Siphonic roof drainage system

Hinz Waldvogel,박성규 통역 대한설비공학회 1997 대한설비공학회 강연회 및 기타간행물 Vol.- No.-

1945: The End of the War and Its Aftemath

Hans Martin Hinz 한국박물관학회 2005 博物館學報 Vol.- No.8

May 8, 1945. Late in the evening- in Moscow the 9th of May had already begun in a former Wehrmacht officers’ casino in the Berlin villa section of Karlshorst, representatives of the German armed forces sign the unconditional surrender before the victorious Allied powers. The Second World War in Europe has come to an end. This point in time marked one of d1e most incisive and far - reaching events in German and European histOlY, and above and beyond iliis as well. National Socialist Germany had in the preceding years brought suffering to humanity, with well over 50 million victims of murder or casualties of war, with cities destroyed, landscapes ravaged and people uprooted and exiled evelywhere.

Geophysical Investigations of the Grenville Front in Ohio, USA

선우돈,김정우,Don Sunwoo,Hinze William J.,Kim Jeong Woo The Korean Society of Economic and Environmental G 2005 자원환경지질 Vol.38 No.3

미국 오하이오주에 있는 Grenville Front의 위치와 특성을 이해하기 위하여 중자력, 탄성파 및 지질자료를 이용한 지구물리학적 연구를 수행하였다. 탄성파 자료에 의하면 서부 오하이오에서의 기반암은 Grenville Front와 관계가 있는 동쪽으로 경사를 이루는 반사면으로 나타나고 이에 반하여 동부 오하이오에서는 서쪽으로 경사를 이루는 반사면이 나타난다. 중자력 자료 분석에 의하면 Grenville Front는 저중력 이상으로 그리고 Grenville Front Tectonic Zone은 고중력 및 고자력 이상으로 특징 지워진다. 탄성파 자료를 근거로 수행한 중자력 모델링 결과는 Grenville Front위치에서 하부지각은 두껍고 Grenville Front Tectonic Zone은 주로 변성도가 높은 변성암으로 구성된다는 것을 제안한다. Grenville Front 위치에서 저중력 이상은 두터운 지각 두께 때문에, 반면에 고자력 이상은 변성도가 높은 변성암들의 존재 때문인 것으로 해석된다. Grenville Front 바로 동쪽의 오하이오 중앙부에서 나타나는 고중력 이상은 밀도가 높은 하부 및 중부 지각이 상부지각으로 트러스팅 (thrusting) 되었기 때문이다. 과거 연구에서는 이 고중력 이상이 선캄브리아대의 열 개지역과 관계된다고 하였는데 이를 뒷받침할 만한 근거는 없다. Seismic reflection profile analysis, potential field analysis, and potential field modeling using deep seismic reflection, gravity, magnetic, and geological data were performed to better understand the location and nature of the Grenville Front in Ohio, USA. The seismic reflection profile reveals a broad zone of east dipping basement reflectors associated with the Grenville Front in western Ohio and a broad region of west dipping reflectors cutting through the entire crust in eastern Ohio. Potential field analysis indicates that the Grenville Front is characterized by a gravity low, an associated gravity positive and a magnetic high. The results of the gravity and magnetic modeling using seismic data suggest that the lower crust is thickened at the interpreted position of the Grenville Front and high grade metamorphic rocks make up the Grenville Front Tectonic Zone (GFTZ). The gravity low at the Grenville Front is due to the thickened crust, while the magnetic high is due to high grade metamorphic rocks. The gravity high immediately east of the GFTZ in central Ohio is caused by thrusting of high density lower and middle crustal rocks into the upper crust. There is no compelling evidence that this gravity high is related to a Precambrian rift zone as has been suggested in previous studies.

EARLY-TYPE GALAXIES WITH TIDAL DEBRIS AND THEIR SCALING RELATIONS IN THE<i>SPITZER</i>SURVEY OF STELLAR STRUCTURE IN GALAXIES (S⁴G)

Kim, Taehyun,Sheth, Kartik,Hinz, Joannah L.,Lee, Myung Gyoon,Zaritsky, Dennis,Gadotti, Dimitri A.,Knapen, Johan H.,Schinnerer, Eva,Ho, Luis C.,Laurikainen, Eija,Salo, Heikki,Athanassoula, E.,Bosma, Al IOP Publishing 2012 The Astrophysical journal Vol.753 No.1

<P>Tidal debris around galaxies can yield important clues on their evolution. We have identified tidal debris in 11 early-type galaxies (T <= 0) from a sample of 65 early types drawn from the Spitzer Survey of Stellar Structure in Galaxies (S(4)G). The tidal debris includes features such as shells, ripples, and tidal tails. A variety of techniques, including two-dimensional decomposition of galactic structures, were used to quantify the residual tidal features. The tidal debris contributes similar to 3%-10% to the total 3.6 mu m luminosity of the host galaxy. Structural parameters of the galaxies were estimated using two-dimensional profile fitting. We investigate the locations of galaxies with tidal debris in the fundamental plane and Kormendy relation. We find that galaxies with tidal debris lie within the scatter of early-type galaxies without tidal features. Assuming that the tidal debris is indicative of recent gravitational interaction or merger, this suggests that these galaxies have either undergone minor merging events so that the overall structural properties of the galaxies are not significantly altered, or they have undergone a major merging events but already have experienced sufficient relaxation and phase mixing so that their structural properties become similar to those of the non-interacting early-type galaxies.</P>

미국 오하이오주에 위치하는 그랜빌 프런트의 지구물리학적 연구

선우돈,김정우,William J. Hinze 대한자원환경지질학회 2005 자원환경지질 Vol.38 No.3

Seismic reflection profile analysis, potential field analysis, and potential field modeling using deep seismic reflection, gravity, magnetic, and geological data were performed to better understand the location and nature of the Grenville Front in Ohio, USA. The seismic reflection profile reveals a broad zone of east dipping basement reflectors associated with the Grenville Front in western Ohio and a broad region of west dipping reflectors cutting through the entire crust in eastern Ohio. Potential field analysis indicates that the Grenville Front is characterized by a gravity low, an associated gravity positive and a magnetic high. The results of the gravity and magnetic modeling using seismic data suggest that the lower crust is thickened at the interpreted position of the Grenville Front and high grade metamorphic rocks make up the Grenville Front Tectonic Zone (GFTZ). The gravity low at the Grenville Front is due to the thickened crust, while the magnetic high is due to high grade metamorphic rocks. The gravity high immediately east of the GFTZ in central Ohio is caused by thrusting of high density lower and middle crustal rocks into the upper crust. There is no compelling evidence that this gravity high is related to a Precambrian rift zone as has been suggested in previous studies.

Biomechanical and histological behavior of zirconia implants: an experiment in the rat

Kohal, Ralf J.,Wolkewitz, Martin,Hinze, Marc,Han, Jung-Suk,Bä,chle, Maria,Butz, Frank Blackwell Publishing Ltd 2009 Clinical oral implants research Vol.20 No.4

<P>Abstract</P><P>Objective</P><P>This study aimed at evaluating the integration of zirconia implants in a rat femur model.</P><P>Material and methods</P><P>Zirconia implants with two distinct surface topographies were compared with titanium implants with similar topographies. Titanium and zirconia implants were placed into the femurs of 42 male Sprague–Dawley rats. Four groups of implants were utilized: machined zirconia implants, zirconia implants with a rough surface, machined titanium implants, and titanium implants with an electrochemically roughened surface. After a healing period of 28 days, the load-bearing capacity between the bone and the implant surface was evaluated by a push-in test. Additionally, after a healing period of 14 and 28 days, respectively, bone tissue specimens containing the implants were processed and histologically analyzed.</P><P>Results</P><P>The mean mineralized bone-to-implant contact showed the highest values after 14 and 28 days for the rough surfaces (titanium: 36%/45%; zirconia: 45%/59%). Also, the push-in test showed higher values for the textured implant surfaces, with no statistical significance between titanium (34 N) and zirconia (45.8 N).</P><P>Conclusions</P><P>Within the limits of the animal investigation presented, it was concluded that all tested zirconia and titanium implant surfaces were biocompatible and osseoconductive. The presented surface modification of zirconia implants showed no difference regarding the histological and biomechanical results compared with an established electrochemically modified titanium implant surface.</P>

Nanocomposite Magnetic Materials

Ludwig Schultz,Alberto Bollero,Axel Handstein,Dietrich Hinz,Karl-Hartmut Muller,Golden Kumar,Juergen Eckert,Oliver Gutfleisch,Anke Kirehner Aru Yan The Korean Powder Metallurgy Institute 2002 한국분말재료학회지 (KPMI) Vol.9 No.6

Recent developments in nanocrystalline and nanocomposite rare earth-transition metal magnets are reviewed and emphasis is placed on research work at IFW Dresden. Principal synthesis methods include high energy ball milling, melt spinning, mold casting and hydrogen assisted methods such as reactive milling and hydrogenation-disproportionation-desorption-recombination. These techniques are applied to NdFeB-, PrFeB- and SmCo-type systems with the aim to produce high remanence magnets with high coercivity. Concepts of maximizing the energy density in nanostructured magnets by either inducing a texture via anisotropic HDDR or hot deformation or enhancing the remanence via magnetic exchange coupling are evaluated. With respect to high temperature applications melt spun $Sm(Co_{0.74}Fe_{0.1}Cu_{0.12}Zr_{0.04})_{7.5}$ ribbons were prepared, which showed coercivities of up to 0.53 T at 50$0^{\circ}C$. Partially amorphous $Nd_{60}Fe_xCo_{30-x}Al_{10}(0{\leq}x{\leq}30)$ alloys were prepared by copper mold casting. The effect of transition metal content on the glass-forming ability and the magnetic properties was investigated. The $Nd_{60}Co_{30}Al_{10}$ alloy exhibits an amorphous structure shown by the corresponding diffraction pattern. A small substitution of Co by 2.5 at.% Fe results In the formation of Fe-rich crystallites embedded in the Nd-rich amorphous matrix. The Fe-rich crystallites show hard magnetic behaviour at room temperature with a coercivity value of about 0.4 T, relatively low saturation magnetization and a Curie temperature of 500 K.

Identifying kinase dependency in cancer cells by integrating high-throughput drug screening and kinase inhibition data

Ryall, Karen A.,Shin, Jimin,Yoo, Minjae,Hinz, Trista K.,Kim, Jihye,Kang, Jaewoo,Heasley, Lynn E.,Tan, Aik Choon Oxford University Press 2015 Bioinformatics Vol.31 No.23

<P><B>Motivation:</B> Targeted kinase inhibitors have dramatically improved cancer treatment, but kinase dependency for an individual patient or cancer cell can be challenging to predict. Kinase dependency does not always correspond with gene expression and mutation status. High-throughput drug screens are powerful tools for determining kinase dependency, but drug polypharmacology can make results difficult to interpret.</P><P><B>Results:</B> We developed Kinase Addiction Ranker (KAR), an algorithm that integrates high-throughput drug screening data, comprehensive kinase inhibition data and gene expression profiles to identify kinase dependency in cancer cells. We applied KAR to predict kinase dependency of 21 lung cancer cell lines and 151 leukemia patient samples using published datasets. We experimentally validated KAR predictions of FGFR and MTOR dependence in lung cancer cell line H1581, showing synergistic reduction in proliferation after combining ponatinib and AZD8055.</P><P><B>Availability and implementation:</B> KAR can be downloaded as a Python function or a MATLAB script along with example inputs and outputs at: http://tanlab.ucdenver.edu/KAR/.</P><P><B>Contact:</B> aikchoon.tan@ucdenver.edu</P><P><B>Supplementary information:</B> Supplementary data are available at <I>Bioinformatics</I> online.</P>

미국 오하이오주에 위치하는 그랜빌 프런트의 지구물리학적 연구

선우돈(Don Sunwoo),William J. Hinze,김정우(Jeong Woo Kim) 대한자원환경지질학회 2005 자원환경지질 Vol.38 No.3

미국 오하이오주에 있는 Grenville Front의 위치와 특성을 이해하기 위하여 중자력, 탄성파 및 지질자료를 이용한 지구물리학적 연구를 수행하였다. 탄성파 자료에 의하면 서부 오하이오에서의 기반암은 Grenville Front와 관계가 있는 동쪽으로 경사를 이루는 반사면으로 나타나고 이에 반하여 동부 오하이오에서는 서쪽으로 경사를 이루는 반사면이 나타난 다. 중자력 자료 분석에 의하면 Grenville Front는 저중력 이상으로 그리고 Grenville Front Tectonic Zone은 고중력 및고자력 이상으로 특징 지워진다. 탄성파 자료를 근거로 수행한 중자력 모델링 결과는 Grenville Front 위치에서 하부지각은 두껍고 Grenville Front Tectonic Zone은 주로 변성도가 높은 변성암으로 구성된다는 것을 제안한다. Grenville Front 위치에서 저중력 이상은 두터운 지각 두께 때문에, 반면에 고자력 이상은 변성도가 높은 변성암들의 존재 때문인 것으로 해석된다. Grenville Front 바로 동쪽의 오하이오 중앙부에서 나타나는 고중력 이상은 밀도가 높은 하부 및 중부 지각이 상부지각으로 트러스팅 (thrusting) 되었기 때문이다. 과거 연구에서는 이 고중력 이상이 선캄브리아대의 열개지역과 관계된다고 하였는데 이를 뒷받침할 만한 근거는 없다. Seismic reflection profile analysis, potential field analysis, and potential field modeling using deep seismic reflection, gravity, magnetic, and geological data were performed to better understand the location and nature of the Grenville Front in Ohio, USA. The seismic reflection profile reveals a broad zone of east dipping basement reflectors associated with the Grenville Front in western Ohio and a broad region of west dipping reflectors cutting through the entire crust in eastern Ohio. Potential field analysis indicates that the Grenville Front is characterized by a gravity low, an associated gravity positive and a magnetic high. The results of the gravity and magnetic modeling using seismic data suggest that the lower crust is thickened at the interpreted position of the Grenville Front and high grade metamorphic rocks make up the Grenville Front Tectonic Zone (GFTZ). The gravity low at the Grenville Front is due to the thickened crust, while the magnetic high is due to high grade metamorphic rocks. The gravity high immediately east of the GFTZ in central Ohio is caused by thrusting of high density lower and middle crustal rocks into the upper crust. There is no compelling evidence that this gravity high is related to a Precambrian rift zone as has been suggested in previous studies.

Association between pathological response in metastasis and long-term survival after preoperative chemotherapy and conversion surgery for metastatic pancreatic cancer

Thomas HANK,Ulla KLAIBER,Ulf HINZ,Denise SCHUETTE,Carl-Stephan LEONHARDT,Frank BERGMANN,Thilo HACKERT,Dirk JAEGER,Markus BUECHLER,Oliver STROBEL 한국간담췌외과학회 2022 Annals of hepato-biliary-pancreatic surgery Vol.26 No.-