纤维水镁石在氨基酸水溶液中的电化学及溶解作用研究

在模拟人体温度３７℃条件下,进行水镁石纤维粉尘与氨基酸作用的实验研究,测定在７２ｈ内溶液过程中ｐＨ值的电导率的变化,结果表明,纤维矿物在氨基酸中发生了有机配合作用,并且中性氨基酸对矿物的溶解能力最强。     

大别造山带北部的中生代火山岩

大别造山带北部的北淮阳中生代火山喷发岩带形成于后造山阶段的晚侏罗世—早白垩世。火山岩可以划分为２个独立的火山旋回,分别对应于高钾钙碱性系列（ＨＫＣＡ）和钾玄岩系列（ＳＨＯ）,从岩石构造组合和岩石地球化学数据提供的约束条件分析,前者形成于晚侏罗世的陆内挤压环境,造山带是有“山根”的增厚陆壳,而早白垩世钾玄岩系列岩石的出现表征着造山带已发生“去根”作用,北淮阳处于陆壳减薄的拉张环境     

Study on topographic compensation model of the Okinawa Trough I. Calculation of theoretical isostatic response function

INTRODUCTIONTo study the compensation model of sea topography and isostatic states by using toPOgraphicand gravity data, is an imPOrtant mean for further researching deep structures as elastic structure,stress state of lithosphere, and so on. Since Airy and Pratt proPOsed local isostatic model in the1850' s, greater development on the theoretical study has been attained. Veining Meinesz (1941 )introduced regional compensation mechanism by considering it as floating crust in elastic fie…     

大亚湾养殖水域沉积物-海水界面营养盐扩散通量

1998年5月10日和11日分别在大亚湾的大鹏澳和澳头养殖水域现场调查,分析了底层海水、上覆水、沉积物间隙水中营养盐的含量和磷的化学形态。结果表明：大亚湾养殖水域NH,HPO和H4SiO4含量从大至小为：间隙水,上覆水,底层海水;NO和NO含量变化不大。估算了沉积物一海水界面营养盐扩散通量,NH,NO,NO,HPO,H4SiO4平均通量分别为302．0,－0．06,－1．82,2．53,47．96μmol·（m2·d）－1。水体和沉积物中磷的主要化学形态分别为DOP（占TP的54％）和无机态（占总态的60％）。大亚湾养殖水域浮游生物生长由磷控制。沉积物间隙水中NO,NO,HPO,H4SiO4的浓度垂直分布变化不大,而NH的浓度垂直分布呈指数下降特征。     

四川盆地大气边界层气象资料数据系统

本文介绍在IBM-PC微机(或兼容机)上利用DBASEⅡ、BASIC和FOR-TRAN语言设计和研制的一套大气边界层气象资料数据库软件系统,给出它的主要结构和功能。该系统实现了大气边界层气象资料共享和信息化处理,不但操作简便、快速、准确、稳定性好,而且具有较强的通用性和较大的实用价值。     

基于ST-ConvLSTM的南海海表面CO2分压的空间和时间序列预测

海表面二氧化碳分压(pCO₂)的未来变化趋势,对统计评估全球碳收支以及理解全球气候变化背景下的海洋酸化现象至关重要。目前传统的海面pCO₂预测方法大部分基于有限的实测数据,然而实测数据存在着时间和地理方面的制约,且计算成本较高。近年来,随着时空观测数据的爆炸性增长,基于深度学习的数据驱动模型在海表面pCO₂预测方面中表现出良好的潜力。然而,由于多种环境因素与海表面pCO₂之间的关系错综复杂,到目前为止尚无十分简单有效的相关模型来对海表面pCO₂进行预测。为应对这一挑战,利用时空卷积长短时记忆神经网络(ST-ConvLSTM)模型,通过海面温度(sea surface temperature, SST)、海面盐度(sea surface salinity, SSS)、叶绿素a浓度(chl a)和海面pCO₂数据,预测南海的海面pCO₂,并将2019年1～12月的数据作为测试集对模型的表现进行了验证。结果显示, ST-ConvLSTM模型...     

Controlling factors on the charging process of oil and gas in the eastern main sub-sag of the Baiyun Sag,Zhujiang River (Pearl River) Mouth Basin

The eastern main sub-sag (E-MSS) of the Baiyun Sag was the main zone for gas exploration in the deep-water area of the Zhujiang River (Pearl River) Mouth Basin at its early exploration stage, but the main goal of searching gas in this area was broken through by the successful exploration of the W3-2 and H34B volatile oil reservoirs, which provides a new insight for exploration of the Paleogene oil reservoirs in the E-MSS. Nevertheless, it is not clear on the distribution of “gas accumulated in the upper layer, oil accumulated in the lower layer” (Gas_upper-Oil_lower) under the high heat flow, different source-rock beds, multi-stages of oil and gas charge, and multi-fluid phases, and not yet a definite understanding of the genetic relationship and formation mechanism among volatile oil, light oil and condensate gas reservoirs, and the migration and sequential charge model of oil and gas. These puzzles directly lead to the lack of a clear direction for oil exploration and drilling zone in this area. In this work, the PVT fluid phase, the origin of crude oil and condensate, the secondary alteration of oil and gas reservoirs, the evolution sequence of oil and gas formation, the phase state of oil and gas migration, and the configuration of fault activity were analyzed, which established the migration and accumulation model of Gas_upper-Oil_lower co-controlled by source and heat, and fractionation controlled by facies in the E-MSS. Meanwhile, the fractionation evolution model among common black reservoirs, volatile reservoirs, condensate reservoirs and gas reservoirs is discussed, which proposed that the distribution pattern of Gas_upper-Oil_lower in the E-MSS is controlled by the generation attribute of oil and gas from source rocks, the difference of thermal evolution, and the fractionation controlled by phases after mixing the oil and gas. Overall, we suggest that residual oil reservoirs should be found in the lower strata of the discovered gas reservoirs in the oil-source fault and diapir-developed areas, while volatile oil reservoirs should be found in the deeper strata near the sag with no oil-source fault area.     

陆水水库的浮游生物及营养类型

报道了１９９１￣１９９５年对面积为１６９３ｈｍ＾２的黑龙滩水库渔业利用优化模式研究的结果,主要内容有：水生生物种类组成和现存量调查、浮游植物初级生产力测定、渔获物统计和鱼产力估算;水体理化性状和水位变化对鱼产量和浮游生物群落结构的影响,网箱养殖鲤、草鱼的高产试验结果;多功能水库生态系统的渔业利用优化模式初步探讨。经三年努力,水库鱼产量由６２２ｔ上升到１２５５．１ｔ,平均单产７５０ｋｇ／ｈｍ＾２。为     

高质量发展下用海效益评估方法研究——以台州市为例

实际用海效益包括海域资源在生产过程中产生的直接经济收益和生态环境系统的负面效应,文章通过建立海洋高质量用海效益评估模型反映和量化实际用海效益,并将该模型在台州市海域应用,研究结果发现,台州市涉海县、市、区中椒江区实际单位用海效益最高为68.85万元/hm2,玉环市最低为4.02万元/ hm2。原因在于椒江区不仅其海域资源价值表现良好,而且生态环境损害程度得到了有效控制。从而得出,海洋经济高质量发展绝对不是海域资源过度使用,也不是海洋生态环境的绝对保护,两者是相互统一、相互协调的,保证海域资源使用价值保值增值是海洋经济合理运行的基础,保护海洋生态环境系统是海域资源使用价值保值增值的根本,这是引导海洋经济高质量发展的重要路径。     

基于SWOT分析的南海区海洋牧场发展路径

海洋牧场作为修复海洋生态系统和实现渔业资源增殖的现代渔业模式,是促进海洋经济绿色发展、推动传统渔业转型升级和构筑海洋命运共同体中的重要一环。然而,在实际建设中存在多种制约现代海洋牧场高质量发展的因素。合理规划海洋牧场,充分发挥其生态、社会、经济效益,对海洋牧场持续发展至关重要。文章对南海区海洋牧场的建设、技术发展及政策管理现状进行了总结,并利用SWOT分析法对南海区海洋牧场的发展情况进行了综合分析,阐释了南海区海洋牧场发展存在的优势、劣势、机遇和挑战,并结合国内外海洋牧场建设的经验及发展趋势,提出了南海区海洋牧场产业发展的路径,以期为我国海洋牧场高质量发展提供借鉴。