概括
海洋中的富含的铁地是,和等战略性金属的潜在资源. 它们位于国家经济区内的位置,与深结节相比,简化了恢复.
科学领域:
- 海洋地质学 海洋地质学
- 矿产资源 矿产资源是指矿产资源.
- 地质化学 地质化学
背景情况:
- 开放海洋中的铁氧化物比其他广泛分布的沉积物或岩石具有更高的丰富度.
- 在海底山脉和海洋山脊上的铁地中,的度可能超过1%.
- 这些地是形成速度最慢的地球材料之一,每1到3个月增长1个分子层.
研究的目的:
- 突出铁甲皮作为战略金属的潜在资源.
- 为了比较铁地的可访问性与深海结节的资源开发.
- 了解地开发环境影响报告的持续发展情况.
主要方法:
- 铁氧化物组成的分析.
- 海底山脉和海洋山脊的地质调查.
- 评估地的生长速度.
- 评估资源位置相对于经济区的位置.
主要成果:
- 铁甲皮显著富含.
- ,和是这些地的关键组成部分,被确定为优先战略金属.
- 富含的地存在于国家专属经济区内,与位于国际水域的深结节不同.
结论:
- 铁甲皮是关键金属的可行的国内资源.
- 由于它们的位置,利用这些地比深结提供了优势.
- 环境影响评估对于负责任的地采矿至关重要,目前正在开发中.
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