod, Department of Agriculture and Food 16. Fungicide options for controlling diseases in oats, Raj Malik and Blakely Paynter, Department of Agriculture and Food 17. Survey of wheat root diseases under intensive cereal production in Western Australia during 2005-2007, Ravjit Khangura, William MacLeod, Vivien Vanstone, Colin Hanbury, Mehreteab Aberra, Gordon MacNish and Robert Loughman, Department of Agriculture and Food 18. Epidemiology studies on Wheat Streak Mosaic Virus in 2007, Brenda Coutts, Geoff Strickland, Monica Kehoe, Dustin Severtson and Roger Jones, Department of Agriculture and Food 19. Bacterial diseases that affect WA export hay quality, Dominie Wright and Megan Jordan, Department of Agriculture and Food SOIL 20. Hardpan penetration ability of drought-stressed wheat under pot and field conditions, Xinhua He1, Eli Manyol1, Song-Ai Nio1, Imran Malik1, Tina Botwright-Acuña1,2and Len Wade1,3,1School of Plant Biology, University of Western Australia, 2Tasmanian Institute of Agricultural Research, University of Tasmania, TAS, 3E.H. Graham Centre, Charles Sturt University, NSW HARVEST MANAGEMENT 21. Calculating the risk – the SEPWA Harvest Calculator, Nigel Metz, South East Premium Wheat Growers Association 22. The relationship between grain moisture and atmospheric conditions in cereal crop harvesting on the South Coast of WA, Nigel Metz, South East Premium Wheat Growers Association (SEPWA) MARKETS 23. Varietal accreditation for Australian Barley, Linda Price, Barley Australia STATISTICAL METHODS 24. Applying data mining tools to improve grain quality for growers, Dean Diepeveen1, Leisa Armstrong2, Peter Clarke1, Doug Abrecht1, Rudi Appels2 and Matthew Bellgard3,1Department of Agriculture and Food, Western Australia 2Edith Cowan University, Western Australia, 3Centre of Comparative Genomics, Murdoch Universit

Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business-as-usual CO2 emission scenario until year 4000 AD

A new model of global climate, ocean circulation, ecosystems, and biogeochemical cycling, including a fully coupled carbon cycle, is presented and evaluated. The model is consistent with multiple observational data sets from the past 50 years as well as with the observed warming of global surface air and sea temperatures during the last 150 years. It is applied to a simulation of the coming two millennia following a business-as-usual scenario of anthropogenic CO2 emissions (SRES A2 until year 2100 and subsequent linear decrease to zero until year 2300, corresponding to a total release of 5100 GtC). Atmospheric CO2 increases to a peak of more than 2000 ppmv near year 2300 (that is an airborne fraction of 72% of the emissions) followed by a gradual decline to ∼1700 ppmv at year 4000 (airborne fraction of 56%). Forty-four percent of the additional atmospheric CO2 at year 4000 is due to positive carbon cycle–climate feedbacks. Global surface air warms by ∼10°C, sea ice melts back to 10% of its current area, and the circulation of the abyssal ocean collapses. Subsurface oxygen concentrations decrease, tripling the volume of suboxic water and quadrupling the global water column denitrification. We estimate 60 ppb increase in atmospheric N2O concentrations owing to doubling of its oceanic production, leading to a weak positive feedback and contributing about 0.24°C warming at year 4000. Global ocean primary production almost doubles by year 4000. Planktonic biomass increases at high latitudes and in the subtropics whereas it decreases at midlatitudes and in the tropics. In our model, which does not account for possible direct impacts of acidification on ocean biology, production of calcium carbonate in the surface ocean doubles, further increasing surface ocean and atmospheric pCO2. This represents a new positive feedback mechanism and leads to a strengthening of the positive interaction between climate change and the carbon cycle on a multicentennial to millennial timescale. Changes in ocean biology become important for the ocean carbon uptake after year 2600, and at year 4000 they account for 320 ppmv or 22% of the atmospheric CO2 increase since the preindustrial era

AI is a viable alternative to high throughput screening: a 318-target study

: High throughput screening (HTS) is routinely used to identify bioactive small molecules. This requires physical compounds, which limits coverage of accessible chemical space. Computational approaches combined with vast on-demand chemical libraries can access far greater chemical space, provided that the predictive accuracy is sufficient to identify useful molecules. Through the largest and most diverse virtual HTS campaign reported to date, comprising 318 individual projects, we demonstrate that our AtomNet® convolutional neural network successfully finds novel hits across every major therapeutic area and protein class. We address historical limitations of computational screening by demonstrating success for target proteins without known binders, high-quality X-ray crystal structures, or manual cherry-picking of compounds. We show that the molecules selected by the AtomNet® model are novel drug-like scaffolds rather than minor modifications to known bioactive compounds. Our empirical results suggest that computational methods can substantially replace HTS as the first step of small-molecule drug discovery

Finishing the euchromatic sequence of the human genome

The sequence of the human genome encodes the genetic instructions for human physiology, as well as rich information about human evolution. In 2001, the International Human Genome Sequencing Consortium reported a draft sequence of the euchromatic portion of the human genome. Since then, the international collaboration has worked to convert this draft into a genome sequence with high accuracy and nearly complete coverage. Here, we report the result of this finishing process. The current genome sequence (Build 35) contains 2.85 billion nucleotides interrupted by only 341 gaps. It covers ∼99% of the euchromatic genome and is accurate to an error rate of ∼1 event per 100,000 bases. Many of the remaining euchromatic gaps are associated with segmental duplications and will require focused work with new methods. The near-complete sequence, the first for a vertebrate, greatly improves the precision of biological analyses of the human genome including studies of gene number, birth and death. Notably, the human enome seems to encode only 20,000-25,000 protein-coding genes. The genome sequence reported here should serve as a firm foundation for biomedical research in the decades ahead

Bedrock geology of DFDP-2B, central Alpine Fault, New Zealand

<p>During the second phase of the Alpine Fault, Deep Fault Drilling Project (DFDP) in the Whataroa River, South Westland, New Zealand, bedrock was encountered in the DFDP-2B borehole from 238.5–893.2 m Measured Depth (MD). Continuous sampling and meso- to microscale characterisation of whole rock cuttings established that, in sequence, the borehole sampled amphibolite facies, Torlesse Composite Terrane-derived schists, protomylonites and mylonites, terminating 200–400 m above an Alpine Fault Principal Slip Zone (PSZ) with a maximum dip of 62°. The most diagnostic structural features of increasing PSZ proximity were the occurrence of shear bands and reduction in mean quartz grain sizes. A change in composition to greater mica:quartz + feldspar, most markedly below c. 700 m MD, is inferred to result from either heterogeneous sampling or a change in lithology related to alteration. Major oxide variations suggest the fault-proximal Alpine Fault alteration zone, as previously defined in DFDP-1 core, was not sampled.</p