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Conditional Optimization of Solution Combustion Synthesis for Pioneered La2O3 Nanostructures to Application as Future CMOS and NVMS Generations

机译:先锋La 2 O 3 纳米结构溶液燃烧合成的条件优化,可应用于未来的CMOS和NVMS世代

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In the Mediterranean region, climate change will result by 2100 in a tempera-ture increase that most likely will range from 2°C to 2.7°C, while annual precip-itation will most likely reduce in the range of 3% to 10%. This paper uses hy-drological modeling of precipitation and evapotranspiration to evaluate the challenge to aquifer natural recharge considering Palestine as a case study. The study showed that the climate change impacts on aquifer recharge will vary according to the distributions of monthly precipitation and evapotranspiration in the recharge areas. The 2°C to 3°C increase in temperature could result in a reduction of 6% to 13% in aquifer annual recharge. Aquifer recharge was found to be sensitive to changes in precipitation as a reduction of 3% to 10% in annual precipitation could result in a reduction in annual recharge ranging from 3% to 25%. It was observed that aquifers with recharge areas characterized by lower precipitation are more sensitive to precipitation reduction and thus groundwater resources will be negatively impacted more in these areas by climate change. Thus, climate change will reduce water availability in drier areas requiring adaptation measures through improving water management and rehabilitation of water infrastructure.
机译:在地中海地区,到2100年,气候变化将导致温度升高,最有可能在2°C至2.7°C范围内,而每年的降水量最有可能在3%至10%的范围内降低。本文以巴勒斯坦为例,利用降水和蒸散的水文模型来评估对含水层自然补给的挑战。研究表明,气候变化对含水层补给的影响将根据补给区每月降水量和蒸散量的分布而变化。温度升高2°C至3°C可能导致含水层年补给量降低6%至13%。发现含水层补给对降水变化敏感,因为年降水量减少3%至10%可能导致年补给量减少3%至25%。据观察,补给区以降水量较低为特征的含水层对降水减少更为敏感,因此这些地区的地下水资源将受到气候变化的负面影响更大。因此,气候变化将通过改善水管理和水基础设施的恢复而减少需要采取适应措施的较干燥地区的水供应。

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