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Academic literature on the topic 'Tufts St'

Author: Grafiati
Published: 4 June 2021
Last updated: 15 February 2022

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Journal articles on the topic "Tufts St"

1

Isner, Jeffrey M., Ken Walsh, Kenneth Rosenfield, et al. "Arterial Gene Therapy for Restenosis. St. Elizabeth's Medical Center, Tufts University School of Medicine, Boston, Massachusetts." Human Gene Therapy 7, no. 8 (1996): 989–1011. http://dx.doi.org/10.1089/hum.1996.7.8-989.

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2

Isner, Jeffrey M., Ken Walsh, James Symes, et al. "Arterial Gene Transfer for Therapeutic Angiogenesis in Patients with Peripheral Artery Disease. St. Elizabeth's Medical Center, Tufts University School of Medicine, Boston, Massachusetts." Human Gene Therapy 7, no. 8 (1996): 959–88. http://dx.doi.org/10.1089/hum.1996.7.8-959.

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3

Senelick, Laurence. "The Accidental Evolution of the Moscow Art Theatre Prague Group." New Theatre Quarterly 30, no. 2 (2014): 154–67. http://dx.doi.org/10.1017/s0266464x14000268.

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During the period of confusion and divided loyalties that followed the 1917 Revolution in Russia, the resources of the Moscow Art Theatre were severely depleted, and its artists and staff found themselves giving barebones performances for the enlightenment of often mystified working-class audiences. By 1919 the decision was taken to split the company, with a contingent sent out on tour with the intention of rejoining the parent group for the new season. In the event, with civil war raging between the forces of the Red Army and the White Guard, this did not happen, and groups of former members of the Art Theatre worked independently in the provinces and eventually abroad. While some returned to Moscow in 1922, the ‘Prague Group of the Moscow Art Theatre’ continued to lead an independent existence, and in this article Laurence Senelick traces the events leading up to and following its creation – which caused much annoyance to Stanislavsky and confusion in the West. A frequent contributor to New Theatre Quarterly, Laurence Senelick is Fletcher Professor of Drama and Oratory at Tufts University and a Fellow of the American Academy of Arts and Sciences. He is a recipient of the St George medal of the Ministry of Culture of the Russian Federation for services to Russian art and scholarship. His latest books are Stanislavsky: a Life in Letters (Routledge) and the forthcoming Soviet Theatre: a Documentary History (Yale University Press).
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4

Grey, I. E., A. R. Kampf, J. R. Price, and C. M. Macrae. "Bettertonite, [Al6(AsO4)3(OH)9(H2O)5]·11H2O, a new mineral from the Penberthy Croft mine, St. Hilary, Cornwall, UK, with a structure based on polyoxometalate clusters." Mineralogical Magazine 79, no. 7 (2015): 1849–58. http://dx.doi.org/10.1180/minmag.2015.079.7.16.

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AbstractBettertonite, ideally [Al6(AsO4)3(OH)9(H2O)5]·11H2O, is a new mineral from the Penberthy Croft mine, St. Hilary, Cornwall, England, UK. It occurs as tufts of white, ultrathin (sub-micrometre) rectangular laths, with lateral dimensions generally <20 μm. The laths are flattened on {010} and exhibit the forms {010}, {100} and {001}. The mineral is associated closely with arsenopyrite, chamosite, liskeardite, pharmacoalumite, pharmacosiderite and quartz. Bettertonite is translucent with a white streak and a vitreous to pearly, somewhat silky lustre. The calculated density is 2.02 g/cm3. Optically, bettertonite is biaxial positive with α = 1.511(1), β = 1.517(1), γ = 1.523(1) (in white light). The optical orientation is X = c, Y= b, Z = a. Pleochroism was not observed. Electron microprobe analyses (average of 4) with H2O calculated on structural grounds and analyses normalized to 100% gave Al2O3 = 29.5, Fe2O3 = 2.0, As2O5= 30.1, SO3 = 1.8, Cl = 0.5, H2O = 36.2. The empirical formula, based on 9 metal atoms is Al5.86Fe0.26(AsO4)2.65(SO4)0.23(OH)9.82Cl0.13(H2O)15.5. Bettertoniteis monoclinic, space group P21/c with unit-cell dimensions (100 K): a = 7.773(2), b = 26.991(5), c = 15.867(3) Å, β = 94.22(3)°. The strongest lines in the powder X-ray diffraction pattern are [dobs in Å(I)(hkl)] 13.648(100)(011); 13.505(50) (020); 7.805(50)(031); 7.461(30)(110); 5.880(20)(130); 3.589(20)(02); 2.857(14)(182). The structure of bettertonite was solved and refined to R1 = 0.083 for 2164 observed (I > 2σ(I)) reflections to a resolutionof 1 Å. Bettertonite has a heteropolyhedral layer structure, with the layers parallel to (010). The layers are strongly undulating and their stacking produces large channels along [100] that are filled with water molecules. The basic building block in the layers is a hexagonal ring ofedge-shared octahedra with an AsO4 tetrahedron attached to one side of the ring by corner-sharing. These polyoxometalate clusters, of composition [AsAl6O11(OH)9(H2O)5]8–, are interconnected along [100] and [001]by corner-sharing with other AsO4 tetrahedra.
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5

Grey, I. E., J. Betterton, A. R. Kampf, C. M. Macrae, F. L. Shanks, and J. R. Price. "Penberthycroftite, [Al6(AsO4)3(OH)9(H2O)5]·8H2O, a second new hydrated aluminium arsenate mineral from the Penberthy Croft mine, St. Hilary, Cornwall, UK." Mineralogical Magazine 80, no. 7 (2016): 1149–60. http://dx.doi.org/10.1180/minmag.2016.080.069.

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AbstractPenberthycroftite, ideally [Al6(AsO4)3(OH)9(H2O)5]·8H2O, is a new secondary aluminium arsenate mineral from the Penberthy Croft mine, St. Hilary, Cornwall, England, UK. It occurs as tufts of white, ultrathin (sub-micrometre) rectangular laths, with lateral dimensions generally < 20 μm. The laths are flattened on {010} and elongated on [100]. The mineral is associated with arsenopyrite, bettertonite, bulachite, cassiterite, chalcopyrite, chamosite, goethite, liskeardite, pharmacoalumite–pharmacosiderite and quartz. Penberthycroftite is translucent with a white streak and a vitreous to pearly lustre. The calculated density is 2.18 g/cm3. Optically, only the lower and upper refractive indices could be measured, 1.520(1) and 1.532(1) respectively. No pleochroism was observed. Electron microprobe analyses (average of 14) with H2O obtained from thermogravimetric analysis and analyses normalized to 100% gave Al2O3 = 31.3, Fe2O3 = 0.35, As2O5 = 34.1, SO3 = 2.15 and H2O = 32.1. The empirical formula, based on nine metal atoms and 26 framework anions is [Al5.96Fe0.04(As0.97Al0.03O4)3(SO4)0.26(OH)8.30(H2O)5.44](H2O)7.8, corresponding to the ideal formula [Al6(AsO4)3(OH)9(H2O)5]·8H2O. Penberthycroftite is monoclinic, space group P21/c with unit-cell dimensions (100 K): a = 7.753(2) Å, b = 24.679(5) Å, c = 15.679(3) Å and β = 94.19(3)°. The strongest lines in the powder X-ray diffraction pattern are [dobs in Å(I) (hkl)] 13.264(46) (011); 12.402(16)(020); 9.732(100)(021); 7.420(28)(110); 5.670(8)(130); 5.423(6)(1̄31). The structure of penberthycroftite was solved using synchrotron single-crystal diffraction data and refined to wRobs = 0.059 for 1639 observed (I> 3σ(I)) reflections. Penberthycroftite has a heteropolyhedral layer structure, with the layers parallel to {010}. The layers are strongly undulating and their stacking produces large channels along [100] that are filled with water molecules. The layers are identical to those in bettertonite, but they are displaced relative to one another along [001] and [010] such that the interlayer volume is decreased markedly (by ∼10%)relative to that in bettertonite, with a corresponding reduction in the interlayer water content from 11 H2O per formula unit (pfu) in bettertonite to 8 H2O pfu in penberthycroftite.
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6

Young, James. "Reviewer Acknowledgements." International Journal of Social Science Studies 7, no. 3 (2019): 133. http://dx.doi.org/10.11114/ijsss.v7i3.4242.

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International Journal of Social Science Studies (IJSSS) would like to acknowledge the following reviewers for their assistance with peer review of manuscripts for this issue. Many authors, regardless of whether IJSSS publishes their work, appreciate the helpful feedback provided by the reviewers. Their comments and suggestions were of great help to the authors in improving the quality of their papers. Each of the reviewers listed below returned at least one review for this issue.Reviewers for Volume 7, Number 3Ahmet Yıkmış, Abant Izzet Baysal Univeersity, TurkeyAmany Albert, Beni-Suef University, EgyptAmir Hossain, IBAIS University, BangladeshAnna Maria Mouza, Technological Educational Institution of Serres, GreeceAntónio Calha, Polytechnic Institute of Portalegre, PortugalAslan,Yasin, Sinop University, TurkeyBassam Yousef Ibrahim Banat, Al-Quds University, PalestineBegoña Montero-Fleta, Universitat Politécnica de València, SpainBo Li, St Ambrose University, USAChris Gilleard, University College London, UKEmanuele Achino, C. D. T. O., ItalyFernando Aragón-Durand, National Autonomous University of Mexico, MexicoGonzalo Capellan-Miguel, Spanish Minister of Education in United Kingdom, SpainHao Liu, Beijing Normal University, ChinaHenry Poduthas, West Texas A&M University, USAHyejin Lee, Tufts University, MA, USA and Konkuk University, Seoul, South Korea, USAJesster Pasule Eduardo, Nueva Ecija University of Science and Technology, PhilippinesJulia M. Mack, Gannon University, USALaura Diaconu Maxim, "Alexandru Ioan Cuza University" of Iasi, RomaniaLing Wei, China Foreign Affairs University, ChinaMałgorzata Haładewicz, Opole University of Technology, PolandMasami Tsuji, Meiji University, JapanMei-Ling Lin, National Open University, TaiwanMickey Langlais, University of Nebraska – Kearney, USAMikiyasu Nakayama, the University of Tokyo, JapanMohamed Mehdi Jelassi, IHEC Carthage, TunisiaMohammad Naji Shah Mohammadi, Kuala Lumpur, MalaysiaOzgur Demirtas, Inonu University, TurkeyRachita Shrivastava Roy, Department of Higher Education, Chhatisgarh-India, IndiaRakesh Arya, Jawaharlal Nehru University, New Delhi, India Raymond Chan, City University of Hong Kong, Hong KongRemigiusz Kijak, "University of Warsaw, PolandRenu, Central University of Haryana, India Riam Elmorshedy, South Valley University, EgyptRodrigo Cabrera Pertusatti, University of Buenos Aires, ArgentinaSana Ali, Allama Iqbal Open University, Islamabad, PakistanSandro Serpa, University of the Azores, PortugalSharif Alghazo, University of Jordan, JordanShariq aziz butt, Superior University Lahore, PakistanYanzhe Zhang, Jilin University, China
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7

Trigiano, R. N., T. A. Rinehart, M. M. Dee, P. A. Wadl, L. Poplawski, and B. H. Ownley. "First Report of Aerial Blight of Ruth's Golden Aster (Pityopsis ruthii) Caused by Rhizoctonia solani in the United States." Plant Disease 98, no. 6 (2014): 855. http://dx.doi.org/10.1094/pdis-11-13-1181-pdn.

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Ruth's golden aster (Pityopsis ruthii (Small) Small: Asteraceae) is an endangered, herbaceous perennial that occurs only at a few sites along the Hiwassee and Ocoee rivers in Polk County, Tennessee. This species is drought, heat, and submergence tolerant and has ornamental potential as a fall flowering landscape plant. In 2012, we vegetatively propagated various genotypes and established plantings in a landscape at Poplarville, Mississippi. In June and July of 2013, during periods of hot and humid weather, several well-established plants exhibited black or brown necrotic aerial blight symptoms including desiccation of stems and leaves. Blighted leaf samples were surface sterilized (10% commercial bleach, active ingredient 8.25% sodium hypochlorite, 1 min), rinsed in sterile water, air-dried, and plated on 2% water agar amended with 3.45 mg fenpropathrin/liter (Danitol 2.4 EC, Valent Chemical, Walnut Creek, CA) and 10 mg/liter rifampicin (Sigma-Aldrich, St. Louis, MO). Rhizoctonia sp. was identified based on hyphal morphology and cultures were maintained on potato dextrose agar. Colonies were fast growing, consisting of light tan to brown mycelia and tufts of crystalline aerial hyphae. Within 10 days, brown exudates were present in cultures and there was no pigmented reverse to the agar. Hyphae were a mean of 5.2 μm wide (4.6 to 6.1 μm; n = 10) and each compartment contained three or more nuclei. Hyphae were constricted at septa with right angle branching and no clamp connections, which is typical for Rhizoctonia solani (1). Light- to medium-brown, oblong to irregularly shaped sclerotia measuring 1.2 mm long (0.7 to 2.1 mm) × 0.9 mm wide (0.5 to 1.2 mm; n = 20) were formed in cultures after 3 weeks of growth. Total genomic DNA was extracted from two different colonies grown in potato dextrose broth for 7 days, amplified with PCR using ITS1 and ITS4 primers for amplification of the 18S rDNA subunit (2), the products purified, and sequenced. A consensus sequence of 657 bp was deposited in GenBank (Accession Nos. KF843729 and KF843730) and was 96% identical to two R. solani Kühn ITS sequences in GenBank (HF678125 and HF678122). R. solani was grown on twice autoclaved oats for 2 weeks at 21°C and incorporated into Pro-Mix BX, low fertility soilless medium (Premier Horticulture, Rivière-du-Loup, Quebec, Canada) at 4% (w/w) to inoculate seven P. ruthii plants grown in 10 cm-diameter pots; seven additional plants were grown in the same medium amended with 4% (w/w) sterile oats. Plants were grown in a greenhouse and covered with a plastic dome to maintain high humidity. After 2 weeks, six of the seven inoculated plants exhibited the same aerial blight symptoms as did the original infected plants from the field; none of the control plants developed disease symptoms. Colony morphology and hyphal characteristics as well as the sequence for the ITS region of rDNA from the re-isolated fungus were identical to the original isolate. To our knowledge, this is the first report of R. solani infecting Ruth's golden aster. We are not aware of the disease occurring in wild populations of the plant, but may impact plants grown in the landscape or greenhouse. References: (1) B. Sneh et al. Identification of Rhizoctonia Species. The American Phytopathological Society, St Paul, MN, 1991. (2) T. J. White et al. Page 315 in: PCR Protocols: A Guide to Methods and Applications. M. A. Innis et al., eds. Academic Press, San Diego, CA, 1990.
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Bradley, C. A., and S. Li. "First Report of Northern Stem Canker of Soybean Caused by Diaporthe phaseolorum var. caulivora in North Dakota." Plant Disease 90, no. 5 (2006): 687. http://dx.doi.org/10.1094/pd-90-0687a.

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In early September 2003, patches of soybean (Glycine max) plants in a field in Foster County, ND had dead branches with reddish brown cankers at the nodes. Stem tissue with cankers from two plants were excised and immersed in a 0.5% NaOCl solution for 1 min, rinsed with sterilized distilled water, and placed into Petri dishes containing potato dextrose agar (PDA) amended with streptomycin sulfate (200 mg/liter). Four fungi were hyphal tipped and grown on PDA, acidified PDA, or water agar (WA) with soybean stem pieces incubated at 21°C with 24-h light and identified by culture and spore morphology after 3 to 4 weeks. Cultures were identified as Diaporthe phaseolorum var. caulivora that produced white colonies with interspersed cottony tufts of mycelium on PDA (1). Stromata were small and scattered irregulary on the plate. Perithecia of the D. phaseolorum var. caulivora isolates were black and globose with eight-spored asci formed on soybean stem pieces on WA. To confirm pathogenicity of the D. phaseolorum var. caulivora isolates, soybean plants (cv. NuTech 0606) were grown in the greenhouse and inoculated with recovered D. phaseolorum var. caulivora isolates. The stems of soybean plants at the V3 stage were excised just below the fourth node. Mycelia plugs of the four different 1-week-old cultures of D. phaseolorum var. caulivora were placed into the large end of disposable micropipette tips (200 μl). The micropipette tip containing a D. phaseolorum var. caulivora culture was subsequently placed over a cut soybean stem. The four D. phaseolorum var. caulivora isolates were used to inoculate 10 stems apiece. To serve as controls, 10 cut soybean stems were inoculated with micropipette tips containing plugs of noninfested PDA and 10 cut stems were not inoculated. Ten days after inoculation, micropipette tips were removed and lesions that had developed on the stem were measured. The mean lesion lengths of the D. phaseolorum var. caulivora inoculated stems ranged from 48 to 82 mm and were significantly (P ≤ 0.05) greater than the lesion lengths of the noninfested PDA (3 mm) and no PDA (1 mm) controls. Northern stem canker was only observed in the one field; however, surveys were not conducted to determine the prevalence of the disease throughout the soybean-production area of North Dakota. To our knowledge, this is the first report of northern stem canker on soybean in North Dakota. Reference: (1) F. A. Fernandez et al. Stem canker. Pages 33–35 in: Compendium of Soybean Diseases. 4th ed. The American Phytopathological Society, St. Paul, MN, 1999.
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Fernández-Pavía, S. P., G. Rodríguez-Alvarado, and J. M. Sánchez-Yañez. "Buckeye Rot of Tomato Caused by Phytophthora capsici in Michoacan, Mexico." Plant Disease 87, no. 7 (2003): 872. http://dx.doi.org/10.1094/pdis.2003.87.7.872c.

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The state of Michoacan is one of the main fresh pepper (Capsicum annuum L.) and tomato (Lycopersicon esculentum Mill.) producers in Mexico. During the last 5 years, pepper-producing areas in the state have become unproductive due to root-rotting pathogens, mainly Phytophthora capsici Leonian. Growers trying to overcome losses have increased tomato production in areas previously used for pepper production. Field-grown tomato plants with diseased green tomato fruits were observed in Tacambaro, Michoacan, during August 2002. Initially, brown-to-black lesions developed on fruits in contact with soil, followed by infection of the upper fruits in the raceme. Lesions enlarged and dark zonate “buckeye” bands were formed in the affected area. Diseased fruit turned mushy. Symptoms observed were similar to those described for buckeye rot of tomato (1). Diseased fruit were surface disinfested with 70% ethanol, cut into 0.5-cm slices, and incubated in a moist chamber to induce mycelial colonization. Isolation from mycelial tufts growing through the tomato slice was performed 3 days later, and mycelia was transferred to PARP selective medium (corn meal agar (CMA) plus ampicillin, pimaricin, rifampicin, and pentachloronitrobenzene). P. capsici was consistently isolated from diseased tomato fruits. Oomycete identification was based on sporangial and gametangial characteristics of cultures grown on CMA (1). Sporangia microscopically observed were spherical, broadly ellipsoid or obovoid with one papilla (occasionally two papillae), and deciduous with a long pedicel. Chlamydospores were not present (2). The isolates were heterothallic, and oogonia with amphigynous antheridia were observed in pairings with A1 and A2 isolates of P. capsici. Three isolates were A1 and two isolates were A2. To confirm pathogenicity, two experiments were performed using 20 healthy unwounded green tomatoes. One isolate of each mating type was tested. Isolates were grown for 5 days on CMA, and fruits were inoculated by placing P. capsici in contact with the fruit. Inoculated fruits were kept in a moist chamber at room temperature (17 to 20°C). Initial symptoms in the form of brown-to-black lesions appeared 24 h after inoculation. One week after inoculation, symptoms were similar to those observed in field-grown plants, and P. capsici was recovered from the margins of the diseased tissue. All inoculated fruits rotted. To our knowledge, this is the first report of P. capsici causing buckeye rot on tomato in Michoacan and of the presence of both mating types in the area. Reference: (1) D. C. Erwin and O. K. Ribeiro. Phytophthora Diseases Worldwide. The American Phytopathological Society. St. Paul MN, 1996. (2) M. Aragaki and J. Y. Uchida. Mycologia 93:137, 2001.
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Awadallah, Sherif AM, and Richard N. Hiscott. "High-resolution stratigraphy of the deep-water lower Cloridorme Formation (Ordovician), Gaspé Peninsula, based on K-bentonite and megaturbidite correlations." Canadian Journal of Earth Sciences 41, no. 11 (2004): 1299–317. http://dx.doi.org/10.1139/e04-078.

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The Ordovician Cloridorme Formation is a thick foreland-basin turbidite succession that for several decades has served as a natural laboratory for the long-distance physical tracing and study of single turbidites. A robust temporal correlation of these deposits is a prerequisite for the evaluation of sedimentary processes. Published stratigraphic subdivisions of the lower part of the Cloridorme Formation have impeded rather than facilitated such studies because of errors in the physical correlation of contemporaneous deposits. Tracing of the deposits of exceptionally large gravity flows, known as "megaturbidites," was previously recognized as a useful stratigraphic tool. Here, we strengthen and revise the stratigraphic framework based on megaturbidites by considering nine widely traceable and geochemically fingerprinted tuffs (K-bentonites). Two discriminant functions incorporating the abundances of six trace elements (V, Sm, Nd, Th, Er, Zr) permit the unambiguous distinction of the lower four tuffs. The other tuffs can be successfully distinguished using bivariate plots of TiO2, Th, Sc, and Eu. The tracing and correlation of 71 megaturbidites and the nine K-bentonites permits a high-resolution subdivision of the lower Cloridorme Formation. Particularly thick megaturbidites mark the boundaries of three newly defined allostratigraphic members (St-Hélier Allomember, St-Yvon Allomember, and Petite-Vallée Allomember). This precise temporal framework shows that the stratigraphic heights of the contacts of lithostratigraphic members defined by other workers in 1969 and 1991 were miscorrelated by more than 400 m over short lateral distances!
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Books on the topic "Tufts St"

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Consultants, GEI. Partial permanent solution statement for 6 Reed Court, Somerville: 50 Tufts Street site, Somerville, Massachusetts. GEI Consultants, Inc., 2016.

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Consultants, GEI. Partial permanent solution statement for 84 Washington Street (Lot 2), Somerville, Massachusetts: 50 Tufts Street site, Somerville, Massachusetts. GEI Consultants, 2016.

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Consultants, GEI. Class B-1 response action outcome partial statement for 67 Knowlton Street, Somerville, Massachusetts: 50 Tufts Street site, Somerville, Massachusetts. GEI Consultants, 2014.

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Consultants, GEI. Class B-1 response action outcome partial statement for 65 Franklin Avenue, Somerville, Massachusetts: 50 Tufts Street site, Somerville, Massachusetts. GEI Consultants, 2014.

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Consultants, GEI. Class B-1 response action outcome partial statement for 79 Washington Street, Somerville, Massachusetts: 50 Tufts Street site, Somerville, Massachusetts. GEI Consultants, 2014.

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Fay, Jessica. ‘My second Self when I am gone’. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198816201.003.0004.

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This chapter traces the cumulative influence of Wordsworth’s reading of a series of topographical and antiquarian studies on the poetry and prose he produced between 1807 and 1810. These sources contain extensive details about medieval monastic life in the north of England and describe how powerful coenobitic communities shaped the cultural and geographical landscapes they inhabited. The chapter shows how knowledge of the civic operation of the monastic world influenced Wordsworth’s thinking about primogeniture, living legacy, memorialization, and familial and democratic representation. It explains why Wordsworth was particularly drawn to St Basil, suggesting that aspects of Basil’s monastic system infiltrated The Tuft of Primroses (1808) and the Convention of Cintra (1809), and that the saint’s formulation of the Holy Trinity inflected Wordsworth’s Essays uponEpitaphs (1810). The chapter offers a new context in which to interpret Wordsworth’s metaphor of language as the ‘incarnation’ of thought.
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Book chapters on the topic "Tufts St"

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Wohl, Ellen. "December: Saving the Dammed." In Saving the Dammed. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190943523.003.0015.

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At the nadir of the year, this is how morning comes to the beaver meadow. Just as the sun rises above the eastern horizon, a flush of pale rose lights the snow newly fallen on the highest peaks. The beaver meadow remains in shadow, silent but for the creek flowing quietly between its rims of ice. The air temperature is well below freezing and frost whitens the pine needles like a dark-haired person starting to go gray. Wisps and sheets of snow flag off the summits in the steady wind. Over the course of a few minutes, the summit snow warms from pale rose to faint orange and then a rich, warm gold that also lights the rock outcrops at lower elevations. The wind reaches the beaver meadow before the sunlight, coming in abrupt blasts that shake loose the little tufts of snow remaining on the pine boughs. The wind sends the snow crystals slaloming across the ice on the creek with a dry, skittering sound like that of blowing sand. Before long, the meadow is submerged in a continual rushing sound created by wind gusting through the pines up slope, along the valley walls. The lateral moraine to the south keeps the beaver meadow in shadow until 9:30 a.m. Nothing is so slow as waiting for the warmth of sunlight on a cold winter morning. When the sunlight does reach the meadow, it brings out the colors of water, ice, grasses, and willows. Flowing portions of the creek change from gray to orange brown. The snow reflects the light in a painfully intense glare broken by the deep, long shadows that everything casts. With the sunlight comes a steady wind that blasts the crystalline snow onto my face like grit. Not much snow has fallen yet, but North St. Vrain Creek is completely frozen in places and covered with snow. The ice records the movements of water, freezing the pulses and turbulence in ice ripples and ledges, motionless swirls and bands. It seems a miracle that any water still flows in this gray and white world of ice and snow.
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PRIOR, RONALD L., and GUOHUA CAO. "IN VIVO TOTAL ANTIOXIDANT CAPACITY: COMPARISON OF DIFFERENT ANALYTICAL METHODS11Mention of a trade name, proprietary product, or specific equipment does not constitute a guarantee by the U.S. Department of Agriculture and does not imply its approval to the exclusion of other products that may be suitable.Address correspondence to: R. L. Prior, Ph.D., USDA, ARS, HNRCA, 711 Washington St., Boston, MA 02111, USA; Tel: (617) 556–3311; Fax: (617) 556-3222; E-Mail: prior@hnrc.tufts.eduDr. Ronald Prior is a Nutritionist and Laboratory Chief of the Phytochemical Laboratory at the Jean Mayer USDA Human Nutrition Research Center on Aging (HNRCA) at Tufts University, Boston, MA. Dr. Prior received his B.S. degree with honors from the University of Nebraska and he received his Ph.D. in Nutrition and Biochemistry from Cornell University in 1972. Dr. Prior has worked with the USDA for more than 20 years.During the past 12 years at the HNRCA, he has been Scientific Program Officer and has directed research activities dealing with the role of flavonoid and other phenolic food components on antioxidant status, their metabolism, and relationships to diseases of aging.Guohua Cao, M.D., Ph.D., is currently a Scientist II at HNRCA. Dr. Cao studied medicine in Nantong Medical College in 1979 and at Nanjing Medical University in 1984. He obtained his Ph.D. in nutritional biochemistry from Beijing Medical University in 1990. Dr. Cao came to the United States in 1991 and worked at NIH where he was instrumental in developing the ORAC method." In Bio-Assays for Oxidative Stress Status. Elsevier, 2001. http://dx.doi.org/10.1016/b978-0-444-50957-4.50009-0.

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