科学素养与现象阐释·英语30篇（8）
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How Plate Tectonics Shapes Long-Term Climate Through Silicate Weathering and Carbon Sequestration
板块构造如何通过硅酸盐风化与碳封存塑造长期气候
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Mountain building from continental collisions exposes fresh silicate rock to atmospheric CO₂ and rainfall, initiating chemical weathering that draws down greenhouse gases over millions of years.大陆碰撞造山使新鲜硅酸盐岩石暴露于大气CO₂和降雨中，启动化学风化作用，从而在数百万年间减少温室气体。
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The reaction converts CO₂ into bicarbonate ions, which rivers carry to oceans where marine organisms precipitate carbonate shells—locking carbon into sediments.该反应将CO₂转化为碳酸氢根离子，由河流带入海洋，被海洋生物用于沉淀碳酸盐外壳，将碳封存于沉积物中。
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This slow carbon cycle acts as Earth’s geological thermostat, counteracting volcanic CO₂ emissions and stabilizing surface temperatures across geologic time.这一缓慢碳循环充当地球的地质恒温器，在地质时间尺度上抵消火山CO₂排放，稳定地表温度。
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The uplift of the Himalayas and Andes since the Miocene accelerated weathering rates, contributing to global cooling and Pleistocene glaciation cycles.自中新世以来喜马拉雅山脉与安第斯山脉隆升加速了风化速率，推动全球变冷及更新世冰期旋回。
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Modern geoengineering proposals mimic this process via enhanced rock weathering—but face scalability limits due to energy-intensive grinding and transport logistics.当前地球工程方案通过增强岩石风化模拟此过程，但受限于研磨与运输所需的高能耗，难以大规模推广。
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Soil microbiologists now quantify microbial mediation of silicate dissolution, revealing that biological activity can double weathering rates in tropical forests.土壤微生物学家正量化微生物对硅酸盐溶解的调控作用，发现热带森林中生物活动可使风化速率翻倍。
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Carbon accounting standards are beginning to include 'geological sequestration potential' when assessing land-use change impacts on national inventories.碳核算标准开始将‘地质固碳潜力’纳入土地利用变化影响评估，用于国家碳排放清单编制。
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Paleoclimatologists use lithium isotope ratios in marine sediments to reconstruct past weathering fluxes—linking tectonic history to climate proxies.古气候学家利用海洋沉积物中锂同位素比值重建历史风化通量，建立构造演化与气候代用指标的联系。
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Urban infrastructure planning considers bedrock composition, as weathering-prone lithologies affect foundation stability and long-term drainage chemistry.城市基础设施规划需考虑基岩成分，因易风化岩性会影响地基稳定性及长期排水水质。
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The timescale mismatch—tectonic processes operate over 10⁶ years, while anthropogenic emissions peak over 10²—highlights why mitigation cannot rely on natural sinks alone.时间尺度错配——构造过程历时百万年，而人为排放峰值仅百年左右——凸显单靠自然碳汇无法实现减排目标。
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Interdisciplinary courses integrate geophysics, biogeochemistry, and climate modeling to show how crustal deformation ultimately regulates biosphere habitability.跨学科课程融合地球物理学、生物地球化学与气候建模，阐明地壳形变如何最终调控生物圈宜居性。
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This perspective shifts climate discourse from short-term emissions control to multi-millennial stewardship of Earth system feedbacks.这一视角推动气候讨论从短期减排转向对地球系统反馈机制的千年尺度 stewardship（守护）