成功施肥的适宜位置和配置方法

Tai-jin Kim
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The iron (Fe) replete compounds, consisting of natural clay, \nvolcanic ash, agar, N2-fixing mucilaginous cyanobacteria, carbon \nblack, biodegradable plastic foamed polylactic acid, fine wood chip, and \niron-reducing marine bacterium, are deployed in the ocean to stay within a \nsurface depth of 100 m for phytoplankton digestion. The deployment method of Fe-replete \ncomposite with a duration of at least several years for the successful iron \nfertilization, is configured to be on the streamline of the Antarctic \nCircumpolar Current (ACC). This will result in high momentum flux for its \nefficient dispersion on the ocean surface where diatom, copepods, krill and \nhumpback whale stay together (~100 m). \nHumpback whales are proposed as a biomarker for the successful iron \nfertilization in large-scale since humpback whales feed on krill, which in turn \nfeed on cockpods and diatoms. 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引用次数: 2

摘要

“高营养、低叶绿素(HNLC)”区域是通过将铁与周围海洋火山喷发产生的硫化氢锁定在沉积的硫化铁中而形成的。在远离火山、地震和构造板块边界的地方施用铁肥,以减少火山硫化合物锁铁的机会。由于南乔治亚州的沙格岩和南大洋德雷克海峡的布兰斯菲尔德海峡的动量通量高,可以有效地部署铁,因此建议在这些地方进行大规模的铁施肥。由天然粘土、火山灰、琼脂、固氮黏液蓝藻、炭黑、可生物降解的塑料泡沫聚乳酸、细木屑和铁还原海洋细菌组成的含铁(Fe)化合物被部署在海洋中,停留在100米的表面深度内供浮游植物消化。在南极环极流(ACC)流线上配置充铁复合材料的部署方法,成功的铁施肥持续时间至少为几年。当硅藻、桡足类、磷虾和座头鲸聚集在一起(约100米)时,这将导致高动量通量,使其在海洋表面有效扩散。座头鲸被认为是大规模铁受精成功的生物标志物,因为座头鲸以磷虾为食,磷虾又以贝壳和硅藻为食。如果在铁施肥之前很长一段时间找不到座头鲸,那么座头鲸的回归可能是大规模铁施肥成功的标志。成功施铁的在线监测重点关注以下两组的同时变化;增加浓度组(叶绿素、O2、溶解氧(DO)、二甲基硫化物(DMS))和降低浓度组(硝酸盐、磷酸盐、硅酸盐、CO2、溶解CO2 (DCO2))。在部署富铁复合体后,昼夜监测叶绿素-a、硝酸盐磷酸盐和硅酸盐浓度,以准确测量藻华。
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Appropriate Location and Deployment Method for Successful Iron Fertilization
“High nutrient, low chlorophyll (HNLC)” regions were created by locking iron into sedimentary iron sulfides with hydrogen sulfide available from volcanic eruptions in surrounding oceans. Appropriate locations and deployment methods for the iron fertilization were far from volcanoes, earthquakes and boundaries of tectonic plates to reduce the chance of iron-locking by volcanic sulfur compounds. The appropriate locations for the large-scale iron fertilization are proposed as Shag Rocks in South Georgia and the Bransfield Strait in Drake Passage in the Southern Ocean due to their high momentum flux causing efficient iron deployment. The iron (Fe) replete compounds, consisting of natural clay, volcanic ash, agar, N2-fixing mucilaginous cyanobacteria, carbon black, biodegradable plastic foamed polylactic acid, fine wood chip, and iron-reducing marine bacterium, are deployed in the ocean to stay within a surface depth of 100 m for phytoplankton digestion. The deployment method of Fe-replete composite with a duration of at least several years for the successful iron fertilization, is configured to be on the streamline of the Antarctic Circumpolar Current (ACC). This will result in high momentum flux for its efficient dispersion on the ocean surface where diatom, copepods, krill and humpback whale stay together (~100 m). Humpback whales are proposed as a biomarker for the successful iron fertilization in large-scale since humpback whales feed on krill, which in turn feed on cockpods and diatoms. The successful large-scale iron fertilization may be indicated by the return of the humpback whales if they could not be found for a long period before the iron fertilization. On-line monitoring for the successful iron fertilization focuses on the simultaneous changes of the following two groups; the increase concentration group (chlorophyll, O2, Dissolved Oxygen (DO), Di Methyl Sulfide (DMS)) and the decrease concentration group (nitrate, phosphate, silicate, CO2, Dissolved CO2 (DCO2)). The monitoring of chlorophyll-a, nitrate phosphate, and silicate concentrations after deploying the Fe-replete complex is carried out throughout the day and night for the accurate measurement of algal blooms.
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