柴达木盆地盐湖卤水及其沉积物硼同位素地球化学研究进展

综述了柴达木盆地盐湖卤水及其沉积物的硼同位素研究成果,并从pH值、离子浓度、物源补给等几方面对盐湖卤水及其沉积物的硼同位素组成进行了探讨。强烈的蒸发作用可以导致盐湖卤水的pH值降低,从而使δ¹¹B值相应地升高;卤水中的B可能会随碳酸盐的析出而进入到固相中,因此Ca²⁺浓度和Ca/Cl比值较高的湖泊,其卤水的δ¹¹B值一般都比较高;盐湖卤水及其补给水源的δ¹¹B值与B/Cl比值具有中等程度的负相关关系,这种特性也可以用来指示河水中硼的来源;当易风化的硅酸盐矿物经剥蚀迁移并最终在湖泊中沉积时,盐湖沉积物的δ¹¹B值会因这些低δ¹¹B值的物源加入而变低;此外,强烈的化学风化会使湖泊中沉积较多的细粒粘土矿物,由于粘土矿物的吸附作用也会使得盐湖沉积物中的δ¹¹B值偏低。关于柴达木盆地盐湖硼同位素的研究,不仅可以为盐湖的形成、演化及成盐成矿规律的研究提供可靠依据,而且可以为盐湖资源评价及合理开发提供科学依据。     

东海南部海域夏秋季沿岸流特征

Current characteristics and vertical variations during summer and autumn in the southern East China Sea were investigated by measuring current profile, tide, wind, and wave data for 90 d from July 28 to October 25, 2015. Our results are:(1) The current was mainly a(clockwise) rotating flow, displaying reciprocating flow characteristics,and vertically the current directions were the same throughout the vertical profile.(2) The horizontal current speed was strongest during August(summer) with an average speed of 51.8 cm/s. The average current speeds during spring tides were highest in August and weakest in September, with speeds of 59.9 and 42.8 cm/s,respectively.(3) Considerable differences exist in average current speeds in different layers and seasons. The highest average current speeds were found in the middle–upper layers in August and in the middle–lower layers in September and October.(4) The residual current speed was highest in August, when the speed was 12.5–47.1 cm/s,whereas the vertical average current speed was 34.3 cm/s. The depth-averaged residual current speeds in September and October were only 50% of that in August, and the residual current direction gradually rotated in a counter-clockwise direction from the lower to surface layers.(5) Typhoon waves had a significant influence on the currents, and even affected the middle and lower water layers at depths of >70.0 m. Our results showed that the currents are controlled by the dynamic interplay of the Taiwan Warm Current, incursion of the Kuroshio Current onto the continental shelf, and monsoonal changes.     

临朐县土地开发整理见实效

临朐县土地总面积1834km^3,山地丘陵占全县土地总面积的87％。1999年国土资源部把临朐县设立为首批全国土地开发整理示范区之一,8年来,临朐县委县政府狠抓山区土地开发整理不放松,先后建设国家级土地开发整理项目2个,省级项目8个,市级项目20个,共开发整理土地2．33万hm^2,增加耕地0．47万hm^2,项目区农业、林果业生产能力提高1．2倍,农民人均纯收入翻了一番。     

莱芜市做好土地开发整理工作

莱芜市地处鲁中山区,地形以山区、丘陵为主,有“六山一水三分田”之说,人均耕地只有0．054hm2（0．82亩）,是全省人均耕地最少的市之一。近年来,莱芜市从人多地少的市情出发,不断强化宣传引导,完善政策措施,加大资金投入,加强项目管理,全面推进土地开发整理工作。自2000年以来,全市市级以上累计投入专项资金3．9亿元,开发整理复垦各类土地3．93万hm2,增加耕地0．98万hm2,改造中低产田1．07万hm2,在增加有效耕地面积、提高耕地质量、保障占补平衡、改善农业生产条件和生态环境、促进农村发展、农业增效、农民增收等方面取得了显著成效。     

临朐山旺古动物群简介

山旺国家自然保护区于1980年国务院批准公布,面积1．2km2,位于临朐县城东22km处,该区为玛珥湖,蕴藏古生物化石丰富,种类繁多,目前已发现10多个门类700多种,形成于新近纪中新世,距今约1800万年。     

Fine-grained Pleistocene deepwater turbidite channel system on the slope of Qiongdongnan Basin, northern South China Sea

Recently, as oil exploitation has become focused on deepwater slope areas, more multi-channel high resolution 2D and 3D seismic data were acquired in the deepwater part of the Qiongdongnan Basin, northern South China Sea. Based on 3D seismic data and coherence time slice, RMS and 3D visualization, a series of deepwater channels were recognized on the slope that probably developed in the late Quaternary period. These channels trend SW–NE to W–E and show bifurcations, levees, meander loops and avulsions. High Amplitude Reflections (HARs), typical for channel–levee complexes, are of only minor importance and were observed in one of the channel systems. Most of the detected channels are characterized by low-amplitude reflections, and so are different from the typical coarse-grained turbidite channels that had been discovered worldwide. The absence of well data in the study area made it difficult to determine the age and lithology of these channels. Using a neighboring drill hole and published data about such depositional systems worldwide, the lithology of these channels is likely to be dominated by mudstones with interbedded thin sandstones. These channels are formed by turbidity currents originated from the little scale mountain river of mid-Vietnam in SW direction and were probably accompanied by a relative sea level drop in the last glacial age. These channels discovered on the northern South China Sea slope are likely to be fine-grained, mud-dominant and low N:G deposits in a deepwater paleogeographic setting.     

JCZ-1T超宽频带地震计作为综合观测仪器的拓展应用

JCZ-1T超宽频带地震计具有全频带覆盖特性,其低频端输出延伸到固体潮汐,提出了获取稳定的低频端数据的观测条件.利用地震计LP通道连续观测数据中的垂直分向数据经过处理获得的重力资料,以及水平分向数据经过处理获得的倾斜资料做了Venedikov调和分析.对印尼8.7级大地震数据进行处理,获得地球自由振荡的功率谱密度.仪器可获取与地震事件密切相关的综合观测数据.     

Forward modeling of tight sandstone permeability based on mud intrusion depth and its application in the south of the Ordos Basin

Permeability is an important index in reservoir evaluation,oil and gas accumulation control,and production efficiency.At present,permeability can be obtained th...     

土地调查中有关城镇与农村土地面积问题的研究

第二次全国土地调查工作中,城镇与农村地区的土地面积在计算方法上有所不同：农村地区的土地面积是以椭球面为基准的面积,即球面面积;城镇地区的土地面积是以平面为基准的面积,即平面面积。二者之间存在差异并按一定规律变化,当调查区处于投影带边缘附近时,同一图斑的球面面积与平面面积之间的差异达到最大。由于采用不同的计算方法而导致面积数量的差异,在进行农村与城镇有关土地数据整合时会出现矛盾。为了建立城乡统一的土地管理信息系统,保证土地面积的一致性,应当采取相应措施消除二者之间的差异。     

2008年初呼和浩特地区持续低温、降雪成因分析

利用常规气象观测资料、以及国家气候中心的海温监测资料等,对2008年初呼市地区出现低温降雪天气的强度、范围、持续时间和灾害影响作了初步分析,并与历史同期进行了比较。分析表明:此次低温降雪天气是在近年来最严重的一次"拉尼娜"事件背景下发生的,与欧亚地区持续大气环流异常密切相关,在"北脊南槽"和西太平洋副高偏北偏强的形势下,北方冷空气不断南下,同时印度洋和孟加拉湾暖湿气流源源不断地往北到东北方向输送,冷暖气流在我国中东部地区频繁交汇,造成了我市持续低温、降雪异常偏多。