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

Amanullakhan Pathan, Kavita Desai, Shailesh Vajapara, C. P. Bhasin
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引用次数: 10

Abstract

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.
溶液燃烧合成La2O3纳米结构的条件优化,以应用于未来的CMOS和NVMS
在地中海地区,到2100年,气候变化将导致气温上升,最有可能在2°C至2.7°C之间,而年降水量最有可能减少3%至10%。本文以巴勒斯坦为例,利用降水和蒸散的水文建模来评估含水层自然补给面临的挑战。研究表明,气候变化对含水层补给的影响会随着补给区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减少6%至13%。含水层补给对降水量的变化很敏感,因为年降水量减少3%至10%可能导致年补给量减少3%到25%。据观察,补给区降水量较低的含水层对降水减少更敏感,因此这些地区的地下水资源将受到气候变化的更大负面影响。因此,气候变化将减少干旱地区的水供应,需要通过改善水管理和恢复水基础设施来采取适应措施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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