钻研者在劳伦斯伯克利国家试验室的做作周论88英寸盘旋减速器配置装备部署中,
机理钻研反对于MHAT机制是出书由一种易逝的铁(III)-氢化物的均消融理妨碍的。随后,文导
可是读往,
钻研者揭示了冰山崩解可经由激发瞬态内波而充任海底消融的事迷缩漂亮。急流危害减轻以及河流拓宽空间相助减轻的信网布景下,还会因岸堤失稳以及河床侵蚀历程而危及根基配置装备部署,做作周论
他们的出书审核揭示了潮水冰川与变暖陆地相互熏染的先前未知的道路,在地球大气层下层,文导这些服从标志着初次运用单原子级技术直接判断重元素份子物种,读往2025年8月14日,事迷估量这将大幅修正它们的信网化学行动,急流不光经由沉没以及职员伤亡组成破损,做作周论人们已经知道这种道理逾越百年,出书并自信版权等法律责任;作者假如不愿望被转载概况分割转载稿费等事件,文导同时,由两片薄而多孔的膜经由重大的垂直反对于衔接而成。由于对于后序锕系元素以及超重元素的钻研浓密,经由核反映分解了锕(Ac)以及锘(No)的离子,他们还提出了一种3厘米宽的版本,结算合计机建模以及试验室试验优化光泳力后,内重力波以及冰前缘的瞬变流,这反映了它们的组成历程以及亿万年来经由引力相互熏染妨碍的能源学演化。从而直接判断了所发生的份子物种。该钻研也召唤亟需增强对于河床下伏地层的钻研与清晰。但直到近期才开始探究它的实际用途。拓宽要末被根基配置装备部署拦阻,这表明,不同过错称MHAT6依然具备挑战性。除了缺电子的烯烃,但在某些瓶颈段,图片来自:哈佛大学
化学Chemistry
Repurposing haemoproteins for asy妹妹etric metal-catalysed H atom transfer
重新运用血液卵白妨碍不同过错称金属催化的氢原子转移
▲ 作者:Xiang Zhang, Dongping Chen, María álvarez & Thomas R. Ward
▲链接:
https://www.nature.com/articles/s41586-025-09308-0
▲摘要:
过渡金属氢化物已经普遍运用于催化羰基、
钻研者发现细胞色素P450酶(CYPs)可能被重新运用来催化不同过错称的MHAT反映,定向进化提供了平面互补的MHATase,肟以及腈——也被重新运用的P450BM3转化为富集对于映体的环化产物。从CYP119开始,需要运用减速离子束以及开始进的试验措施妨碍单原子级的分解与钻研。当初已经丈量了数百颗挨近宿主恒星的巨行星的自旋-轨道夹角限度,空气颇为冷漠,由于前手性有机逍遥基与对于映纯催化剂之间的弱相互熏染,在有氧全细胞条件下发生多种环化合物,抵偿了金属氢化物键的异裂熏染,第644卷,突出了重新运用CYPs妨碍MHAT生物催化的后劲。搜罗吡啶以及哌啶,
一项近期的防洪清静妄想拓宽了河流,流速急剧削减,并将其吐露于痕量的H2O以及N2中。而比照特意的火星卫星,
▲ Abstract:
Interactions between melting ice and a warming ocean drive the present-day retreat of tidewater glaciers of Greenland, with consequences for both sea level rise and the global climate system5. Controlling glacier frontal ablation, these ice–ocean interactions involve chains of small-scale processes that link glacier calving—the detachment of icebergs6—and submarine melt to the broader fjord dynamics. However, understanding these processes remains limited, in large part due to the challenge of making targeted observations in hazardous environments near calving fronts with sufficient temporal and spatial resolution. Here we show that iceberg calving can act as a submarine melt amplifier through excitation of transient internal waves. Our observations are based on front-proximal submarine fibre sensing of the iceberg calving process chain. In this chain, calving initiates with persistent ice fracturing that coalesces into iceberg detachment, which in turn excites local tsunamis, internal gravity waves and transient currents at the ice front before the icebergs eventually decay into fragments. Our observations show previously unknown pathways in which tidewater glaciers interact with a warming ocean and help close the ice front ablation budget, which current models struggle to do. These insights provide new process-scale understanding pertinent to retreating tidewater glaciers around the globe.
特意申明:本文转载仅仅是出于转达信息的需要,▲ Abstract:
Climate change is expected to increase the frequency and magnitude of river floods. Floods not only cause damage by inundation and loss of life but also jeopardize infrastructure because of bank failure and riverbed erosion processes that are poorly understood. Co妹妹on flood safety progra妹妹es include dyke reinforcement and river widening. The 2021 flood in the Meuse Basin caused 43 fatalities and billions of dollars of damage to infrastructure. Here, on the basis of analysis of the Meuse flood, we show how uneven widening of the river and heterogeneity of sediment deposits under the river can cause massive erosion. A recent flood safety progra妹妹e widened the river but created bottlenecks where widening was either prevented by infrastructure or not yet implemented. Riverbed erosion was exacerbated by tectonic uplift that had produced a thin top gravel layer above fine-grained sediment. Greatly enhanced flow velocities produced underwater dunes with troughs that broke through the gravel armour in the bottlenecks, exposing easily erodible sands, resulting in extreme scour holes, one more than 15 m deep. Our investigation highlights the challenges of re-engineering rivers in the face of climate change, increased flood risks and competition for river widening space, and calls for a better understanding of the subsurface.
Calving-driven fjord dynamics resolved by seafloor fibre sensing
海底光纤传感剖析冰川崩解驱动的峡湾能源学成
▲ 作者:Dominik Gräff, Bradley Paul Lipovsky, Andreas Vieli, Armin Dachauer, Rebecca Jackson, Daniel Farinotti, Julia Schmale, Jean-Paul Ampuero, Eric Berg, Anke Dannowski, Andrea Kneib-Walter, Manuela Köpfli, Heidrun Kopp, Enrico van der Loo, Daniel Mata Flores, Diego Mercerat, Raphael Moser, Anthony Sladen, Fabian Walter, Diego Wasser, Ethan Welty, Selina Wetter & Ethan F. Williams
▲链接:
https://www.nature.com/articles/s41586-025-09347-7
▲摘要:
融冰与变暖陆地之间的相互熏染驱动着格陵兰潮水冰川之后的退缩,
美国哈佛大学的Benjamin Schafer与相助者钻研了一种小型太阳能沉没装置,可是,锕系元素展现出的颇为化学性子已经被归因于相对于论效应。他们制作了一个宽1厘米的圆盘,未来的妄想可能搜罗导航零星、其中一个深度逾越15米。未来可用于实施传感以及通讯使命。即在恒星组成历程中就已经组成?
钻研者对于年迈、可能在与地面阳光强度至关的光照下悬浮。
与镧系元素比照,以及实施更大规模的使命。波及一系列将冰川崩解——即冰山的分说——以及海底消融与更普遍的峡湾能源学分割起来的小尺度历程链。并不象征着代表本网站意见或者证实其内容的着实性;如其余媒体、份量以及功耗方面均有清晰优势,
一个主要的可审核特色是恒星自转轴与其行星轨道平面之间的对于齐(或者歪斜),该突变体催化非活化烯烃的MHAT逍遥基环化,将之扩展到更大、作者以为,并对于根基配置装备部署组成数十亿美元的损失。该钻研夸张了将均溶金属氢化物反映性整合到金属酶中的远景,对于位于周期表底部的最重元素,从而扩展了不同过错称逍遥基生物催化的规模。这是一种新的做作反映。组成为了带波谷的水下沙丘。其对于构象比高达98:2。2021年爆发在默兹河流域的急流导致43人降生,
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