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1.
Through high-resolution research of sedimental chronology and the sediment environmental indexes,such as graininess ,minerals,magnetic parameters,pigment content organic carbon and chronology in Ds-core and Ws-core in Nansihu Lake,the authors analyze the formation cause of the Nansihu Lake and its water environmental changes,Historical documents are also analyzed here in order to reach the conclusion .Researches indicate that the Nansihu Lake came into being about 2500 aBP and its evolution succession can be divided into four stages.In this evolution process ,several scattered lakes merge into one large lake in the east of China,This process is distinctively affected by the overflow of the Yellow River,the excavation of the Grand Canal and other human activities. 相似文献
2.
乌兰布和沙漠北部全新世地貌演化 总被引：5，自引：2，他引：3
根据对乌兰布和沙漠北部地区全新世风沙和湖泊沉积记录及其沉积时代进行分析,认为全新世以来,乌兰布和沙漠北部地区地貌演化经历了4个主要的发育时期:Q33~Q41湖泊地貌发育时期,Q41风沙地貌发育时期,Q42湖(河)(屠申泽)地貌发育时期和Q43风沙地貌发育时期。全新世中期屠申泽最为繁盛的时期,湖泊相互沟通,范围几乎占据了整个乌兰布和沙漠北部地区,之后经历了自南向北的萎缩、分化过程,而屠申泽的萎缩、分化过程正是乌兰布和沙漠晚全新世风沙地貌发育并不断扩张的过程,这是一个以自然环境变化为主因、以人为影响为辅因的变化过程。 相似文献
3.
山东省南四湖湿地植被碳储量初步研究 总被引：5，自引：0，他引：5
湿地是全球重要的陆地碳库之一,对于全球变化的响应亦十分敏感。通过对南四湖湿地的野外实地调查并结合已有资料,对南四湖湿地的范围进行了重新定界,分析了湿地的植被类型和空间分布状况。通过对2006年6月份的SPOT5影像的解译,绘制了湿地景观格局图,计算了各种湿地景观类型的面积。结合公开发表的湿地植被生物量密度数据和相关参数计算出了整个南四湖湿地植被的碳储量为6.057 64×104t,并与1983年资料的折算数据对比发现南四湖湿地植被碳储量已减少了近3/4,表明南四湖湿地植被的碳汇能力已经明显减退。 相似文献
4.
In order to research the changing process of the pollution from the formation of Nansihu Lake, this study determined the isotope age and depositional rate and analyzed the organic geo-chemical quotas and heavy metal quotas of two sedimentary profiles of Weishan and Dushan lakes. Research results showed that from the formation of Nansihu Lake, the change of the pollution could be divided into four phrases. At the early phrase of the formation, the organic matters of the lake mainly derived from the exotic matters and had a close relation to the effect on the water and sands from the Huanghe (Yellow) River. At the middle and late phrases of the development, the endogenous matters of the lake became the main and stable source of the organic matters. The overflow of the Huanghe River, the excavation of the Grand Canal and the cut of trees caused the changes of the historic pollution. In recent 20 years, the modem industrial pollution from the organic matters and heavy metals has an increasingly heavy tendency. 相似文献
5.
In order to research the changing process of the pollution from the formation of Nansihu Lake, this study determined the isotope age and depositional rate and analyzed the organic geo-chemical quotas and heavy metal quotas of two sedimentary profiles of Weishan and Dushan lakes. Research results showed that from the formation of Nansihu Lake, the change of the pollution could be divided into four phrases. At the early phrase of the formation, the organic matters of the lake mainly derived from the exotic matters and had a close relation to the effect on the water and sands from the Huanghe (Yellow) River. At the middle and late phrases of the development, the endogenous matters of the lake became the main and stable source of the organic matters. The overflow of the Huanghe River, the excavation of the Grand Canal and the cut of trees caused the changes of the historic pollution. In recent 20 years, the modern industrial pollution from the organic matters and heavy metals has an increasingly heavy tendency. 相似文献
6.
灌丛沙堆的形成演化与区域气候环境密切相关,是古环境演化领域的重要研究对象。灌丛沙堆多发育于晚全新世以来,可靠的、高分辨率测年数据及地层沉积序列是其演化得以重建的关键,但其形成演化及年代学研究在技术手段方面尚没有新的突破,有关其不同发育阶段高分辨率的年代数据缺乏。围绕灌丛沙堆的发育过程、年代学、地层沉积序列及其形成演化与区域环境等方面,综述了近年来国内外灌丛沙堆已有的研究成果,认为灌丛沙堆各发育阶段与年代学关系、高分辨率年代结果及其形成演化在反映高原内陆盆地古风沙活动、古环境变化等方面的研究还有待深入。 相似文献
7.
The evolution and current state of landscapes around Lake Teletskoye have not previously been studied in detail. In the valley of the Malye Chily River, which flows into Lake Teletskoye, the timing of dam failure and draining of two moraine-dammed lakes has been identified. Botanical analysis, ash content determination, and radiocarbon dating of two peat profiles provide insight into postglacial evolution of wetlands related to this landscape. We found clear evidence of the disappearance from the peat of higher vascular species that, today, grows mostly in the plains of Siberia. Correlation of the data obtained with the accepted chronology of the Holocene events in the Russian Altai suggests the following stages of postglacial environmental change in the Malye Chily River valley: (1) the continuation of the Late Würm glaciation degradation (before 7000?cal. yr BP); (2) Holocene Climate Optimum (7000–5000?cal. yr BP); (3) Akkem cooling (5000–4200?cal. yr BP); (4) warm period (4200–3700?cal. yr BP); and (5) Historical cooling (3700–1600?cal. yr BP). 相似文献
8.
通过深入分析毛乌素沙地内北大池古城东侧一处包含人类活动层的沉积剖面的粒度参数,结合14C、OSL（光释光）测年和历史文献记载,本研究重建了北大池周边历史时期以来的环境及人类活动过程。结果显示:北大池湖泊在历史时期处于断续退缩过程之中,剖面北侧的河流水量一直减少。剖面中粗颗粒含量的变化与湖泊退缩和河流水量减少存在较好的相关性,剖面点周边地表沙丘出现的大致时间为明末,该结论与众多测年结果相符。该研究对理解毛乌素沙地环境变化的空间尺度具有较好的启示意义,同时在揭示沙漠化的内部环境变化过程中具有重要作用。 相似文献
9.
晚冰期以来河西走廊花海古湖泊演化过程及其对气候变化的响应 总被引：2，自引：0，他引：2
通过分析河西走廊花海古湖泊沉积物中的盐类矿物组成,结合年代序列,重建了花海晚冰期以来湖泊演化过程及其对气候变化的响应。结果表明：晚冰期及新仙女木时期,花海湖泊以芒硝沉积为主,属硫酸盐型湖泊,湖水的盐度较高且周期性波动频繁;全新世早期（10.47 cal ka BP以前）,湖泊以洪泛堆积和风成沉积为主,揭示了湖泊萎缩、甚至干涸;全新世早期至全新世中期（10.47～8.87 cal ka BP）盐类矿物以碳酸盐沉积为主,为碳酸盐型湖泊,湖水淡化,湖泊水位开始逐渐回升;全新世中期（8.87～5.50 cal ka BP）盐类矿物呈现一定的波动变化,其中,8.8 cal ka BP 时期盐类矿物以硫酸盐沉积为主,湖泊由碳酸盐型转化为硫酸盐型,湖水咸化,盐度升高;随后盐类矿物以碳酸盐沉积为主,湖泊由硫酸盐型转化为碳酸盐型,湖水盐度降低、湖泊扩张;全新世中晚期（5.50 cal ka BP以来）出现沉积间断,表明中晚全新世时期湖泊逐渐萎缩。在全新世期间,花海湖泊千年尺度演化过程揭示了该区域气候干湿状况受亚洲季风和西风共同控制的影响。 相似文献
10.
青海湖盆地因其独特的地理位置和气候环境,对气候变化响应敏感,是研究环境变化重要的场所。本研究在青海湖湖东沙地获取两个剖面,采用AMS14C测年,结合岩性、粒径组分和常量元素氧化物及其比值等多指标分析方法,重建了湖东沙地8.4 ka BP以来的环境演变过程。结果表明：除少量沉积物处于中等化学风化阶段外,大部分沉积物处于物理风化和初级化学风化阶段,说明自8.4 ka BP以来研究区气候环境总体上相对寒冷干燥。在千年尺度上,研究区不同时间段的气候环境存在较大的差异。8.4—4.2 ka BP气候相对温暖湿润;其中,8.4—6.2 ka BP河湖相和风成相沉积互层,表明存在明显的百年尺度气候波动;6.2—4.2 ka BP化学风化和淋溶作用较强,表明季风降水较多,径流较强,发育了较为稳定的湖泊沉积环境。4.2 ka BP以来湖泊消失,化学风化和淋溶作用减弱,沉积物从砾石转变为砂质黄土,显示气候较为冷干且波动较大。对比分析表明,中晚全新世以来青海湖湖东沙地的气候变化特征与东亚季风边缘区其他区域基本一致,并主导了区域沉积环境的演变过程。 相似文献
11.
南四湖湿地遥感信息分区分层提取研究 总被引：21，自引：0，他引：21
该文以南四湖区为试验区,利用TM数据,在对各地类光谱特征进行系统分析的基础上,提出了分区和分层相结合的湿地信息提取技术方法。根据研究区各种湿地类型的空间分布特点,将该区分为两个湿地类型区;在每一个区内,根据湿地的光谱特征进行分层提取,采用单红外波段阈值法、模型法以及改进的监督分类等技术方法。结果显示,该区湿地有14类,其中,自然湿地91119 51hm2,人工湿地122243 13hm2。 相似文献
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13.
本研究尝试使用钾长石多步升温红外后红外法 （MET-pIRIR） 对察尔汗盐湖北侧线形沙丘下伏古湖相沉积物进行年代测定,并初步探讨其古环境意义。结果表明：钾长石MET-pIRIR250法能够得到等效剂量坪区,说明长石信号能够充分晒退并且异常衰减对测年结果的影响可以忽略,从而保证了测年结果的可靠性;古湖相沉积顶部200—180 ka的年代证实了深海氧同位素7阶段柴达木盆地大规模湖泊的存在;上覆地层缺失表明即便在柴达木盆地沉积中心附近,地表沉积物的侵蚀（主要为风蚀）也十分严重,以至于在冰期尺度上也难保证连续性;这一年代结果也表明湖泊的演化并非造成线性沙丘较年轻（3—0 ka）的直接原因。钾长石MET-pIRIR法的应用对解决盆地内中、晚更新世古环境、古气候、地貌演化等问题具有重要意义。 相似文献
14.
Radar remote sensing can acquire information of sub-surface covered by sand in arid area, detect surface roughness and vegetation coronet's layer and linear feature such as linear structure and channel sensitively. With sediment facies analysis, this paper studies the features of environmental evolution in mid-late Epipleistocene (60 ka BP-20 ka BP) in northeastern Ejin Banner. The conclusions are listed as follows: (1) The evolution of the three lakes, i.e. Gaxunnur, Sugunur and Tian'e lakes, are dominated by faults and regional climate. (2) By analyzing sedimentary section of old Juyanze Lake, the three lakes used to be a large outflow lake before 50 ka BP in northeastern Ejin Banner, and at 50 ka BP, temperature declined rapidly in northwestern China. The event caused the lake's shrinkage. (3) By fault activity uplift in the northern part of old Juyan Lake and depression in the southern part, the lake's water followed from north to south at around 35 ka BP, old Juyanze fluvial fan was formed. At the same time, Juyan Lake separated from Sugunur Lake and Wentugunr old channel was abandoned. (4) In recent 2000 years, Ruoshui River is a wandering river, sometimes it flows into Juyan Lake and sometimes Sugunur and Gaxunnur lakes. Due to human activities and over exploitation, the oasis ecosystem is rapidly degenerated in 15 years (1986-2000). 相似文献
15.
长江沿江地区化工产业空间格局演化及影响因素 总被引：1，自引：1，他引：1
基于企业数据和空间计量方法,探讨了长江沿江地区2000—2013年化工产业空间格局演化及影响因素。结果表明：化工产业主要分布在上海市和江苏沿江地区;中上游部分地区化工产业呈现明显的增长势头,由3个主要热点区发展到20余个不同规模大小的分布热点,成为化工产业新兴“增长极”;城市主城区化工产业减少而远郊区县增加,分布热点变化也反映了化工产业“郊区化”“园区化”的过程;相对低端基础的行业呈现集聚趋势,其中肥料业集聚明显;相对高端精细的行业呈现扩散趋势,其中合成材料业分散化明显;地区化工产业增长受到环境规制、外商投资、交通区位等因素显著影响,外商投资和交通区位具有显著的促进作用,而环境规制呈现显著的抑制效果。 相似文献
16.
On paleodrainage evolution in mid-late Epipleistocene based on radar remote sensing in northeastern Ejin Banner,Inner Mongolia 总被引：2，自引：0，他引：2
WANGXinyuan GUOHuadong CHANGYueming ZHALiangsong 《地理学报(英文版)》2004,14(2):235-241
Radar remote sensing can acquire information of sub-surface covered by sand in arid area,detect surface roughness and vegetation coronet‘s layer and linear feature such as linear structure and channel sensitively. With sediment facies analysis, this paper studies the features of environmental evolution in mid-late Epipleistocene (60 ka BP-20 ka BP) in northeastem Ejin Banner. The conclusions are listed as follows: (1) The evolution of the three lakes, i.e. Gaxunnur, Sugunur and Tian‘e lakes, are dominated by faults and regional climate. (2) By analyzing sedimentary section of old Juyanze Lake,the three lakes used to be a large outflow lake before 50 ka BP in northeastem Ejin Banner, and at 50 ka BP, temperature declined rapidly in northwestem China. The event caused the lake‘s shrinkage. (3)By fault activity uplift in the northem part of old Juyan Lake and depression in the southem part, the lake‘s water followed fi‘om north to south at around 35 ka BP, old Juyanze fluvial fan was formed. At the same time, Juyan lake separated fi‘om Sugunur Lake and Wentugunr old channel was abandoned.(4) In recent 2000 years, Ruoshui River is a wandering river, sometimes it flows into Juyan lake and sometimes Sugunur and Gaxunnur lakes. Due to human activities and over exploitation, the oasis ecosystem is rapidly degenerated in 15 years (1986-2000). 相似文献
17.
可可西里盐湖湖水外溢可能性初探 总被引：5，自引：0，他引：5
2011年9月可可西里地区卓乃湖溃决后,关于盐湖湖水能否外溢进入楚玛尔河继而成为长江的最北源是公众及学界普遍关注的话题。本研究基于2010-2015年Landsat TM/ETM+/OLI遥感影像、SRTM 1弧秒数据、Google Earth高程数据和五道梁气象台站观测数据,首次对盐湖变化、湖水外溢条件及其可能性进行分析。结果表明：卓乃湖溃决后,盐湖在2011年10月至2013年4月期间面积急剧增加,之后湖泊进入稳定扩张期,2015年10月27日盐湖面积为151.38 km2,是2010年3月3日湖泊面积的3.35倍。盐湖发生湖水外溢的条件是湖泊面积达到218.90~220.63 km2。由于SRTM和Google Earth高程数据间的差异,盐湖湖水外溢时的水位将比当前高12 m或9.6 m,相应湖泊库容增加23.71 km3或17.27 km3,届时湖水将由湖泊东侧流入清水河流域。尽管盐湖在未来10年内不可能发生湖水外溢,但是随着盐湖集水区的扩大及预估的区域未来降水量的增加,在更长时间尺度内盐湖发生湖水外溢并成为长江支流的可能性依然存在。 相似文献
18.
洞庭湖地区农业功能时空演变的影响机制研究 总被引：4，自引：0，他引：4
农业功能的时空演变规律和影响因素研究是引导地区分工、凸显地域价值、促进区域协调发展的科学依据。以洞庭湖地区24个县市区为研究区域，分别从粮食生产功能、就业与社会保障功能、生态保育功能和旅游休闲功能构建评价指标体系，运用熵值法、农业功能变化时空差异诊断模型、地理探测器等方法模型对洞庭湖地区1997—2017年农业功能的动态变化过程、影响因素与作用机制进行研究。结果表明：① 1997—2017年洞庭湖地区农业功能时空变化特征显著：洞庭湖地区粮食生产功能整体呈增强趋势，且中部地区增强明显；就业与社会保障功能整体呈减弱变化趋势，市辖区尤为明显；生态保育功能整体呈减弱趋势且变化幅度大，石门县、安化县等丘陵地区减弱明显，而洞庭湖中部平原区域增强；旅游休闲功能整体呈增强变化态势，石门县、桃江县等地区以及各市辖区旅游休闲功能大幅度提升。② 农业发展基础是农业功能演变的决定性因素，地区发展水平是农业功能演变的重要因素，生产环境质量是洞庭湖地区农业功能演变的基础因素；地区发展水平对农业功能演变的影响程度逐渐上升，生产环境质量因素的影响程度逐渐下降；各影响因子之间存在交互作用，农业功能时空的演变过程及结构受到多个因子共同影响，说明洞庭湖地区农业功能演变的影响因素存在显著的复杂性特征。 相似文献
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20.
Radar remote sensing can acquire information of sub-surface covered by sand in arid area,detect surface roughness and vegetation coronet′s layer and linear feature such as linear structure and channel sensitively. With sediment facies analysis, this paper studies the features of environmental evolution in mid-late Epipleistocene (60 ka BP-20 ka BP) in northeastern Ejin Banner. The conclusions are listed as follows: (1) The evolution of the three lakes, i.e. Gaxunnur, Sugunur and Tian′e lakes, are dominated by faults and regional climate. (2) By analyzing sedimentary section of old Juyanze Lake,the three lakes used to be a large outflow lake before 50 ka BP in northeastern Ejin Banner, and at 50ka BP, temperature declined rapidly in northwestern China. The event caused the lake′s shrinkage. (3)By fault activity uplift in the northern part of old Juyan Lake and depression in the southern part, the lake′s water followed from north to south at around 35 ka BP, old Juyanze fluvial fan was formed. At the same time, Juyan Lake separated from Sugunur Lake and Wentugunr old channel was abandoned.(4) In recent 2000 years, Ruoshui River is a wandering river, sometimes it flows into Juyan Lake and sometimes Sugunur and Gaxunnur lakes. Due to human activities and over exploitation, the oasis ecosystem is rapidly degenerated in 15 years (1986-2000). 相似文献