青海盐湖镁资源开发与利用研究进展          下载免费PDF全文

毕秋艳  党力  曹海莲  高莉  郭强  柴克松  鲁云花  徐世爱 《盐湖研究》2021,29(1)

本文简要介绍了青海盐湖资源的分布、储量,重点对青海盐湖镁资源的研究开发和利用现状进行了综述,分析了其中存在的问题和关键技术瓶颈。在此基础上,对未来青海盐湖镁资源的高值化利用和研究方向进行了展望,并提出了相应的建议。  相似文献   

盐胁迫对枸杞(Lycium barbarum)叶片生理的影响     

张雯莉  刘玉冰  刘立超 《中国沙漠》2018,(2):294-299

枸杞(Lycium barbarum)耐盐碱能力强,在盐渍化土壤中种植枸杞具有一定程度改良土壤的功效。然而对枸杞在不同盐渍生境和不同盐渍化程度下的生理适应基础研究较少。选取扦插的"宁杞5号"一年实生苗为材料,分别在渗透势为-0.48、-0.82、-1.18 MPa下采用单盐(NaCl或Na_2SO_4)和混合盐NaCl+Na_2SO_4进行处理,对比分析不同处理时段内枸杞生理活性的响应。结果表明:随着渗透势降低,叶绿素(Chl)含量呈下降趋势;代表膜脂过氧化程度的丙二醛(MDA)、渗透调节物质脯氨酸(Pro)和可溶性糖(SS)含量明显增加;抗氧化酶系统超氧化物歧化酶(SOD)和过氧化氢酶(CAT)活性增加;渗透势为-1.18 MPa盐处理则抑制了过氧化物酶(POD)的活性。相同渗透势的不同盐处理之间,Chl、Pro、MDA和SS含量以及SOD和CAT活性在混合盐处理下或多或少都有增加;随着处理时间的延长,MDA、Pro、SS含量和CAT活性增加。这说明盐渍化程度增加,渗透调节物质和抗氧化酶系统的保护加强;不同盐渍环境下枸杞的生理响应不同,-1.18 MPa下混合盐胁迫相对于单盐影响更大;胁迫时间延长,渗透调节物质的累积增加,枸杞的适应性增强。  相似文献   

柴达木盆地盐湖周边灌丛沙丘微量元素特征与环境意义   总被引：2，自引：0，他引：2  

凌智永  陈亮  芦宝良  王建萍 《盐湖研究》2018,26(3):35-43

对柴达木盆地盐湖周边灌丛沙丘沉积物微量元素、粒度测试,并与其他体系沉积物对比,分析微量元素地球化学特征及环境状况。结果表明:1)微量元素以V、Cr、Zn、Rb、Sr含量较大,其中Sr含量最高,Rb次之;与中国黄土、新疆灰钙土相关系数R2为0. 96,斜率分别为1. 07和0. 99,含量总体相似; Sr、U高于灰钙土和黄土,其中,Sr含量表现为灌丛沙丘灰钙土黄土,Rb、Sn、Cs、Pb、Th含量介于二者之间,其余元素含量均低于二者;其与中国沉积层元素丰度存在差异。2) Sc、V、Co、Ni、Cu、Cs、U与黏粒(2μm)和粉砂(2～63μm)相关度均较高,而Ga、Rb、Pb主要受控于黏粒组分,Cr、Zn、Sr、Nb、Sn主要取决于粉砂组分; Y、Th与其他元素及不同组分无相关性; Rb/Sr比仅与Ga、Rb、Pb元素及 63μm的砂组分呈极显著正相关,与其余元素相关度低或不相关,或极显著负相关。3) Rb、Sr分别反映了沉积物近地化学风化成壤作用和源区物理风化过程; Sr/Cu值介于15～20之间,Th/U值介于3. 5～4之间,C. V值差异不大,元素垂直变异较小;总体表面灌丛沙丘沉积发育于极端干热环境,未发生明显还原作用。  相似文献   

湘澧盐矿卤水50 ℃等温蒸发析盐规律研究     

颜开  蔡晓琳  李瑞琴  王春连  廖磊  余小灿 《盐湖研究》2018,26(2):59-65

湘澧盐矿区位于江陵凹陷南缘,该地区卤水中溴和钾的含量都达到了工业品位。对采集的湘澧盐矿卤水样品进行了化学全分析,并对分析的结果进行了研究,查明了卤水中钾和溴等元素的富集机理;提出关于卤水综合利用的工艺路线及可行性建议。等温蒸发实验表明,整个蒸发过程中均有石盐析出,失水量达到31.23%时,芒硝开始析出;此后,石盐和芒硝共同析出。整个蒸发过程中该卤水的析盐规律为,首先析出氯化钠,再析出硫酸钠,最后析出硫酸钾。  相似文献   

岩土勘察与盐湖卤水矿产开发          下载免费PDF全文

颜辉 《盐湖研究》2018,26(3)

概要：本文通过对盐湖地区岩土类型复杂性及特性的叙述,分析了盐湖矿产开发中不良地质现象产生的原因和岩土条件对开发规模、工程布局、工程安全、经济效益等方面产生的影响。论述岩土工程勘察在盐湖矿产开发中的特殊地位和重要价值,总结出岩土勘察与盐湖卤水矿产开发的关系并提出盐湖岩土勘察方案的简单建议。  相似文献   

Architecture of the evaporite accumulation and salt structures dynamics in Tiddlybanken Basin,southeastern Norwegian Barents Sea     

Muhammad Hassaan  Jan I. Faleide  Roy H. Gabrielsen  Filippos Tsikalas 《Basin Research》2021,33(1):91-117

An extensive, reprocessed two‐dimensional (2D) seismic data set was utilized together with available well data to study the Tiddlybanken Basin in the southeastern Norwegian Barents Sea, which is revealed to be an excellent example of base salt rift structures, evaporite accumulations and evolution of salt structures. Late Devonian–early Carboniferous NE‐SW regional extensional stress affected the study area and gave rise to three half‐grabens that are separated by a NW‐SE to NNW‐SSE trending horst and an affiliated interference transfer zone. The arcuate nature of the horst is believed to be the effect of pre‐existing Timanian basement grain, whereas the interference zone formed due to the combined effect of a Timanian (basement) lineament and the geometrical arrangement of the opposing master faults. The interference transfer zone acted as a physical barrier, controlling the facies distribution and sedimentary thickness of three‐layered evaporitic sequences (LES). During the late Triassic, the northwestern part of a salt wall was developed due to passive diapirism and its evolution was influenced by halite lithology between the three‐LES. The central and southeastern parts of the salt wall did not progress beyond the pedestal stage due to lack of halite in the deepest evaporitic sequence. During the Triassic–Jurassic transition, far‐field stresses from the Novaya Zemlya fold‐and‐thrust belt reactivated the pre‐salt Carboniferous rift structures. The reactivation led to the development of the Signalhorn Dome, rejuvenated the northwestern part of the salt wall and affected the sedimentation rates in the southeastern broad basin. The salt wall together with the Signalhorn Dome and the Carboniferous pre‐salt structures were again reactivated during post‐Early Cretaceous, in response to regional compressional stresses. During this main tectonic inversion phase, the northwestern and southeastern parts of the salt wall were rejuvenated; however, salt reactivation was minimized towards the interference transfer zone beneath the centre of the salt wall.  相似文献   

The Cyclic Spectrum Analysis of IMFs of EMD and Its Application to Gravity Tide     

Quan Haiyan  Liu Yan 《地球科学进展》2016,31(9):919-925

IMFs sifted out by EMD are the FM-AM components. In the paper, by the cyclic spectrum analysis, IMFs are demodulated as the two periodic components which are identical to the intrinsic physical concepts. Using the method, the half-day-tide M₂, the day-tide O₁, and the half-month-tide M_f are extracted from the gravity tide signal, and a conclusion is drawn that the half-day-tide M₂ and the day-tide O₁ are primary components of gravity tide signal, and the half-month-tide M_f is modulated in the half-day-tide M₂ and the day-tide O₁.  相似文献   

吐鲁番盆地地下水与植被的关系研究          下载免费PDF全文

张晓  魏青军  刘亮 《山东国土资源》2016,32(7)

吐鲁番盆地是我国西部极端干旱地区的一个山间盆地,气候干旱、降雨稀少,荒漠生态典型,生态环境脆弱。文章从植被生长与土壤含水率、含盐量、地下水矿化度、埋深等方面进行分析,得出吐鲁番盆地艾丁湖周缘低湿地植被生态可持续发展的合理生态水位为埋深2.5~3.5 m。总结了吐鲁番盆地天然绿洲区的植被随地下水变化的关系及其演替模式。  相似文献   

Assessment of SARAL-ALTIKA Tidal Corrections in the Coastal Oceans Around India     

R. K. Nayak  M. Salim  S. K. Sasamal  P. C. Mohanthy  R. K. Bharadwaj  K. H. Rao 《Marine Geodesy》2016,39(5):331-347

The present tidal correction of sea level records of Satellite with ARgoes and ALtimeter (SARAL) is based on the finite element solution (FES) of global tide model FES2012 tidal solution. In this study, we examined the validity of the tidal corrections in the coastal oceans around India using tide gauge measurements and a regional tidal model. Our regional model is based on the barotropic version of the Princeton Ocean Model that is forced by the time-varying tidal levels at the open ocean end based on the global FES99 tidal solution. Tide charts prepared from the simulated tidal levels are very similar to the FES tidal solutions. Comparison with the tide gauge measurement shows close agreement with the regional tidal solutions. On the other hand, the agreement with the FES tide models differ significantly in the Gulf of Khambhat and the Gulf of Kutch on the northwest, and in the Hooghly estuary on the northeast continental shelf. However, the agreement is exceptional in other parts of the study domain. These tidal solutions are used in the SARAL-ALTIKA X-track data to assess the FES tidal correction and to draw some inferences associated with the coastal processes. It is revealed that these corrections are reasonably accurate for the coastal oceans around India except the aforementioned converging channels.  相似文献   

基于FVCOM的台湾海峡三维潮汐与潮流数值模拟研究          下载免费PDF全文

王道生  刘晓东  庄海东 《应用海洋学学报》2016,35(4):491-498

基于FVCOM海洋数值模式,采用非结构三角形网格较好地刻画了台湾海峡复杂的岸线边界及海底地形,建立了台湾海峡的三维潮汐潮流数值模型.模拟结果同长期观测资料符合良好,较好地反映出台湾海峡内潮汐、潮流运动的变化状况和分布特征,利用T_tide工具包进行水位潮流调和分析给出了M2、S2、K1、O1四个主要分潮的同潮图、表层潮流椭圆分布.分析表明,M2分潮由台湾岛南北两端传入台湾海峡,两支潮波在澎湖—台湾浅滩南缘相遇,呈NE—SW向倾斜,振幅最大值为2.45m,出现在福建省湄洲湾、兴化湾一带.K1分潮潮波由东北向西南传入,并向南海传播,传播方向上右侧振幅较左侧大0.05m.台湾海峡存在一条分潮潮流椭圆率为0的分隔线,该分隔线大致呈NE—SW走向,分隔线上半部分潮流椭圆旋转方向为逆时针方向,下半部分为顺时针方向.四个主要分潮潮流椭圆长轴基本呈NE—SW走向,但在台湾浅滩表层潮流椭圆长轴方向为NW—SE向,澎湖水道呈N—S向.台湾浅滩处四个分潮的潮流椭圆均较大,对应的潮流也强,可能受当地水深较浅的影响.  相似文献