共查询到19条相似文献,搜索用时 140 毫秒
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通过对滇池地区某高硅磷块岩中Si元素的赋存状态研究,查明了Si元素及其赋存矿物的矿物学特征。该矿样中Si元素约90%赋存在硅质矿物石英、玉髓中,且以石英为主,约占71%;约10%赋存在硅酸盐矿物白云母、水云母、长石、高岭石、海绿石等中,故该矿样选矿脱硅应以脱石英为主。矿样中石英多呈不规则粒状,平均粒径为0.05mm;玉髓主要以硅质条带(条纹)或粒状胶磷矿的胶结物形态出现,和胶磷矿嵌布紧密;硅酸盐矿物的平均粒径为0.02mm。矿样需要细磨才能使有用矿物和脉石矿物解离,矿样磨至-0.074mm质量分数占99.10%时胶磷矿的单体解离度为92.52%,石英、玉髓的单体解离度为84.37%,单体解离情况较好。矿样中硅酸盐矿物的质量分数虽然较低,但会给选矿流程和后续湿法磷酸生产带来不利影响,因此在制定选矿工艺流程时应采取有效的脱硅方法。 相似文献
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黄麦岭磷矿是一大型沉积变质磷灰岩矿床。尽管矿石易采易选,但碳酸盐的抑制也相当困难,许多科研单位对此进行了广泛研究,本文将对研究结果作一综合评述。 一、矿石性质 黄麦岭磷矿上层为风化矿,下部为原生矿,碳酸盐矿物主要赋存在原生矿中。有用矿物主要为氟磷灰石及少量黄铁矿,脉石矿物主要是石英、微斜长石、白云石、白云母、 炭质,石墨等。 磷灰石矿物粒度一般介于0.08~0.3毫米,常与石英、长石、白云石密切共生。碳酸盐以白云石为主,仅含少量方解石。形状多呈不规则粒状,不均匀分布,常充填于其它矿物间隙中,粒度介于0.1~0.6毫米。 相似文献
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云南难选混合型低品位胶磷矿磷含量低、硅镁铁铝等杂质含量高,通过磨矿细度试验,在最佳磨矿细度下对该矿石开展了矿物可选性和试验产品的工艺矿物学研究,结果表明:在磨矿细度为-0.074 mm质量分数占96%时,各浮选时间段的精矿中有用矿物碳氟磷灰石与其他脉石矿物的总体解离(88%~91%)较好,连生体较少;而石英单体解离相对较差(77%~90%),与碳氟磷灰石连生体较多(7%~20%);在相同浮选时间内,白云石与碳氟磷灰石的可浮性相近,相对易浮;褐铁矿、云母矿、石英和玉髓可浮性相近,褐铁矿、云母矿相对石英较难浮。各矿物的可浮性相近难以有效分离是磷精矿指标差的主要原因。 相似文献
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石门磷矿枫箱坡矿段属浅海相沉积层状磷块岩矿床,矿石类型为硅钙质胶磷矿,呈极细粒嵌布,P_2O_5平均品位16.12%,为中低品位磷矿石,矿石中有用矿物为胶磷矿(微碳氟磷灰石),脉石矿物主要为白云石、石英。矿石呈条带状、微层状、块状嵌布。胶 相似文献
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浏阳磷矿含P_2O_5大于24%的原矿作商品矿或生产黄磷,小于15%的低品位矿石堆积在廖岩坡。为解决该矿石的工业应用,进行了实验室及扩大脱泥浮选试验。 一、矿石特性 浏阳磷矿属浅海沉积变质磷块岩矿床,胶磷矿集合体包裹微细石英、褐铁矿及粘土矿物,致密相嵌。含磷矿物80%是胶磷矿,其次磷赋存在银星石、纤磷钙铝石和粘土矿物中,含量分别为(%):8.37、4.31、6.56。 相似文献
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云南浮选风化磷矿生产湿法磷酸起泡原因研究 总被引:1,自引:0,他引:1
风化磷矿是碳酸盐类磷矿经风化作用形成的一种高质量矿石,是一种新的磷矿石工业类型。二水湿法磷酸生产企业采用浮选风化磷矿作为生产原料时萃取槽会出现大量稳定性泡沫。经过实验,证明起泡的主要原因来自于风化磷矿浮选药剂,而非风化矿自身的物理性质。解决起泡的关键在于调整浮选药剂配方,即使用高效低泡浮选药剂以及在萃取工序增加必要的消泡措施。 相似文献
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S. Agyin-Birikorang M. K. Abekoe O. O. Oladeji 《Nutrient Cycling in Agroecosystems》2007,79(2):113-123
Phosphorus inputs are required in highly weathered tropical soils for sustainable crop production. However, high cost and
limited access to mineral P fertilizers limit their use by resource-poor farmers in West Africa. Direct application of finely
ground phosphate rock (PR) is a promising alternative but low solubility of PR hampers its use. Co-application of PR with
manure could be a low cost means of improving the solubility of natural PR and improve their agronomic effectiveness. Our
objective was to quantitatively estimate the enhancement effect of poultry manure on P availability from low reactive PR (Togo
phosphate rock) applied to highly weathered soils. We utilized two highly weathered soils from Ghana and Brazil for this greenhouse
study. Using 32P isotopic tracers, the agronomic effectiveness of poultry-manure-amended Togo rock phosphate (TPR) was compared with partially
acidulated Togo rock phosphate (PAPR) and triple superphosphate (TSP). Four rates of poultry manure: 0, low (30 mg P kg−1 soil), high (60 mg P kg−1 soil) and very high (120 mg P kg−1 soil) were, respectively, added to a constant amendment (60 mg P kg−1 soil) of the P sources and applied to each pot of 4 kg soil. A Randomized Complete Block Design was used for the greenhouse
experiment and Maize (Zea mays L.) was used as a test crop. The plants were grown for 42 days after which the above ground biomass was harvested for analysis.
Without poultry manure addition, the agronomic effectiveness, represented by the relative agronomic effectiveness (RAE) and
proportion of P derived from fertilizer (% Pdff) was in the order TSP > PAPR > TPR = control (P0). In the presence of low rate poultry manure addition, the agronomic effectiveness followed the order TSP > PAPR = PR > P0. However, at the high and very high rates of poultry manure addition, no significant differences in agronomic effectiveness
were observed among the P sources, suggesting that at this rate of poultry manure addition, PR was equally as effective as
TSP. The study showed that direct application of PR co-applied with poultry manure at a 1:1 P ratio will be a viable option
for P replenishment. Thus a combination of PR and poultry manure could be a cost-effective means of ensuring sustainable agricultural
production in P-deficient, highly weathered tropical soils. 相似文献
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安宁市县街磷矿床属古生代下寒武统梅树村组大型浅海相层状磷块岩矿床。磷矿层有上、下两层,分别产于梅树村组中谊村段的1m1-3和1m1-1两个层位。中低品位磷矿石产于下矿层,主要由磷酸盐矿物和脉石矿物两部分组成,含较多碎屑成分,矿石品位10%~20%。磷酸盐矿物以胶磷矿为主,主要呈球粒或集合体球粒产出,以及在基质中呈胶结物。矿石类型主要为白云质球粒磷块岩、碎屑状砂屑磷块岩。矿石结构、构造主要为内碎屑结构、条带状构造。矿层相对稳定,但P2O5含量与矿石结构构造关系密切,品位变化明显。 相似文献
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In a series of greenhouse experiments granulated phosphate fertilizers prepared by mixing triple superphosphate with phosphate rock and partially acidulated phosphate rock, ranging in their content of water souble P from 95 to 17 per cent of total P were applied to neutral and slightly alkaline (pH 6.9–7.8), sandy loam to clay soils ranging in calcium carbonate content from 2 to 35 percent. Dry matter yield of clover, alfalfa, millet or maize were obtained, P uptake determined and sodium bicarbonate extractable P in soil measured. In one field experiment triple superphosphate was compared to mixture of triple superphosphate and phosphate rock on maize. X ray difraction on one triple superphosphate — phosphate rock mixture and on one partially acidulated phosphate rock showed that both fertilizers contain mainly monocalcium phosphate and fluorapatite. After incubation in soil the dicalcium phosphate content rose and the monocalcium phosphate disappeared.Parameters received in greenhouse experiments and in the field indicate that phosphate fertilizers composed of superphosphate and up to 50 percent phosphate rock are as efficient source of P to plants on calcareous and slightly alkaline soils as superphosphate. If this indication would be proven in extensive field experimentation it would lead to savings in acid consumption and in fertilizer manufacturing plant capacity for calcareous soils. 相似文献
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牙舟陶在陶瓷业界具有举足轻重的地位,陶土对牙舟陶性能具有重要的影响。为加强对牙舟陶的研究,采用化学分析法、激光粒度仪、X射线衍射仪、综合热分析仪、数显白度仪等测试手段对牙舟陶土的化学组成、粒度分布、晶相组成、热性能及白度进行了检测。结果表明:牙舟陶土主要由石英和珍珠石组成,石英质量分数为59.34%、珍珠石质量分数为34.78%。牙舟陶土颗粒分布广泛,粒径小于6.5 μm的颗粒质量分数达到58.67%,粒径越小石英含量越低。在此基础上,结合贵州黔南丰富的磷矿资源,研究加入磷矿后牙舟陶土在煅烧过程中白度、硬度及物相组成的变化规律。研究表明:牙舟陶土的白度随着温度的升高先增大后减小,在1 100 ℃时达到最大值45.5%;加入磷矿组分后,在1 100 ℃时牙舟陶土的白度增加至54%,且煅烧时固熔体形成温度下降、烧结温度降低,并伴随钙长石矿物的产生。 相似文献