乳山湾外邻近海域氮和磷的分布与收支过程研究     

臧家业  赵晨英  刘军  张爱军  尹训强  刘季花  王昊  王以斌  冉祥滨 《海洋学报》2019,41(12):26-38

基于2009年6–9月，2014年5月，2014年7–8月在乳山湾外邻近海域的综合调查资料，分析了该开放海域水体与沉积物中氮、磷营养盐的组成和分布，并在潮汐潮流数值模式计算水通量的基础上分析了近岸开放区域无机氮(DIN)和无机磷(DIP)的循环与收支的主要过程，量化了潮汐潮流、初级生产的消耗与转化、底界面过程与内部循环等过程对氮和磷营养盐循环与收支的影响。结果表明，夏季乳山湾外邻近海域水体DIN和DIP的浓度与分布受陆源输入和潮汐潮流的共同影响，高值均出现在湾口区域；沉积物-水界面存在DIN和DIP从沉积物向上覆水释放的现象，使得底层水体的氮、磷营养盐浓度高于表层水体。氮的收支表明，研究海域水体内部循环过程是初级生产所需DIN的主要来源，占初级生产总消耗量的86%，其次是水交换作用(11%)，底界面扩散对初级生产的贡献相对较小(3%)；水体DIN的移出主要是通过埋藏、向外海的输送和水体反硝化作用，其比例分别为80%、16%和4%。磷的收支显示，研究海域水体内部循环过程贡献了初级生产所需DIP的91%，其次是水交换作用(9%)，底界面扩散对初级生产的贡献小于1%；水体DIP支出主要是通过沉积埋藏和向外海的输送，其比例分别为67%和33%。研究结果表明内部循环过程是近海水体氮和磷获得补充的主要途径，不过外部来源的氮、磷营养盐结构与系统内部具有显著的差异，且系统内磷的埋藏效率要高于氮，其必将对乳山湾外邻近海域营养盐结构和初级生产产生长远的影响。  相似文献   

夏季南极普里兹湾氮吸收受融冰调控     

张润  马嫱  陈敏  郑敏芳  曹建平  邱雨生 《海洋学报(英文版)》2019,38(8):1-7

本研究将稳定同位素（¹⁵N）与放射性核素（²²⁶Ra）示踪相结合，探讨了2006年夏季南极普里兹湾融冰过程对氮吸收的调控作用。硝酸盐及铵盐的比吸收速率均与浓度呈正相关关系，表明底物浓度效应的存在。开阔洋区具有较高的f比值，而在埃默里冰架附近f比值低得多。f比值与冰融水份额之间存在负相关关系，暗示融冰过程在调控水体氮吸收方面起着重要作用。融冰改变了当地上层水体的层化条件，显著地影响南大洋的生物泵效率及对大气二氧化碳的吸收。本研究为南大洋上层水体碳、氮动力学的调控机制提供了新的认识，且有助于对历史记录的解读及对未来气候变化的预测。  相似文献   

南海北部海域沉积物中生物钡、碳氮同位素的组成特征及其与表层水体初级生产之间的关系     

倪建宇  赵军  江巧文  姚旭莹 《海洋学报》2019,41(2):41-51

通过对采集自南海北部的D06和S0612两个短柱状沉积物样品中的不同赋存形态钡、有机碳和生物硅的含量以及有机质碳氮同位素组成的分析，结果表明沉积物中的钡主要以碎屑钡和自生的生物钡形式存在。沉积物中生物钡的含量在10.3~385.2 μg/g之间，平均值为177.0 μg/g，据此计算的新生产力在12.3~146.7 mg/（d·m2）（以碳计）之间，平均为78.9 mg/（d·m2）；D06站计算的结果和附近站位的实测值相当。沉积物中有机碳的含量在0.64%~1.34%之间，平均值为0.89%，C/N比值为4.96~5.93，平均值为5.54。有机碳的δ13C值在-22.98‰~-20.73‰之间，平均值为-21.46‰，依据端元组份同位素组成计算的陆源有机质比率显示，D06站位的有机质主要来自海洋生物，而S0612站位则受陆源有机质的影响较大。沉积物中有机质的δ15N值在3.96‰~6.29‰之间，平均值为5.26‰，反映的是该海区氮源的同位素组成，而不受硝酸盐利用率的影响。  相似文献   

大气氮沉降对南黄海初级生产过程影响的数值研究     

郭伟  史洁  朱君莹  赵亮 《中国海洋大学学报(自然科学版)》2020,(1):115-125

本研究利用三维物理-生物耦合模型模拟了大气氮沉降对南黄海主要初级生产过程的影响,并通过数值实验区分了不同季节大气氮沉降的贡献。模拟结果显示,大气氮沉降明显增大了南黄海表层溶解无机氮的浓度,近岸海域增加量较大,可以达到3.0 mmol/m^3,且由近岸海域到黄海中部海域有明显的递减趋势,这主要是由于近岸海域无机氮来源众多,导致浓度较高,大气沉降的氮不会被浮游植物生长吸收,出现氮累积。大气氮沉降明显促进了黄海中部春季表层水华和夏季次表层叶绿素最大值两个重要初级生产过程,春季表层叶绿素增加量最大,可达0.20 mg/m^3,夏季次表层叶绿素浓度增加最显著,可达0.10 mg/m^3,分别约为峰值浓度的10%和6%。不同季节大气氮沉降对初级生产过程的贡献不同,冬季氮沉降可以存留下来影响春季水华过程,但作用小于春季氮沉降;夏季,由于水体层化较强,本季的氮沉降对次表层叶绿素最大值的促进作用并不明显,反而冬季氮沉降的影响大于春季和夏季的氮沉降。同时,大气氮沉降也促进了氮循环的各个过程,包括浮游植物生长吸收、呼吸释放和矿化过程。  相似文献   

氨氮胁迫对方斑东风螺六种免疫酶活性的影响     

谭春明  赵旺  吴开畅  张玥  杨蕊  温为庚  陈旭  于刚 《海洋科学》2019,43(3)

本文研究了氨氮对方斑东风螺(Babylonia areolata)的急性毒性及不同浓度的氨氮溶液(22、47.5、102和220 mg/L)对其体内六种免疫酶(CAT、ACP、AKP、T-SOD、GSH-PX和POD)活性的影响。实验结果表明：氨氮浓度越大,其毒性作用越强,方斑东风螺死亡率越高；500 mg/L氨氮处理组于24 h便出现(20.3±2.1)%死亡率,并且96 h后存活率降为0。而相同条件下,随试验时间的延长,方斑东风螺死亡率也越高。氨氮浓度和处理时间均对方斑东风螺免疫酶活力有显著的影响(P < 0.05)。与对照组相比,处理组CAT和AKP活性均表现出“诱导—抑制”的趋势,ACP和T-SOD活性表现出“抑制—诱导”的趋势,CSH-PX活性呈现“诱导—抑制—诱导”的趋势,而氨氮对处理个体POD活性的影响整体表现为抑制作用。可见,养殖水体中的氨氮会对方斑东风螺免疫酶活性产生较大的影响。本研究从生态现象和生理指标相结合的方式阐述了氨氮对方斑东风螺个体的致毒特性,将对方斑东风螺的养殖具有实用意义,充实了氨氮对贝类毒理实验免疫性能层面的基础数据,可为其他贝类氨氮胁迫实验提供数据基础和科学依据。  相似文献   

Effects of Forest Types and Environmental Factors on Soil Microbial Biomass in a Coastal Sand Dune of Subtropical China     

GAO Wei  LIN Meimei  HUANG Yongrong  HUANG Shide  YE Gongfu  HUANG Zhiqun 《资源与生态学报(英文版)》2020,11(5):454-465

Coastal sand dune ecosystems generally have infertile soil with low water-holding capacity and high salinity. However, many plant species have adapted to the harsh sand environment along the southeastern coast of China. Studying the microbial biomass in such an ecosystem can improve our understanding of the roles that microbes play in soil fertility and nutrient cycling. We investigated the differences in soil microbial biomass carbon (MBC) and nitrogen (MBN) contents and their seasonal dynamics in five forest types (a secondary forest and plantations of Casuarinas, Pine, Acacia, and Eucalyptus). The results indicated that the seasonal variations of soil MBC and MBN contents in all five forest stands were higher in spring and winter, but lower in summer and autumn. The MBC content was lower in the Casuarinas plantation than in the other plantations in the same soil layer. However, no significant differences were observed in MBN contents among the different forest types. The MBC and MBN concentrations were positively correlated with soil moisture, but negatively correlated with soil temperature. The MBC and MBN contents also decreased with increasing soil depth. Across all soil layers, secondary forest had the highest MBC and MBN concentrations. Our study also showed that the MBC and MBN contents were positively affected by total soil carbon (TC), pH, and litter N content, but were negatively impacted by soil bulk density and litter C content. Moreover, the MBN content was positively correlated with root N content. In summary, environmental factors and the differences in litter and fine roots, soil nutrient contents, as well as the soil physical and chemical properties caused by different tree species collectively affected the concentrations of the soil MBC and MBN.  相似文献   

浒苔Up-MIR-843及其靶基因分析     

杨娟娟  於大春  沈颂东 《海洋学报(英文版)》2020,39(10):27-34

非编码小分子RNA (non-coding small RNAs, microRNAs)在植物的生长，发育和应对非生物胁迫过程中发挥着重要作用。本研究分析了氮剥夺和高温刺激条件下，浒苔Up-miR-843及其靶基因的表达变化。结果表明，生物信息学分析可以得到184个Up-miR-843靶基因。氮缺乏可以显著增加Up-miR-843的水平，同时降低细胞周期相关基因Cyclin A3和Cyclin L的表达，而高温刺激对Up-miR-843的表达不产生影响。同时，Up-miR-843高表达的浒苔与正常条件培养的浒苔比较，生物量和光合作用合成速率显著增加。因此，我们推测氮剥夺和高温应激响应microRNAs可能通过介导其靶基因表达，调节浒苔的生长。  相似文献   

Physical and biological drivers of sediment oxygenation and denitrification in a New Zealand intermittently closed and open lake lagoon     

Josie A. Crawshaw  Marc Schallenberg  Candida Savage 《新西兰海洋与淡水研究杂志》2019,53(1):33-59

Intermittently closed and open lakes and lagoons (ICOLLs) are shallow estuarine ecosystems, many of which show eutrophication symptoms. The physical and biological drivers of sediment oxygenation and denitrification were examined in a New Zealand ICOLL using in situ enclosures for one year. Denitrification was seasonally and spatially variable, and higher denitrification rates were driven by organic matter availability, temperature and nitrate flux. The bulldozing invertebrates generally deepened oxygen penetration in 18% of oxygen profiles, consistent with their effect in multiple regressions. Chironomid larvae (Chironomidae) dominated the benthic community, and their tubular burrows modified oxygen penetration into the sediment in 18% of profiles, potentially affecting denitrification in the ICOLL through bioirrigation. Our study shows that macroinvertebrates support increased sediment oxygenation; therefore the use of artificial opening regimes in many ICOLLs may have negative effects on macroinvertebrate community composition and may consequently inhibit denitrification.  相似文献   

氨氮对海月水母螅状体和碟状体的急性及慢性毒性作用     

葛建龙  孟乾  陈四清  刘琨  刘长琳  谭杰  边力 《海洋与湖沼》2018,49(4):809-814

本研究采用静水实验法,在水温21℃、盐度30、pH8.10条件下,分析了水体氨氮对海月水母(Aurelia coerulea)螅状体以及碟状体的急性毒性作用,并且探讨了慢性氨氮胁迫对海月水母螅状体无性生殖的影响。急性毒性实验结果显示,氨氮毒性效应与浓度和胁迫时间呈正相关,氨氮对螅状体24、48、72、96h半致死浓度分别为225.60、164.26、62.67和25.44mg/L,氨氮对碟状体24、48、72、96h半致死浓度分别为49.96、31.53、24.54和21.43mg/L,螅状体与碟状体的总氨氮安全浓度分别为2.54和2.14mg/L,非离子氨安全浓度分别为0.13和0.11mg/L。慢性氨氮毒性实验显示,实验组螅状体产生的子代螅状体数少于对照组,而随着胁迫时间延长,螅状体繁殖子体的速率恢复至对照组水平。研究结果表明,氨氮对海月水母具有毒性作用,富营养化水体中氨氮含量升高不是海月水母暴发的直接原因;此外,海月水母螅状体可能具有一定的适应慢性氨氮胁迫的自我调节能力。  相似文献   

Nitrate removal processes in the riverbed during a single-peak flood event     

Qihao Jiang  Guangqiu Jin  Hongwu Tang  Junzeng Xu  Qi Wei  Ling Li 《水文研究》2021,35(2):e14041

The effect of the interplay between unsteady flow and bedform in a flood event on nitrogen cycling in the hyporheic zone (HZ) remains poorly understood. In this study, a reactive transport groundwater model with different flood hydrographs was proposed to investigate the effect of modified hyporheic flow on nitrate dynamics in the HZ, including nitrate source-sink function, response to the single-peak flood event and removal efficiency. The results demonstrate that there exists an optimal range of river channel gradients that could enhance the biogeochemical reactions (respiration, nitrification and denitrification) in a flood event. The HZ acts as a nitrate sink especially after the flood event, and its source-sink function is independent of the unsteady discharge/stage conditions. The nitrate in the HZ has a hysteretic response to peak stage/discharge, and its removal efficiency is decreased by up to 70% compared to steady flow conditions. These findings not only provide a better understanding of nitrogen dynamics under the effect of unsteady channel flow, but also can be applied for river restoration to efficiently remove nitrate in the HZ by modifying river channel gradients.  相似文献