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1.
主要调查环渤海湿地的盐地碱蓬对碳、氮、磷的吸收通量。调查表明,环渤海湿地的盐地碱蓬面积为7 397 hm2。2009年7月、10月和11月盐地碱蓬总生物量(干重)分别为2.104×104t、2.615×104t和1.523×104t。7月、10月和11月,盐地碱蓬对碳的吸收通量分别为6 577 t、8 538 t和5 713 t;对氮的吸收通量分别为201.2 t、278.6 t、177.7 t;对磷的吸收通量分别为17.00 t、32.40 t、16.60 t;盐地碱蓬对碳、氮、磷的最大吸收通量均为10月。 相似文献
2.
盐胁迫对不同生境种源盐地碱蓬幼苗生长、光合色素及渗透调节物质的影响 总被引：2，自引：0，他引：2
《海洋湖沼通报》2017,(1)
为探讨盐地碱蓬(suaeda salsa)适应不同生境的生理机制,研究了不同盐分处理(0、200和400mmol/L的NaCl;0、200和400mmol/L的KCl)对盐碱地和潮间带生境盐地碱蓬地上部分鲜重、干重、肉质化程度、光合色素及渗透调节物质的影响。结果表明:200mmol/L的NaCl处理使盐地碱蓬的地上部鲜重、干重、肉质化程度显著增加,400mmol/L的NaCl处理和两种浓度的KCl处理均使盐地碱蓬的鲜重、干重、肉质化程度显著降低;NaCl和KCL处理均使碱蓬的叶绿素含量显著降低,但使叶绿素a/b的值显著提高;NaCl和KCl处理使盐地碱蓬有机酸含量呈降低趋势,但使脯氨酸含量显著增加;200mmol/L的NaCl和KCl处理使碱蓬的可溶性糖含量显著增加,而400mmol/L的NaCl和KCl处理则其显著降低;潮间带生境盐地碱蓬的地上部鲜重、干重、肉质化程度、叶绿素a和叶绿素b含量显著低于盐碱地生境;钾盐对盐地碱蓬的胁迫效应显著大于钠盐;盐碱地生境碱蓬对盐分胁迫的响应显著高于潮间带生境。 相似文献
3.
AGO蛋白(Argonature protein)作为RNA诱导沉默复合物的核心元件,在植物的非生物胁迫过程中发挥着重要作用。以前期获得的盐地碱蓬转录组数据为基础,开展了针对盐地碱蓬(Suaeda salsa)AGO蛋白的生物信息学及盐胁迫下的表达规律研究。采用RACE技术克隆2个AGO基因家族成员(SsAGO1、SsAGO16)的cDNA全长序列,并对其蛋白结构、进化关系、表达模式等进行分析。结果表明:盐地碱蓬2类AGO蛋白家族成员基因长度分别为3 212 bp和3 766 bp,编码的蛋白均是一个无跨膜结构域、无信号肽的亲水性蛋白,α-螺旋散布于每个蛋白质的整体结构中;SsAGO1和SsAGO16都含有一个未知的结构域DUF1785,除此之外,SsAGO1还含有PAZ和PIWI两个特征结构域,而SsAGO16仅含有PIWI结构域,SsAGO1和SsAGO16亲缘关系较远,且具有不同的时空表达模式。首次从盐地碱蓬鉴定了AGO蛋白基因并进行了盐胁迫下的表达规律分析,为研究AGO蛋白家族在盐生植物耐盐生理过程中的作用奠定了基础。 相似文献
4.
种植盐地碱蓬修复滨海盐渍土效果的研究 总被引：25，自引：0，他引：25
利用盐生植物——盐地碱蓬进行天津河口滨海盐碱地的生物修复。通过比较种植盐地碱蓬土壤和对照土壤的电导率、有机质和微生物数量的差异等研究了其修复效果。结果表明，种植区碱蓬根际土壤的电导率与对照土壤相比下降了13％；有机质和总氮与对照土壤相比分别增加43％和18％；根际土壤的微生物数量明显增加，放线菌和真菌分别比对照增加了5倍和16倍。根际微生物优势种群的盐耐受性结果显示，部分根际土壤的优势种群的盐耐受性明显下降，耐盐性较低的微生物种群已成为优势种群。以上结果表明，种植盐地碱蓬对改善滨海盐碱地的生态有明显的效果。 相似文献
5.
主要调查环渤海湿地的盐地碱蓬对碳、氮、磷的吸收通量.调查表明,环渤海湿地的盐地碱蓬面积为7397 hm2.2009年7月、10月和11月盐地碱蓬总生物量(干重)分别为2.104× 104t、2.615×104t和1.523×104t.7月、10月和11月,盐地碱蓬对碳的吸收通量分别为6577 t、8538 t和5713 t;对氮的吸收通量分别为201.2 t、278.6 t、177.7 t;对磷的吸收通量分别为17.00 t、32.40 t、16.60 t;盐地碱蓬对碳、氮、磷的最大吸收通量均为10月. 相似文献
6.
建立药用耐盐植物盐地碱蓬(Suaeda salsa)的HPLC指纹图谱。运用DAD-Agilent 1100高效液相色谱仪,色谱条件:Agilent Zorbax XDB C18柱(4.6 mm×250 mm;5.0μm)色谱柱,1.0 mL.min-1流速,320 nm检测波长,360 nm参比波长,10μL进样量,30℃柱温,乙腈(A)-0.1%磷酸水(B)梯度洗脱。建立了盐地碱蓬的HPLC指纹图谱,包含16个共有峰,指纹图谱特征明显,化学信息完整。方法的系统适应性测定结果符合指纹图谱的技术规范。结论:首次建立的盐地碱蓬HPLC参考指纹图谱可用于盐地碱蓬的快速真伪鉴别。 相似文献
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文章依据2021年9月黄河口盐沼湿地沉积物调查数据,分析了沉积物粒度、容重、有机碳分布特征,并对黄河口盐沼湿地沉积物碳密度及碳储量进行评估。结果显示,黄河口盐沼湿地沉积物类型以粉砂为主,部分层次为砂质粉砂和黏土质粉砂;4种植被类型中,不同深度的沉积物容重差异性不大,互花米草和盐地碱蓬分布区容重整体大于柽柳和芦苇分布区;互花米草、盐地碱蓬、芦苇和柽柳分布区沉积物中有机碳含量分别为0.199%、0.200%、0.184%和0.161%,互花米草和盐地碱蓬分布区底质中有机碳含量较芦苇和柽柳分布区偏高,这与互花米草和盐地碱蓬分布区含有更多的黏土组分有关;计算得出,黄河口盐沼湿地沉积物总碳储量为33.47万t,其中互花米草分布区为14.31万t,芦苇分布区为12.05万t,柽柳分布区为5.27万t,盐地碱蓬分布区为1.84万t。 相似文献
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以纠正碱蓬属Suaeda盐生植物研究中广泛存在的分类错误为目的,针对碱蓬属研究中因缺乏正确的种属鉴定与使用错误种名等导致无法确定研究对象是何植物,使研究结果丧失确定性和科学价值的问题,通过对相关错误文献的梳理,对包括《中国高等植物图鉴》在内的有关碱蓬属植物研究文献进行了初步分析,指出了有关碱蓬属植物研究中的同物异名、同名异物以及中文名与拉丁名错乱等问题并予以纠正。对提高碱蓬属植物研究的科学性与可靠性具有重要参考价值。 相似文献
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《海洋湖沼通报》2020,(1)
植物冠层反射光谱与叶片叶绿素含量密切相关。以滨海湿地生态修复的重要植物碱蓬为研究对象,采用盆栽控盐试验研究了碱蓬在盐胁迫条件下叶片叶绿素含量以及冠层反射光谱的响应特征,利用单因素方差分析(one-way ANOVA)和事后检验(Dunnett)相结合的方法分析了叶片叶绿素含量与一阶微分冠层光谱反射率之间的响应关系,以对碱蓬叶片叶绿素含量敏感的波段构建比值光谱指数和归一化光谱指数,并识别出对碱蓬叶片叶绿素含量响应显著的高光谱指数。研究结果表明:50 mmol/L盐胁迫下,碱蓬叶片叶绿素含量最高,当盐胁迫大于50 mmol/L时会抑制碱蓬的光合作用;在可见光波段范围(400-700 nm),中度(300-400 mmol/L)与高度(600 mmol/L)盐胁迫下,碱蓬冠层光谱反射率随叶片叶绿素含量的增加而降低;在不同盐胁迫条件下,543 nm、645-647 nm、663 nm、667 nm、669-670 nm、682 nm、686-687 nm等波段处的一阶微分光谱与叶绿素含量的响应最为显著(p0.05);利用反射率差值法确定对碱蓬叶片叶绿素含量敏感的高光谱指数的参数D_(543)、D_(645)、D_(663)、D_(667)、D_(682)、D_(686)、D_(687),发现比值光谱指数D_(543)/D_(663)、D_(543)/D_(682)、D_(645)/D_(663)和归一化光谱指数(D_(543)-D_(667))/(D_(543)+D_(667))、(D_(645)-D_(667))/(D_(645)+D_(667))、(D_(645)-D_(682))/(D_(645)+D_(682))在盐胁迫下对叶片叶绿素含量的响应较为显著(p0.01),多重判定系数r~2均在0.995以上,其中比值光谱指数D_(543)/D_(682)的显著性最好,多重判定系数r~2高达0.998。盐胁迫下碱蓬叶片叶绿素含量的高光谱指数识别可为探讨滨海湿地盐地碱蓬滩退化和生态修复的高光谱响应机理研究提供理论参考。 相似文献
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黄须菜,即盐地碱蓬,藜科(Sueada Salsa Pau),一年生草本,高20～100厘米;茎直立或斜向上,通常基部分枝,无梗。分布于山东、河北、天津、江苏、山西等省市的盐碱地的盐地碱蓬,系盐碱地的指示植物。耐碱、耐旱、耐涝,适盐范围在3％左右。可形成单优势种植物 相似文献
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《Marine and Petroleum Geology》2012,38(1):195-208
Rowan et al. (2012) vehemently argue that salt tectonics is entirely driven by differential sedimentary loading and refute all the results of our work (Brun and Fort, 2011) showing that salt tectonics on passive margins is dominated by gliding, which we referred to in our paper as “dominant gliding”; in other words the deformation is controlled by salt flowing down the regional dip of these margins. We point out that “pure spreading” would be driven by differential sedimentary loading only if margins could remain strictly horizontal (i.e. not tilted), whereas “dominant gliding”, which combines spreading and gliding, affects sedimentary successions above salt layers on passive margins as soon as these are titled. Our work shows that the fundamental dynamic difference between the two processes is that in “pure spreading” salt resists deformation whereas in “dominant gliding” salt drives deformation. In “dominant gliding”, even in absence of sediments, salt flows down dip with a component of spreading, demonstrating that differential sedimentary loading is not a necessary condition of salt tectonics and that spreading – i.e. layer parallel stretching- does not require sedimentation to occur. Rowan et al. (2012) put forward arguments, related to thrust mechanics and deduced from some “pure spreading” sand and silicon box models, to backup their claims about “pure spreading” but none of them is applicable to salt basins at margin-scale. The objections made by Rowan et al. (2012) about shelf break migration and slope deformation in the Gulf of Mexico are not substantiated nor justified by verifiable and validated data. Using an adequately scaled laboratory sand-silicone box experiment, in which sedimentary progradation is oblique to silicone (salt) flow, we show that transfer zones develop with directions close to silicone (salt) flow and define patterns directly comparable to those observed in the northern Gulf of Mexico. This paper documents the results of a review of all the arguments and statements contradicting the results of our work put forward in Rowan et al. (2012), and suggests that none of them is valid. 相似文献
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Yixin Yu Xinhuai Zhou Liangjie Tang Wenxu Peng Dingyou Lu Weiguo Li 《Marine and Petroleum Geology》2009,26(8):1600-1607
Using the new high-quality 3D seismic data, this paper addresses the salt structures in the KL11 area of the Laizhouwan depression in the southern offshore Bohai Bay basin. In the study area, the salt in the Sha-4 Member of the Paleogene Shahejie Formation thickened, and then formed an S–N trending salt wall, which changes shape regularly along its trend from salt diapir to salt pillow. The change in thickness of the suprasalt layers record five growth phases of the salt wall from the Eocene to the Quaternary: (1) early diapirism, (2) active diapirism, (3) passive diapirism, (4) relative structural quiescence, and (5) arching. The evolution of the salt structures was mostly governed by the multi-phase compression induced by the dextral strike-slip of the Tan–Lu fault, which formed a restraining bend in the study area. There was an original passive stock in the south, which was later tectonically squeezed by E–W compression and became a diapir. As the shortening propagated to the north from the original stock, the salt pillow was created in the north. Relative structural quiescence then followed until the next phase of compression, which arched the thick roof of the salt wall. 相似文献
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Using the seismic profiles and analog modeling, this paper addresses the salt structures in the M and B blocks in the Southern Precaspian Basin. The salt structural features, the formation mechanism and the controlling factors of structural deformation are investigated and discussed systematically. The interpretation of the seismic profiles shows that typical salt-related structures include salt wall, (flip-flop) salt diapir, salt roller, salt pillow (dome), salt weld, salt withdrawal minibasin and drag structure (or drape fold). In addition, model results demonstrate that the gravity spreading driven by progradation and aggradation is probably the primary factor in controlling the formation of the salt structures in the research area. Due to the differential loading driven by progradation, passive salt diapir developed near the progradational front followed by the formation of intrasalt withdrawal minibasin bounded by two salt diapirs, and secondary reactive triangle salt diapir or salt pillow might form within the intrasalt withdrawal minibasin. Model results also indicate that the pattern of the subsalt basement has important influence on the formation and evolution of salt structures. Salt diapirs primarily developed along the margin of the subsalt uplift basement, where high shear deformation was induced by differential sedimentary loading between the uplift area and the slope area. 相似文献
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A marine controlled source electromagnetic (CSEM) campaign was carried out in the Gulf of Mexico to further develop marine electromagnetic techniques in order to aid the detection and mapping of gas hydrate deposits. Marine CSEM methods are used to obtain an electrical resistivity structure of the subsurface which can indicate the type of substance filling the pore space, such as gas hydrates which are more resistive. Results from the Walker Ridge 313 study (WR 313) are presented in this paper and compared with the Gulf of Mexico Gas Hydrate Joint Industry Project II (JIP2) logging while drilling (LWD) results and available seismic data. The hydrate, known to exist within sheeted sand deposits, is mapped as a resistive region in the two dimensional (2D) CSEM inversion models. This is consistent with the JIP2 LWD resistivity results. CSEM inversions that use seismic horizons provide more realistic results compared to the unconstrained inversions by providing sharp boundaries and architectural control on the location of the resistive and conductive regions in the CSEM model. The seismic horizons include: 1) the base of the gas hydrate stability zone (BGHSZ), 2) the top of salt, and 3) the top and bottom of a fine grained marine mud interval with near vertical hydrate filled fractures, to constrain the CSEM inversion model. The top of salt provides improved location for brines, water saturated salt, and resistive salt. Inversions of the CSEM data map the occurrence of a ‘halo’ of conductive brines above salt. The use of the BGHSZ as a constraint on the inversion helps distinguish between free gas and gas hydrate as well as gas hydrate and water saturated sediments. 相似文献
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The Ukrainian Dniepr-Donets Basin (DDB) is a Late Palaeozoic intracratonic rift basin, with sedimentary thicknesses up to 19 km, displaying the effects of salt tectonics during its entire history of formation, from Late Devonian rifting to the Tertiary. Hundreds of concordant and discordant salt structures formed during this time. It is demonstrated in this paper that the variety of styles of salt structure formation in the DDB provide important constraints on understanding the triggering and driving mechanisms of salt kinematics in sedimentary basins in general. Salt movement in the DDB began during the Devonian syn-rift phase of basin development and exerted controls on the later distribution of salt structures though the geometry of basement faults is not directly responsible for the regular spacing of salt structures. Post-rift salt movements in the DDB occurred episodically. Episodes of salt movement were triggered by tectonic events, specifically two extensional events during the Carboniferous, an extensional reactivation at the end of Carboniferous–earliest Permian, and a compressional event at the end of the Cretaceous. Extensional events that induced salt movement were ‘thick-skinned’ (i.e. basement involved in deformation) rather than ‘thin-skinned’. Most overburden deformation related to salt movements is ductile regardless of sedimentary bulk lithology and degree of diagenesis, while the deformation of sedimentary cover in areas where salt is absent is mainly brittle. This implies that the presence of salt changes the predominant mode of deformation of overlying sedimentary rocks. Episodes of salt movement lasted longer than the periods of active tectonics that initiated them. Buoyancy, erosion, and differential loading all played a role in driving halokinesis once tectonic forces had pushed the salt-overburden system into disequilibrium; among these factors, erosion of overburden above growing salt structures acted as a key self-renewing force for development of salt diapirs. Very high sedimentation rates (related to high post-rift tectonic subsidence rates), particularly during the Carboniferous, were able to bury diapirs and to load salt bodies such that buoyancy, erosion, and differential loading forces eventually became insufficient to continue driving diapirism—until the system was perturbed by an ensuing tectonic event. In contrast, some salt anticlines and diapirs developed continuously during the entire Mesozoic because of much-reduced tectonic subsidence rates (and sedimentation supply) during this time. However, a Lower Permian salt series and overhangs of buried diapirs played an important role in preventing overburden piercing (and fracturing) during the Mesozoic and, specifically, during the Late Cretaceous salt diapirism phase. 相似文献
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加蓬海岸盆地主要分为南加蓬次盆和北加蓬次盆,是典型的西非被动大陆边缘含盐盆地,盐岩的分布具有一定规律性和差异性,并且对盆地内油气成藏具有重要的控制作用。分析了加蓬海岸盆地的构造演化与沉积充填特征、基本石油地质条件、盐岩的分布特征及其对盆地烃源岩特征、储层分布、圈闭特征、封盖条件、油气成藏,以及油气藏储量等各方面的影响与控制作用,并指出,由于加蓬海岸盆地的绝大多数油气成藏都与盐岩密不可分,因此深化盆地内盐岩展布特征的研究,对进一步评价北加蓬次盆的盐下层系及南次盆登泰尔地堑的勘探潜力具有重要意义。 相似文献
17.
Jia He 《Marine Georesources & Geotechnology》2017,35(3):441-445
Salt in soil can cause cementation effect and increase the shear strength and stiffness of soil during the drying process. In this paper, an experimental study is presented to explore the strength, stiffness, and particle level structure of a salt-cemented sand at the dry state. Unconfined compression tests were carried out on sands with various amounts of precipitated dry salt. Scanning electron microscopic and elemental analysis were also conducted. The study shows that the strength and stiffness of sand can increase significantly with salt content. The strength versus salt content curve displays a convex shape, instead of a concave shape as found in cemented or biocemented sands. This implies that the effect of dry salt on soil strength is strong at low levels of salt content. The microscopic and elemental analysis evidences that salt tends to precipitate at particle contacts and form bridges between particles at relatively low salt content. The results presented in the paper may explain why even small amount of salt can lead to an overestimation of soil strength. 相似文献
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报道利用盐化工废弃物高低温盐制取无机阻燃剂氢氧化镁和具有广泛用途的氟硅酸钠的几种新方法。本文采用沉淀法，使高低温盐中的Ｍｇ２＋、Ｎａ＋得以有效的利用，其利用率可达１００％ 相似文献