首页> 外文OA文献 >Geochemical variations in glauconitic minerals : application as a potassium fertiliser resource.
【2h】

Geochemical variations in glauconitic minerals : application as a potassium fertiliser resource.

机译:青光石矿物的地球化学变化:用作钾肥资源。

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Nutrients for plant growth are often limited in soil systems and additions are required in the form of fertiliser. Potassium is an essential macro-nutrient for plants and demands for K are expected to increase in the future. Glaucony is an abundant marine mineral which may provide an alternative K-rich fertiliser resource. The South Island of New Zealand contains deposits of glaucony-rich rocks which were deposited in the Early- to Mid-Cenozoic during periods of low sedimentation to the seafloor. Here, the geochemistry of glaucony from the Waitaki Basin (Otago), the Waipara Greensand (North Canterbury) and the Stoney Creek Limestone (Karamea) was examined using spatially resolved geochemical analysis and dissolution experiments. Grain-by-grain analysis using Laser Ablation Induction Coupled Plasma Mass Spectrscopy (LA-ICP-MS) and Scanning Electron Microscopy with Energy Dispersive Spectroscopy (SEM + EDS) revealed that glaucony from all deposits were of the mature type and were enriched in K. Glaucony derived from growth inside faecal pellets was found to contain elevated K and Fe concentrations compared to bioclast hosted glaucony. These variations can be explained by the physical properties of host grains and sea-floor redox conditions at the time of precipitation, both of which increased ionic mobility into the zone of glauconitisation. Solubility analysis showed that K^{+} was released from glaucony more rapidly than any other element. Additionally, decreasing the pH and introducing an oxidising agent (i.e, birnessite which is ubiquitous in soil environments) accelerated K^{+} release 13-fold. Trace metals including Cr, Zn, Cu and Ni were present in the solid phase analysis, however further investigation revealed that these elements were released into solution in low concentrations and may present a source of micro-nutrients, not a soil contaminant. These results suggest that glaucony may offer a source of slow releasing K fertiliser, and the South Island of New Zealand is ideally situated as a place to consider using glaucony as a locally sourced, environmentally sustainable K resource for agriculture.
机译:用于植物生长的营养素通常在土壤系统中受到限制,并且需要以肥料的形式添加。钾是植物必不可少的大量养分,钾的需求在未来有望增加。青草是一种丰富的海洋矿物,可提供替代的富含钾的肥料资源。新西兰南岛的沉积物富含冰川灰岩,沉积在海底低沉积时期的新生代早期至中期。在这里,使用空间分辨地球化学分析和溶出实验研究了怀塔基盆地(奥塔哥),怀帕拉格林桑德(北坎特伯雷)和斯托尼克里克石灰石(卡拉梅亚)的青瓷的地球化学。使用激光烧蚀诱导耦合等离子体质谱(LA-ICP-MS)和带能谱仪(SEM + EDS)的扫描电子显微镜进行的逐颗粒分析表明,所有沉积物中的青光眼属于成熟类型,并且富含K与生物碎裂寄主的青冈相比,发现粪便颗粒内部生长产生的青冈含有较高的钾和铁浓度。这些变化可以通过沉淀时宿主颗粒的物理特性和海底氧化还原条件来解释,这两者都增加了进入青光眼炎区域的离子迁移率。溶解度分析表明,K ^ {+}的释放比其他任何元素都快。另外,降低pH值并引入氧化剂(即在土壤环境中普遍存在的水钠锰矿)加速了K ^ {+}的释放13倍。固相分析中存在痕量金属,包括Cr,Zn,Cu和Ni,但是进一步的研究表明,这些元素以低浓度释放到溶液中,可能是微量营养素的来源,而不是土壤污染物。这些结果表明,青草可能提供了缓释钾肥的来源,新西兰的南岛地理位置优越,可以考虑将青草用作当地来源的,环境可持续的农业钾素资源。

著录项

  • 作者

    Smaill Joshua Ballantyne;

  • 作者单位
  • 年度 2015
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类

相似文献

  • 外文文献
  • 中文文献
  • 专利

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号