盘锦市海洋功能区划研究

在全面分析盘锦市海洋资源特点及开发利用中存在的问题，及充分考虑盘锦市未来社会发展需求的基础上，对盘锦海域进行了科学的功能分区，并确定了各功能区的主导功能。这将为盘锦市合理开发利用海洋资源，实现海洋综合管理提供服务，同时也有利于地区经济的持续发展。     

浙江沿岸海域海洋动物体内的石油烃水平

报道了浙江沿岸32种海洋动物体中的石油烃含量。结果表明，海洋动物体内的石油烃含量明显有软体类＞甲壳类＞鱼类的趋势；海洋动物的石油烃含量还与它们的生活方式有关，其含量有定居性动物＞游泳能力弱动物＞游泳能力强动物的特征；比较了各类海洋动物内石油烃在浙江沿岸不同海域的含量水平，还与国内外其他海域的海洋动物体内的石油烃含量作了比较。     

琼州海峡海洋环境现状调查与评价

根据 2 0 0 1年 9月份的调查资料 ,对琼州海峡的海洋环境质量现状进行初步评价。结果表明 ,水质因子全部满足二类海水水质标准 ,大部分满足一类标准 ,沉积物仅有个别样品超标 ,底栖生物残毒量均能满足评价标准。调查海域中北断面质量状况较差 ,南断面次之 ,中间断面最好 ,但整体上琼州海峡的海洋环境状况良好。     

有机磷农药对海洋微藻致毒性的生物学研究Ⅰ．四种海洋微藻对久效磷的耐受力与其SOD活性的相关性

本文研究了久效磷农药对扁藻、三角褐指藻、金藻和盐藻的毒性实验。结果表明，四种海洋微藻对久效磷的耐受力依次为：盐藻＞三角褐指藻＞金藻＞扁澡。对微藻细胞内过氧化物歧化酶（ＳＯＤ）活性的测定表明，四种海洋微藻对久效磷的耐受力与其ＳＯＤ活性具相关性，耐受力最强的盐藻其细胞内ＳＯＤ活性较高，并在久效磷的胁迫下保持相对稳定；耐受力较弱的三角褐指藻和金藻其细胞内ＳＯＤ活性随着久效磷浓度的提高逐渐下降；而耐受力弱的扁藻在久效磷胁迫下，其细胞内ＳＯＤ活性迅速下降。因此，可从ＳＯＤ活性及其变化规律上判断久效磷对海洋环境污染的程度以及海洋微藻的耐受力。     

Functionalization of nitrogen-doped graphene quantum dot: A sustainable carbon-based catalyst for the production of cyclic carbonate from epoxide and CO2

A series of organic compounds were successfully immobilized on an N-doped graphene quantum dot (N-GQD) to prepare a multifunctional organocatalyst for coupling reaction between CO₂ and propylene oxide (PO). The simultaneous presence of halide ions in conjunction with acidic- and basic-functional groups on the surface of the nanoparticles makes them highly active for the production of propylene carbonate (PC). The effects of variables such as catalyst loading, reaction temperature, and structure of substituents are discussed. The proposed catalysts were characterized by different techniques, including Fourier transform infrared spectroscopy (FTIR), field emission scanning electron microscopy/energy dispersive X-ray microanalysis (FESEM/EDX), thermogravimetric analysis (TGA), elemental analysis, atomic force microscopy (AFM), and ultraviolet–visible (UV-Vis) spectroscopy. Under optimal reaction conditions, 3-bromopropionic acid (BPA) immobilized on N-GQD showed a remarkable activity, affording the highest yield of 98% at 140°C and 10⁶ Pa without any co-catalyst or solvent. These new metal-free catalysts have the advantage of easy separation and reuse several times. Based on the experimental data, a plausible reaction mechanism is suggested, where the hydrogen bonding donors and halogen ion can activate the epoxide, and amine functional groups play a vital role in CO₂ adsorption.     

Carbon Management in Agricultural Soils

World soils have been a major source of enrichment of atmospheric concentration of CO₂ ever since the dawn of settled agriculture, about 10,000 years ago. Historic emission of soil C is estimated at 78 ± 12 Pg out of the total terrestrial emission of 136 ± 55 Pg, and post-industrial fossil fuel emission of 270 ± 30 Pg. Most soils in agricultural ecosystems have lost 50 to 75% of their antecedent soil C pool, with the magnitude of loss ranging from 30 to 60 Mg C/ha. The depletion of soil organic carbon (SOC) pool is exacerbated by soil drainage, plowing, removal of crop residue, biomass burning, subsistence or low-input agriculture, and soil degradation by erosion and other processes. The magnitude of soil C depletion is high in coarse-textured soils (e.g., sandy texture, excessive internal drainage, low activity clays and poor aggregation), prone to soil erosion and other degradative processes. Thus, most agricultural soils contain soil C pool below their ecological potential. Adoption of recommend management practices (e.g., no-till farming with crop residue mulch, incorporation of forages in the rotation cycle, maintaining a positive nutrient balance, use of manure and other biosolids), conversion of agriculturally marginal soils to a perennial land use, and restoration of degraded soils and wetlands can enhance the SOC pool. Cultivation of peatlands and harvesting of peatland moss must be strongly discouraged, and restoration of degraded soils and ecosystems encouraged especially in developing countries. The rate of SOC sequestration is 300 to 500 Kg C/ha/yr under intensive agricultural practices, and 0.8 to 1.0 Mg/ha/yr through restoration of wetlands. In soils with severe depletion of SOC pool, the rate of SOC sequestration with adoption of restorative measures which add a considerable amount of biomass to the soil, and irrigated farming may be 1.0 to 1.5 Mg/ha/yr. Principal mechanisms of soil C sequestration include aggregation, high humification rate of biosolids applied to soil, deep transfer into the sub-soil horizons, formation of secondary carbonates and leaching of bicarbonates into the ground water. The rate of formation of secondary carbonates may be 10 to 15 Kg/ha/yr, and the rate of leaching of bicarbonates with good quality irrigation water may be 0.25 to 1.0 Mg C/ha/yr. The global potential of soil C sequestration is 0.6 to 1.2 Pg C/yr which can off-set about 15% of the fossil fuel emissions.     

大弹涂鱼(Boleophthalmus Pectinirostris)作为放射性核素指示物的研究

以大弹涂鱼为对象,模拟其两栖生活的环境,采用示踪法并用S-80智能多道分析器与Ge(Li)探头研究了大弹涂鱼的整体及其组织器官对~(137)Cs、~(134)Cs、~(65)Zn、~(60)Co的富集与排出.探讨了其积累量、残留量与海水中核素浓度的相关性,推荐性腺、肌肉、头部作为监测海洋中~(137)Cs、~(134)Cs、~(65)Zn、~(60)Co污染的生物指示物.     

舟山潮差带海相沉积物的物理和化学特征

为舟山潮差带海相沉积物固结机理的深入研究提供物质基础,采用激光粒度仪分析了海相沉积物的粒度组成,并测试了海相沉积物的化学元素、化合物种类及其相对含量,还使用X-射线衍射技术分析了海相沉物的矿物组成。结果表明:海相沉积物含水率高、初始孔隙比大、呈流塑状,为低液限粉质黏土;活性指数为12.4,属于活动黏性土,矿物的亲水性较好;全盐含量高达9~11.2 g/kg,阳离子交换能力不强,有机质含量(5.82~12.7 g/kg)较高;pH 值为7.35~8.36,呈弱碱性,加上孔隙水中K+ ,Na+ ,Ca2+ ,Mg2+ 的存在,使得高岭石常不稳定,有向伊利石、蒙脱石或绿泥石转化的趋势。     

我国海洋塑料垃圾和微塑料排放现状及对策

当前海洋塑料和微塑料污染问题是全球研究热点,随着我国陆源垃圾减量化处置率和生活污水处理覆盖率的提高,重新核算我国海洋塑料垃圾和微塑料排放量尤为重要,基于文献已报道的关于海洋塑料垃圾和微塑料排放量估算的方法并结合相关统计数据对我国相应排放量进行了核算.结果表明:2016年我国向海洋中排放塑料垃圾124×104~331×104 t,略低于2010年的132×104~353×104 t;生活污水处理厂向环境中排放塑料微珠约109.95×1012粒（折合131.78 t）,远低于2014年报道的209.7×1012粒（折合306.9 t）.此外,2016年我国生活污水处理厂向环境中排放合成化学纤维类微塑料约1 296.95×1012个（折合648.48 t）,轮胎与地面摩擦产生合成橡胶轮胎粉尘约78.85×104 t;合成化纤类微塑料和合成橡胶轮胎粉尘等已成为陆源微塑料的重要来源.通过与发达国家和地区在海洋垃圾和微塑料污染、陆源垃圾处置、海洋垃圾污染应对等方面进行比较,未来我国应通过完善"限塑令"和生活垃圾分类体系、尽早实施"塑料微珠"限令、明晰生活污水处理厂微塑料排放状况等手段从源头控制排放,此外需有效控制塑料垃圾和微塑料的输送途径,制定和完善相关法律法规和监测标准,提升我国应对海洋塑料垃圾和微塑料污染的能力和国际影响力.