烧结终点(Burning Through Point-简称BTP)是指烧结原料经过点火后,在机床上恰好完全进行物理和化学反应的那一点,即烧结结束时的位置。烧结终点是影响烧结质量和产量的重要因素,控制好烧结终点位置具有重要的意义。本文在参考已有研究...烧结终点(Burning Through Point-简称BTP)是指烧结原料经过点火后,在机床上恰好完全进行物理和化学反应的那一点,即烧结结束时的位置。烧结终点是影响烧结质量和产量的重要因素,控制好烧结终点位置具有重要的意义。本文在参考已有研究文献的基础上,给出了烧结终点位计算的算法。展开更多
烧结终点（Burning Through Point-简称BTP）是指烧结原料经过点火后,在机床上恰好完全进行物理和化学反应的那一点,即烧结结束时的位置。烧结终点是影响烧结质量和产量的重要因素,控制好烧结终点位置具有重要的意义。通过研究开发并参...烧结终点（Burning Through Point-简称BTP）是指烧结原料经过点火后,在机床上恰好完全进行物理和化学反应的那一点,即烧结结束时的位置。烧结终点是影响烧结质量和产量的重要因素,控制好烧结终点位置具有重要的意义。通过研究开发并参考已有研究文献,给出了烧结终点位计算的算法。展开更多
Petermann Glacier is a marine-terminating outlet glacier that had a 70 km-long floating ice tongue prior to a～270 km2calving event that was observed from satellite sensors in August 2010,shortening the ice tongue by...Petermann Glacier is a marine-terminating outlet glacier that had a 70 km-long floating ice tongue prior to a～270 km2calving event that was observed from satellite sensors in August 2010,shortening the ice tongue by～27 km.Further,in July 2012,another 10 km was lost through calving.In order to understand these events in perspective,here the authors perform a long-term data analysis of Petermann Glacier calving-front variability and ice velocity for each year in the 1990s–2000s,supplemented by available observations from the previous three decades.Five major(on the order of 100 km2)calving events are identified,with～153 km2calved from1959 to 1961,～168 km2in 1991,～71 km2in 2001,～270 km2in 2010,and～130 km2in 2012—as well as～31km2calved in 2008.The increased frequency of major calving events in recent years has left the front terminus position retreated nearly 25 km beyond the range of observed in previous decades.In contrast,stable ice-dynamics are suggested from ice-velocity measurements made each year between 1993–2012,which are on average1063 m yr–1,with limited interannual variability and no significant trend;moreover,there is no apparent relationship between ice-velocity variability and calving events.The degree to which the massive calving events in 2010and 2012 represent natural episodic variability or a response to atmospheric and/or oceanic changes remains speculative;however,melt-induced weakening of the floating ice tongue in recent years is strongly suggested.展开更多
基金supported by the Trond Mohn Donation to the Mohn-Sverdrup Center at the Nansen Center,the Research Council of Norway’s UK/Netherlands/Norway RAPID programthe project AWAKE under the Polish-Norwegian Research Fund(2009–2011)
文摘Petermann Glacier is a marine-terminating outlet glacier that had a 70 km-long floating ice tongue prior to a～270 km2calving event that was observed from satellite sensors in August 2010,shortening the ice tongue by～27 km.Further,in July 2012,another 10 km was lost through calving.In order to understand these events in perspective,here the authors perform a long-term data analysis of Petermann Glacier calving-front variability and ice velocity for each year in the 1990s–2000s,supplemented by available observations from the previous three decades.Five major(on the order of 100 km2)calving events are identified,with～153 km2calved from1959 to 1961,～168 km2in 1991,～71 km2in 2001,～270 km2in 2010,and～130 km2in 2012—as well as～31km2calved in 2008.The increased frequency of major calving events in recent years has left the front terminus position retreated nearly 25 km beyond the range of observed in previous decades.In contrast,stable ice-dynamics are suggested from ice-velocity measurements made each year between 1993–2012,which are on average1063 m yr–1,with limited interannual variability and no significant trend;moreover,there is no apparent relationship between ice-velocity variability and calving events.The degree to which the massive calving events in 2010and 2012 represent natural episodic variability or a response to atmospheric and/or oceanic changes remains speculative;however,melt-induced weakening of the floating ice tongue in recent years is strongly suggested.
