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31.
磷化氢在海水中的转化及其影响因素研究 总被引：1，自引：0，他引：1
通过室内模拟实验,研究了磷化氢在海水中的转化过程,分析了光照条件、氧化条件、通入方式等环境因子对磷化氢转化的影响。结果表明,在日光照射条件下,磷化氢在海水中可部分转化为磷酸盐,但转化率相对较低,转化过程复杂;环境因子在磷化氢转化过程中起重要作用,日光照射、紫外光照射、氧化条件等均能促进海水中磷化氢向磷酸盐和总磷的转化,在紫外光照射条件下检测到磷化氢向磷酸盐的最大转化率为66.6%。本研究对探索磷化氢在海洋环境生物地球化学循环中的作用具有重要意义。 相似文献
32.
Long-term data on diatom assemblages in a sediment core （60 cm） obtained from the Changjiang （Yangtze） River estuary were analyzed in order to assess the environmental changes that took place in the approximately 38 years （as determined by 210pb measurements）, i.e., between 1974 and 2012, of sediment accumulation. From the sediment core, 62 diatom taxa and genera were identified. The diatom biomass in the core generally increased beginning in the mid-1990s （core depth： 35 cm）, accompanied by a shift in the dominant species from Podosira stelliger and two species of Cyclotella （C. stylorum and C. striata） to Paralia sulcata, three species of Thalassiosira （ T. eccentria, I＂. oestrupii, and T. excentrica）, Actinoptychus undulates, and Thalassionema nitzschioides. The changes in both species diversity and abundance suggested that since the 1980s the estuary has undergone extensive eutrophication. This conclusion was supported by the increased proportion of planktonic species, another indicator of high nutrients inputs, in the Changjiang River estuary. 相似文献
33.
有害赤潮对海洋生态环境和沿海经济危害巨大,如何安全、有效地治理有害赤潮非常重要。文章考察了几种常见芽孢杆菌对近海典型赤潮生物——东海原甲藻(Prorocentrum donghaiense)的去除作用,发现解淀粉芽孢杆菌(Bacillus amyloliquefaciens)对其去除作用最强。进一步考察解淀粉芽孢杆菌对不同赤潮生物的去除作用,发现该芽孢杆菌对米氏凯伦藻(Karenia mikimotoi)和赤潮异弯藻(Heterosigma akashiwo)的去除作用高于东海原甲藻。在此基础上,将解淀粉芽孢杆菌与高岭土复合,研究了微生物复合粘土对典型赤潮生物的去除效果。结果表明,解淀粉芽孢杆菌与高岭土复合后,能够有效促进该菌的生长,进而提升了其对赤潮生物的去除能力。文章对芽孢杆菌及其复合粘土去除赤潮生物的机制进行了分析和探讨,为进一步发展和优化改性粘土治理赤潮技术体系提供了重要参考。 相似文献
34.
麻痹性贝类毒素(paralytic shellfish toxins,PSTs)是由某些甲藻产生的一种高毒性神经毒素,在海洋环境中分布广、危害大,可对水产养殖和人类健康造成重大危害;PSTs毒素的毒性大小随种类和结构的不同有较大差异。迄今,国内外学者针对PSTs的来源分布、迁移转化、生物合成及其影响因素等开展了大量的调查研究,但目前对于藻细胞产毒的生物合成途径、遗传学特征及其环境调控机理等研究仍处于起步阶段。PSTs的生物合成过程不仅与藻细胞自身生长阶段有关,还会受到光照、温度、营养盐等多种环境因素的影响,环境条件的改变会引起藻细胞毒素组成和含量发生不同程度的变化。近年来,研究人员应用基因组学和蛋白质组学技术,发现了产生PSTs的典型甲藻——亚历山大藻(Alexandrium)细胞内与PSTs毒素生物合成相关的某些基因或蛋白质,对我们更清晰地了解亚历山大藻产生PSTs毒素的机制具有重要意义。本文综合以往的研究报道,对亚历山大藻中PSTs的生物合成与转化及其主要影响因素进行了总结,以期为产毒有害藻华的防治提供科学依据。 相似文献
35.
长江水体溶解态无机氮和磷现状及长期变化特点 总被引：2，自引：0，他引：2
于2006年2、5、8和11月对长江从攀枝花至河口和上游的两条支流雅砻江和嘉陵江的溶解态无机氮(NO-3-N、NO-2-N和NH+4-N)和磷酸盐(PO43--P)进行了取样调查,同时结合长江营养盐的历史数据,分析了长江水体中溶解态无机氮、磷的长期变化特点。结果表明,长江NO-3-N、NH+4-N、DIN(包括NO-3-N、NO-2-N和NH+4-N)和PO3-4-P浓度从上游到下游显示出增加趋势,但存在季节差异;NO2-N浓度总体较低,在长江中下游(武汉—南京)浓度较高。长江从上游到下游DIN通量的变化主要受径流量的影响,从上游到下游单位面积年产N量逐渐升高;PO3-4-P输送通量从上游往下游呈增加趋势,也主要受径流量控制,但从季节变化来讲,PO3-4-P的月输送通量受其浓度的控制更加明显。自20世纪60年代来,长江水体中NO3--N、NO2--N、DIN和PO3-4-P的浓度都处于缓慢上升趋势,但到80年代上升速度明显加快;不同阶段DIN和34PO-P的季节变化特点也不尽相同,反映了其来源的差异。目前,长江水体中溶解态无机氮、磷浓度与国内及国际河流相比处于中等水平。 相似文献
36.
We established a budget model of nitrogen (N) inputs and outputs between watersheds and waterbodies to determine the sources of riverine N in the Changjiang (Yangtze) River drainage area. Nitrogen inputs in the budget included N from synthetic fertilizer, biological fixation by leguminous and other crops, wet/dry atmospheric deposition, excreta from humans and animals, and crop residues. The total N input was estimated to be 17.6 Tg, of which 20% or 3.5 Tg N was transported into waterbodies. Of the total N transported into waterbodies, the largest proportion was N from animal waste (26%), followed by N from atmospheric wet/dry deposition (25%), synthetic fertilizer N (17%), N in sewage wastes (17%), N in human waste from rural areas (6%) and industrial wastewater N (9%). We studied the spatial patterns of N inputs and outputs by dividing the Changjiang River drainage area into four sub-basins, from upstream to downstream: the Tongtian River drainage area (TTD, the headwater drainage area, 138 000 km 2 , less disturbed by human activities); the Jinsha River drainage area (JSD, 347 000 km 2 , less disturbed by human activities, approx. 3 500 km upstream of the Changjiang estuary); the Pingshan-Yichang drainage area (PYD, 520 500 km 2 , large-scale human disturbance, about 2 000 km upstream of the Changjiang estuary); and the Yichang-Datong drainage area (YDD, 699 900 km 2 , large-scale human disturbance, approx. 620 km upstream of the Changjiang estuary). The average N input into waterbodies was 2.3, 7.3, 24.1, and 28.2 kg N/ha in the TTD, JSD, PYD, and YDD sub-basins, respectively, suggesting an increase of N-components of more than 10 times from upstream to downstream areas. 相似文献
37.
To solve nutrient flux and budget among waters with distinct salinity difference for water-saltnutrient budget,a traditional method is to build a stoichiometrically linked steady state model.However,the traditional way cannot cope appropriately with those without distinct salinity difference that parallel to coastline or in a complex current system,as the results would be highly affected by box division in time and space,such as the Changjiang(Yangtze) River estuary(CRE) and adjacent waters(30.75°-31.75°N,122°10′-123°20′E).Therefore,we developed a hydrodynamic box model based on the traditional way and the regional oceanic modeling system model(ROMS).Using data from four cruises in 2005,horizontal,vertical and boundary nutrient fluxes were calculated in the hydrodynamic box model,in which flux fields and the major controlling factors were studied.Results show that the nutrient flux varied greatly in season and space.Water flux outweighs the nutrient concentration in horizontal flux,and upwelling flux outweighs upward diffusion flux in vertical direction(upwelling flux and upward diffusion flux regions overlap largely all the year).Vertical flux in spring and summer are much greater than that in autumn and winter.The maximum vertical flux for DIP(dissolved inorganic phosphate) occurs in summer.Additional to the fluxes of the Changjiang River discharge,coastal currents,the Taiwan Warm Current,and the upwelling,nutrient flux inflow from the southern Yellow Sea and outflow southward are found crucial to nutrient budgets of the study area.Horizontal nutrient flux is controlled by physical dilution and confined to coastal waters with a little into the open seas.The study area acts as a conveyer transferring nutrients from the Yellow Sea to the East China Sea in the whole year.In addition,vertical nutrient flux in spring and summer is a main source of DIP.Therefore,the hydrodynamic ROMS-based box model is superior to the traditional one in estimating nutrient fluxes in a complicated hydrodynamic current system and provides a modified box model approach to material flux research. 相似文献
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39.
改性粘土治理赤潮生物的主要原理是絮凝作用,但水体中未被去除的微藻对改性粘土有怎样的生理生化响应尚不清楚。本文以小球藻(Chlorella vulgaris)为模式生物,考察了改性粘土絮凝后水体中残余小球藻生理生化性质的变化情况。研究发现,经改性粘土或原土絮凝后,残余小球藻的生长受到了明显抑制,其丙二醛(malondialdehyde,MDA)含量迅速上升,改性粘土组的MDA含量高于原土组。除了原土组过氧化氢酶(catalase,CAT)活性相比对照组没有明显变化外,改性粘土组和原土组超氧化物歧化酶(superoxide dismutase,SOD)、CAT、抗坏血酸过氧化物酶(ascorbate peroxidase,APX)和谷胱甘肽过氧化物酶(glutathione peroxidase,GSH-PX)等酶活,均呈现先上升后下降、并稳定在较高水平的变化趋势。原土组各酶活普遍低于改性粘土组,但GSH-PX活性则相反。结果表明,改性粘土不仅能高效去除水体中的小球藻,而且能够刺激残余的藻细胞积累较多的O2-·和H2O2,从而对藻细胞造成过氧化伤害,抑制未被去除部分海洋微藻的正常生长。 相似文献
40.
球形棕囊藻(Phaeocystis globosa)赤潮是一种全球范围的生态灾害,而硝酸盐稳定同位素技术是研究海洋富营养化与赤潮暴发机制的前沿技术。为将该技术应用于球形棕囊藻赤潮暴发机制方面的研究,首先需了解其同化吸收硝酸盐的稳定同位素分馏特征。为此开展了球形棕囊藻室内培养实验,获取培养过程中氮、磷、硅等营养盐的浓度及硝酸盐氮、氧稳定同位素(δ15N-NO3-、δ18O-NO3-)等参数的变化特征,计算球形棕囊藻同化吸收硝酸盐的稳定同位素分馏系数。结果显示,NO3-和PO43-浓度随培养时间均呈现先明显下降后稳定的特征,同时伴随直径2~3mm的囊体出现并生长至2~3cm。NH4+浓度先后两次出现升高,推测可能是受到有机氮矿化过程的补充所致。随NO3-浓度降低,δ15N和δ18O的值分别在第13天和第7天达到相对峰值。经计算,球形棕囊藻同化吸收硝酸盐过程δ15N和δ18O分馏系数分别为3.32‰±0.38‰和3.12‰±0.59‰,而前者的分馏系数呈逐渐降低的特点,原因可能是随球形棕囊藻生长,发生酶还原的NO3-较参与跨膜运输的NO3-比例逐渐升高。研究首次给出了球形棕囊藻同化吸收硝酸盐过程的氮、氧稳定同位素分馏系数及其变化特征,补充了海洋微藻同位素分馏数据库,为稳定同位素技术研究球形棕囊藻赤潮暴发的营养机制提供了重要的基础数据。 相似文献