Deze layer definition is automatisch gegenereerd, gebaseerd op de volgende metadata (provincie Zuid-Holland).

          SamenvattingOp basis van laseraltimetrie gegenereerd hoogtegrid met een resolutie van 0.5 meter. Het geïnterpoleerde hoogtegrid is d.m.v. interpolatie van de gefilterde laserpunten (die punten die op maaiveld liggen) ontstaan en beschrijft het maaiveld. In het geïnterpoleerde grid zijn in tegenstelling tot het niet geïnterpoleerde grid incidentele cellen met nodata value met een waarde gevuld via interpolatie van de waarden van tenminste 6 buurcellen.Het AHN-2 is de opvolger van het bestaande Actueel Hoogtebestand Nederland 1. Het kenmerkt zich daar een hogere puntdichtheid bij inwinning waardoor naast een 5 meter grid ook 3 verschillende 0.5 meter grids zijn vervaardigd. In tegenstellnig tot AHN-1 bevat het 0.5 meter grid AHN-2 hoogte-waarden in meters i.p.v. centimeters. Het AHN-2 wordt gefaseerd tot/met 2012 ingewonnen.

          Dataset gepubliceerd: 2009-01-01

          Update frequentie: Niet gepland
          Downloads, views en links
          Bezoek de metadata-pagina voor de kaartlaag- en dataset services.
          Open metadata 

          Algemene beschrijving herkomstDoor middel van het FLI-MAP systeem ingewonnen LiDAR puntenwolk, gefilterd in een iteratief filterproces tot een puntenwolk voor het maaiveldniveau, welke vergrid is tot ADF hoogtegrids.

Deze layer definition is automatisch gegenereerd, gebaseerd op de volgende metadata (provincie Zuid-Holland).

          SamenvattingOp basis van laseraltimetrie gegenereerd hoogtegrid met een resolutie van 0.5 meter. Het geïnterpoleerde hoogtegrid is d.m.v. interpolatie van de gefilterde laserpunten (die punten die op maaiveld liggen) ontstaan en beschrijft het maaiveld. In het geïnterpoleerde grid zijn in tegenstelling tot het niet geïnterpoleerde grid incidentele cellen met nodata value met een waarde gevuld via interpolatie van de waarden van tenminste 6 buurcellen.Het AHN-2 is de opvolger van het bestaande Actueel Hoogtebestand Nederland 1. Het kenmerkt zich daar een hogere puntdichtheid bij inwinning waardoor naast een 5 meter grid ook 3 verschillende 0.5 meter grids zijn vervaardigd. In tegenstellnig tot AHN-1 bevat het 0.5 meter grid AHN-2 hoogte-waarden in meters i.p.v. centimeters. Het AHN-2 wordt gefaseerd tot/met 2012 ingewonnen.

          Dataset gepubliceerd: 2009-01-01

          Update frequentie: Niet gepland
          Downloads, views en links
          Bezoek de metadata-pagina voor de kaartlaag- en dataset services.
          Open metadata 

          Algemene beschrijving herkomstDoor middel van het FLI-MAP systeem ingewonnen LiDAR puntenwolk, gefilterd in een iteratief filterproces tot een puntenwolk voor het maaiveldniveau, welke vergrid is tot ADF hoogtegrids.

Differential cross section DSIG/DT for photon energy 2.07 to 2.17 GeV.

Deze layer definition is automatisch gegenereerd, gebaseerd op de volgende metadata (provincie Zuid-Holland).

          SamenvattingOp basis van laseraltimetrie gegenereerd hoogtegrid met een resolutie van 0.5 meter. Het geïnterpoleerde hoogtegrid is d.m.v. interpolatie van de gefilterde laserpunten (die punten die op maaiveld liggen) ontstaan en beschrijft het maaiveld. In het geïnterpoleerde grid zijn in tegenstelling tot het niet geïnterpoleerde grid incidentele cellen met nodata value met een waarde gevuld via interpolatie van de waarden van tenminste 6 buurcellen.Het AHN-2 is de opvolger van het bestaande Actueel Hoogtebestand Nederland 1. Het kenmerkt zich daar een hogere puntdichtheid bij inwinning waardoor naast een 5 meter grid ook 3 verschillende 0.5 meter grids zijn vervaardigd. In tegenstellnig tot AHN-1 bevat het 0.5 meter grid AHN-2 hoogte-waarden in meters i.p.v. centimeters. Het AHN-2 wordt gefaseerd tot/met 2012 ingewonnen.

          Dataset gepubliceerd: 2009-01-01

          Update frequentie: Niet gepland
          Downloads, views en links
          Bezoek de metadata-pagina voor de kaartlaag- en dataset services.
          Open metadata 

          Algemene beschrijving herkomstDoor middel van het FLI-MAP systeem ingewonnen LiDAR puntenwolk, gefilterd in een iteratief filterproces tot een puntenwolk voor het maaiveldniveau, welke vergrid is tot ADF hoogtegrids.

This dataset contains the digitized treatments in Plazi based on the original journal article Lee, Seung-Gyu, Ahn, Kee-Jeong (2014): Two new combinations and a key to the species of the genus Earota Mulsant & Rey (Coleoptera: Staphylinidae: Aleocharinae). Zootaxa 3765 (2): 187-193, DOI: 10.11646/zootaxa.3765.2.6

Fat and protein supplementations used in this study, related to Fig 6.

Micrographs of U20S 2-6-3 (lac array cells) analyzed for partitioning of cofactors or reporter activation by NUP98 IDR, FtoA mutant, or control (CFP-LacI without fusion).

AHN DEM là một DEM 0,5 m bao phủ Hà Lan. Dữ liệu này được tạo từ dữ liệu LIDAR thu thập vào mùa xuân trong khoảng thời gian từ năm 2007 đến năm 2012. Phiên bản này chứa cả mẫu ở cấp độ mặt đất và các mục ở trên cấp độ mặt đất (chẳng hạn như toà nhà, cầu, cây cối, v.v.). Đám mây điểm được chuyển đổi thành lưới 0,5 m bằng phương pháp trọng số nghịch đảo bình phương khoảng cách.

This dataset contains the concentrations of 34 elements, chloride, methane, ammonium, and dissolved inorganic carbon, as well as δ2H, δ18O, δ7Li, δ34S, 87Sr/86Sr and δ13C-DIC in groundwater and seawater samples as well as in sediment porewater samples from pockmarks associated with submarine groundwater discharge (SGD) at the Hanko cape in Finland, northern Baltic Sea. The groundwater samples were collected onshore from an observation well using a suction pump and from a water intake well. The seawater and pockmark porewater samples were collected from the research vessel Geomari of the Geological Survey of Finland (GTK). The seawater samples were collected onboard from 2 m, 6 m, and 10 m below sea surface at the pockmark locations using a Limnos water sampler. The porewater samples were extracted using Rhizons at 1-2 cm vertical intervals from sediment cores that were collected from the pockmarks at 11 m water depth. Multielement composition of the seawater, groundwater and porewater samples were analyzed using inductively coupled plasma optical emission and mass spectrometry (ICP-OES and ICP-MS). Ca, Fe, K, Mg, Mn, Na, and S were analysed by ICP-OES, whereas Ag, Al, As, B, Ba, Be, Bi, Cd, Co, Cr, Cu, I, Li, Mn, Mo, Ni, P, Pb, Rb, Sb, Se, Sr, Th, Tl, U, V, and Zn were analysed by ICP-MS. Major anions (Br, Cl, F, NO3 and SO4) were analyzed using ion chromatography. Alkalinity (as HCO3-), electrical conductivity, pH and KMnO4 consumption of the unfiltered and unpreserved groundwater samples were measured immediately upon arrival at the laboratory. Methane concentrations in the seawater, groundwater and porewater samples were determined by gas chromatography with flame ionization detector. Headspace CH4 concentrations were converted to total dissolved phase concentrations in the original porewater sample using Henry's Law. δ13CDIC values were determined by means of continuous-flow isotope-ratio-monitoring mass spectrometry (CF-irmMS). The concentrations of NH4+ and PO4 were analyzed spectrophotometrically. Hydrogen and oxygen isotope ratios of the groundwater, seawater and porewater samples were analyzed by cavity ring down spectroscopy (CRDS). The isotope ratios are reported as deviation from the international VSMOW-standard. The uncertainty (2σ) of measurement is <0.1‰ for oxygen analysis and <0.3‰ for hydrogen analysis. For the determination of δ7Li, δ34S and 87Sr/86Sr, the elements were eluted from the groundwater, seawater and porewater samples by liquid column chromatography. The isotope ratios in the eluted samples were analyzed by multi-collector ICP-MS. The Li, S and Sr isotope ratios are reported against the LSVEC, NBS987 and CDT reference materials, respectively. The standard mean deviations of Li and S isotope determinations are +/- 0.32 and +/- 0.52 ‰, respectively. The mean 2SE of Sr isotope determinations is +/- 0.000015. In the dataset, The given ‰ values are equivalent to mUr (milli Urey)

Actueel Hoogtebestand Nederland (AHN) là một tập dữ liệu có dữ liệu độ cao chi tiết và chính xác cho toàn bộ Hà Lan. Thông tin về độ cao được thu thập từ máy bay trực thăng và máy bay bằng công nghệ laser với độ chính xác theo phương thẳng đứng là 5 cm. Tập dữ liệu AHN3 chứa các biến DSM và DTM 0,5 m của AHN tại Hà Lan. Dữ liệu …

AHN DEM là một DEM 0,5 m bao phủ Hà Lan. Dữ liệu này được tạo từ dữ liệu LIDAR thu thập vào mùa xuân trong khoảng thời gian từ năm 2007 đến năm 2012. Nó chứa các mẫu ở cấp độ mặt đất và tất cả các mục khác trên mặt đất (chẳng hạn như các toà nhà, cầu, cây cối, v.v.) đều bị xoá. Phiên bản này không được nội suy; các vùng đã xoá đối tượng sẽ bị bỏ trống và không được điền bằng các giá trị nội suy. Đám mây điểm được chuyển đổi thành lưới 0,5 m bằng phương pháp trọng số nghịch đảo bình phương khoảng cách.

AHN DEM là một DEM 0,5 m bao phủ Hà Lan. Dữ liệu này được tạo từ dữ liệu LIDAR thu thập vào mùa xuân trong khoảng thời gian từ năm 2007 đến năm 2012. Nó chứa các mẫu ở cấp độ mặt đất và tất cả các mục khác trên mặt đất (chẳng hạn như các toà nhà, cầu, cây cối, v.v.) đều bị xoá. Phiên bản này được nội suy; các vùng mà đối tượng đã bị xoá sẽ được điền bằng các giá trị nội suy. Đám mây điểm được chuyển đổi thành lưới 0,5 m bằng phương pháp trọng số khoảng cách nghịch đảo bình phương. Lưu ý: Tập dữ liệu này không bao gồm một số ít ô được liệt kê trong tệp kê khai chỉ có ở độ phân giải thấp hơn.

sunovivid/sd2.1_coco dataset hosted on Hugging Face and contributed by the HF Datasets community

sunovivid/sit-latents-3.0 dataset hosted on Hugging Face and contributed by the HF Datasets community

sunovivid/sd2.1_coco-aes-scores dataset hosted on Hugging Face and contributed by the HF Datasets community

Crystallization and glycan soaking conditions for S. Typhi PltB homopentamer.

Summary of the six horse groups.

SHIRPA of 5 week-old F2 mice fed with normal and malnourished isocaloric diets, related to Fig 2 (n = 6).

PurposeTo analyze and compare the survival rates of recurrent breast cancer patients in Korea between two periods (period I: 2000–2007; period II: 2008–2013) and to identify the factors associated with outcomes and changes over time in the duration of survival after recurrence.MethodsWe retrospectively analyzed 2,407 patients who had recurrent breast cancer with treated between January 2000 and December 2013 and divided them into two periods according to the year of recurrence. We reviewed the age at diagnosis, clinical manifestations, pathology report, surgical methods, types of adjuvant treatment, type of recurrence, and follow-up period.ResultsThe median follow-up was 30.6 months (range, 0–223.4) from the time of relapse, and the median survival time was 42.3 months. Survival after recurrence (SAR) significantly improved from 38.0 months in period I to 49.7 months in period II (p < 0.001). In the analysis performed according to the hormone receptor and HER2 status subtypes, all subtypes except the triple-negative subtype showed higher SAR in period II than period I. Age at diagnosis, tumor stage, and treatment after recurrence were significantly correlated with survival outcomes.ConclusionThe survival outcomes of Korean patients with breast cancer after the first recurrence have improved in Korea. Such improvements may be attributed to advances in treatment.

Number of districts, district hospitals and schools by province.