Kvæðasafn, 1. bindi Benedikt Þórðarson; Bjarni Jónsson; Bjarni Jónsson á Þorleifsstöðum ...
1845/1840
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Jón Sigurðsson fékk handritin frá Þorsteini ÞorsteinssyniSveini Skúlasyni
Auk þess er hér að finna margt fornkvæða, þjóðkvæða og lausavísna ónafngreindra höfunda.
Pappír.
Skinnband.
The Krýsuvík area in SW Iceland is characterized by a 40 km long and around 6–8 km wide fissure swarm and two NE-SW trending tindars complexes. Associated with the fissure swarms are fumarole fields ...located primarily on parallel postglacial eruptive fissure segments. There are indications that Krýsuvík hosts a buried caldera and an intrusion complex in its roots. The geothermal surface manifestations cover an area of around 50–60 km2 and has potential for future exploitation. Faulting accompanies the ridges and postglacial volcanic fissures, with normal faults and open fissures with a maximum throw of 10 m.
A 3D inversion was performed of the static shift corrected off-diagonal impedance tensor elements of 102 MagnetoTelluric (MT) resistivity soundings from the Greater Krýsuvík geothermal area. In the inversion, 21 periods were used, evenly distributed from 0.01 to 100 s on a logarithmic scale. The robustness of the inversion was tested by using three different initial models: A model compiled from a joint 1D inversion of TEM and MT soundings, with a homogeneous Earth of resistivity 100 Ω m and a homogeneous Earth of resistivity 10 Ω m. A flat topographic surface was assumed in the 3D inversion. The resulting models were later elevation corrected. The results of the 1D inversion and the 3D inversion are strikingly similar, where the 1D inversion reproduces the main resistivity structures while the 3D inversion shows considerably more details. An analysis of the electrical strike directions based on the vertical magnetic field data is in fairly good agreement with the final resistivity model.
The subsurface resistivity structure in Krýsuvík has the same main features as other high temperature areas in Iceland and in general where the host rocks are basaltic. Above a shallow conductive cap, a high resistivity zone is seen, reflecting unaltered rock. The conductive cap reflects smectite hydrothermal mineral alteration. Below the low-resistivity cap, a resistive core is found, reflecting chlorite-epidote alteration. Good correlation is observed in the Krýsuvík field between the subsurface resistivity structure and the hydrothermal alteration revealed by boreholes cuttings. Parts of the field have cooled down and therefore the resistivity structure indicates alteration mineralogy but not necessarily the present rock temperature. The geothermal up-flow zones are therefore most likely where the hydrothermal alteration and the resistive core reach the highest elevation.
The 3D inversion shows an indication of a relatively deep-seated conductive body below the central part of the high temperature area. This body coincides horizontally with the centre of the 2010–2011 inflation source at 4–5 km depth. It has been suggested that the 2007–2016 inflation/deflation periods are linked to gas flux, as no signs of S-wave attenuation have been found. It is therefore unlikely that the deep-seated conductive body resolved by our resistivity models comprises partial melt. The body is probably connected to the heat source of the geothermal field and could be due to emission of gas or dehydration.
•Selection of drill site for the IDDP-1 well at Krafla in NE-Iceland.•Superheated and supercritical reservoir conditions.•MT-resistivity survey, seismic data and information from production well ...K-36.
This paper describes the site selection for the IDDP-1 well within the Krafla volcano in 2008. In a feasibility study in 2003, 12 potential well sites within three geothermal areas were suggested and prioritized to meet the goal of finding supercritical temperatures and pressures together with high permeability. In 2006 one of these priority sites was selected within the Krafla field, but in autumn 2007 due to its proximity to the Krafla power plant a new location had to be selected only a few months before drilling. Choice of that new site was justified by new MT-resistivity survey data, seismic data and information from an earlier nearby production well, K-36.
Prior to infusion, cryopreserved autologous peripheral blood stem cell (auto-PBSC) grafts can either be thawed at the bedside or thawed and washed at the laboratory. At our center, manual washing of ...grafts prior to infusion was discontinued in April 2012 and bedside thawing was implemented.
This study compares the outcomes of two patient groups who received auto-PBSC either after post-thaw washing (n = 84) or bedside thawing (n = 83).
No life-threatening infusion-related side effects were reported in either group. There was no significant difference in the mean CD34+ cells/kg dose of infused auto-PBSC in the two groups (p = 0.41), nor in the number of days to neutrophils > 0.5 × 10(9)/L (p = 0.14), days to platelets > 20 × 10(9)/L (p = 0.64), or days to platelets > 50 × 10(9)/L (p = 0.62) after transplant. There was also no difference in the number of days on total parenteral nutrition (p = 0.69), days on G-CSF therapy (p = 0.48), or days with fever (p = 0.73). Finally, there was no significant difference in the number of red cell units transfused (p = 0.32), or platelet units transfused (p = 0.94) after the transplant. One-hundred-day mortality was identical in the two groups (2.4%).
Both thawing procedures are safe and result in acceptable engraftment and patient outcomes.
Asthma is a complex genetic disorder with a heterogeneous phenotype, largely attributed to the interactions among many genes and between these genes and the environment. Numerous loci and candidate ...genes have been reported to show linkage and association to asthma and atopy. Although some studies reporting these observations are compelling, no gene has been mapped that confers a sufficiently high risk of asthma to meet the stringent criteria for genomewide significance. Using 175 extended Icelandic families that included 596 patients with asthma, we performed a genomewide scan with 976 microsatellite markers. The families were identified by cross-matching a list of patients with asthma from the Department of Allergy/Pulmonary Medicine of the National University Hospital of Iceland with a genealogy database of the entire Icelandic nation. We detected linkage of asthma to chromosome 14q24, with an allele-sharing LOD score of 2.66. After we increased the marker density within the locus to an average of one microsatellite every 0.2 cM, the LOD score rose to 4.00. We designate this locus “asthma locus one” (
AS1). Taken together, these results provide evidence of a novel susceptibility gene for asthma on chromosome 14q24.
Sögu- og rímnabók
Bjarnar saga Hítdælakappa
Grettis saga
Víglundar saga
Lýsing Grænlands
Rímur af Illuga Tagldarbana
10 rímur.
Rímur af Otúel frækna
8 rímur.
Rímur af Trójumönnum
Einungis mansöngvar ...rímnanna.
Pappír.
Vatnsmerki.
Skreyttir stafir, einna helst upphafsstafir hvers kafla á blöðum 2-52
Bókahnútar: 195v233v257v
Saurblöð eru úr ýmsum áttum meðal annars er uppskrift á dánarbúi Bjarni BjarnasonYtri-Þorsteinsstöðum
Skinnband með tréspjöldum, þrykkt
Stafirnir B.Þ. og S.A. eru þrykktir framan á kápu, að aftan er þrykkt ártalið 184….
Fremra spjaldblað er úr prentaðri Egils sögu.
Aftari spjaldblöð eru tvö, laus frá spjaldi, úr prentuðum ritum á dönsku og latínu.
Aftast í handriti liggur seðill (176 x 90 mm) úr bandi sem geymir brot úr kveðskap.
Kver Guðmundur Bergþórsson; Sigurður Breiðfjörð; Jóhannes Árnason ...
1833
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Kver
Illuga saga Gríðarfóstra
Úlfars saga sterka
Herrauðar saga og Bósa
Rímur af Eiríki víðförla
Rímur af Tístran og Indíönu
Kvæði
Þjófsbragur
Jóabragur
Roðhattskvæði
Pappír með vatnsmerkjum.
Á ...blöðum 1-8 er ekkert vatnsmerki.
Vatnsmerki 1. Aðalmerki: DEDB undir býkúpuDEERVEN D BLAUW9-16
Vatnsmerki 2. Aðalmerki: ØRHOLM & NYEMØLLE17-24
Vatnsmerki 3. Aðalmerki: Pro patriaKLIPPAN25-3956
Vatnsmerki 4. Aðalmerki: KórónaSHB40-55
Vatnsmerki 5. Aðalmerki: RONNEBY57-64
Vatnsmerki 6. Aðalmerki: BýkúpaH&S undir tvöföldu X65-72
Vatnsmerki 7. Aðalmerki: Pro patria yfir ljóni með sverði í sigð (VRYHEIT)73-79
Handrit hefur verið blaðmerkt með blýanti.
Eindálka.
Leturflötur er um 145-15087-92
Línufjöldi er 22-35.
Leturflötur er afmarkaður að ofanverðu með striki.
Líklega samtímaband ( 15211520 Skinnheft. Handritið hefur verið tekið úr bandi.
Líklega samtímaband ( 15211520
Skinnheft.
Handritið hefur verið tekið úr bandi.
Samtíningur Guðrún Þórðardóttir; Helgi Árnason; Ólafur Björnsson ...
um 1860-1890.
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Samtíningur
Maríugrátur
Útfararljóð
Um Jón Þórðarson
Draumur
Jóns Jónssonar
Orðskviðir og spakmæli
Illónskvæði
Brúðkaupsvísur
Til Þórðar EinarssonarGuðbjargar Magnúsdóttur
Ýmis kvæði
Þorsteinn ...Helgason
Sjóvíkingurinn
Járnsmíði
Minning
Jón Skúlason
Ljóðabréf
Ljóðabréf til Sigurðar Pálssonar
Gáta
Um forustusauð með klukku í horni.
Draumur Rögnvaldar SigmundssonarÞorsteinn Helgason
Helgi Guðmundsson Magnús Magnússon Halldóra Gísladóttir
Afmælisvísur
Til yngismannsins Þorsteins Helgasonar
Til jómfrú Vigdísar Sæmundsdóttur
Ljóðabréf tilskrifað maddömu Guðrúnu Friðriksdóttur
Samtíngur
Tvö ljóðabréf
Minningakvæði
Um Stefán A. Thorarensen
Ort til Helgu Engilbertsdóttur
Til síra Gísla Gíslasonar
Ljóðabréf fyrir Ásgeir JónssonÞ. Jónssonar
Ljóðabréf til handar G. Vigfússyni
Ljóðabréf til jómfrú Guðrúnar Jónsdóttur
Undir nafni A. ÞórðarsonarS. Sæmundsdóttir
Til Guðmundar Jónssonar
Kveðið 1774.
Vísur
Upphvatning til guðótta og móti fégirni
Tilskrifað Ólöfu Helgadóttur
Eftirmæli
Eftirmæli G. Ólafsson
Bárðarríma
Píslarminning
Sálmur
Minning eftir barn
Grátur Jakobs yfir Rakel
Sjómannavers
Mansöngur
Skipbrotið
Ljóð og ljóðabréf
Íslendingahvöt
Íslendingahvöt, ort þá er lög um stjórnarstöðu Íslands voru valdboðin 1871. Timburmennirnir, brot.
Sálmar
Með nótnasetningu
Um fullgilt dagsverk
Til að syngja í brúðkaupi Jóns og Karólínu
Vísa
Stökur
Vorvísa kveðinn til lítillar stúlku
Leppaljóð
Atlaríma
Draugafrétt
Ungamannskvæði
Eftir meybarn
Eftir Guðnýju
Ortur við byrjun ársins 1878
Heimspekingaskólinn
Reikningur
Til Guðlaugs Helgasonar
Pappír.
Óinnbundið.
Rímna- og kvæðabók Sigfús Jónsson; Sigurður Breiðfjörð; Grímur? ...
1830
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Rímna- og kvæðabók
Rímur af Selikó og Berissu
Rímur af Sóróaster og Selímu
Ljóðabréf til Gísla Konráðssonar
Rauðsvísur
Rímur af Jannesi
Bekraríma
Kvæði af Trýanus og Floradabel
Kvæði og vísur
Kvæði
...Ljóðabréf
Gortaraljóð
Um hellunhnoðra
Úr Klausturpóstinum.
Hákons þáttur Hárekssonar
Heimspekingaskóli
Vísur
Ýmsar mælieiningar
Bændaríma um Fljótsdal 1805
Pödduminning
Látrabréf
Mót Fjölni
Pappír.
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