地籍管理适时变更系统（农村部分）试点工程可行性研究设想

对土地调查成果进行适时变更,是确保地籍成果的现势性和准确性的必要手段。如果采用传统工作方式,工作量大、时效低、费用高。本文针对双鸭山市实际情况,提出建立网络卫星定位服务系统,利用GPS进行外业数字采集,然后输入地籍数据变更终端系统,由系统自动进行变更。该技术优化了地籍管理变更工作流程,方便快捷、运行成本低廉,保证了地籍成果适时更新,具有现势性和可操作性。     

Simulation of permafrost changes on the Qinghai–Tibet Plateau,China, over the past three decades

ABSTRACT

Permafrost is one of the largest elements of the terrestrial cryosphere and is extremely sensitive to climate change. Based on mean annual ground temperature (MAGT) data from 189 boreholes on the Qinghai–Tibet Plateau (QTP), terrain factors, and climate data from China Meteorological Forcing Dataset, we propose a new mean annual ground air temperature (MAGAT) statistical model between meteorological parameters with subsurface temperatures to simulate permafrost distribution and variation of MAGT on the QTP over the past three decades (1981–2010). Validation of the model with MAGT data from 13 boreholes and permafrost maps of the QTP indicated that the MAGAT model is applicable to simulate the distribution and evolution of permafrost on the QTP. Simulation results show that the spatiotemporal MAGT of permafrost significantly increased by 0.37°C, or 0.25°C/10 yr, and the total area of permafrost decreased by 2.48?×?10⁵?km² on the QTP over the past three decades. Regionally, the changes of permafrost in the southwestern QTP were greater than other regions of the QTP.     

Early–Middle Ordovician conodont biofacies on the Yangtze Platform margin,South China: Applications to palaeoenvironment and sea-level changes

9172 Conodonts have been recovered from the uppermost Hunghuayuan Formation and the Zitai Formation at two sections in Shitai County, southern Anhui Province, South China, which was situated close to the margin of the Lower Yangtze Platform during the Early to Middle Ordovician. Systematic and multivariate statistical studies on these conodonts permit recognition of seven conodont biofacies: Tropodus biofacies, Diaphorodus biofacies, Oepikodus biofacies, Baltoniodus biofacies, Paroistodus biofacies, Periodon biofacies and Protopanderodus biofacies. Each biofacies is restricted to a particular lithofacies and stratal position and shows a consistent order and/or position within the succession. Turnover of these conodont biofacies is related to sea-level changes. The transgressive–regressive patterns demonstrated by the conodont biofacies compare closely to published sea level curves for South China, and highlight the utility of conodont biofacies as a means of confirming sedimentological evidence of relative sea-level change.     

珠江三角洲陈村钻孔剖面沉积特征及有机碳同位素古环境意义

陈村剖面位于佛山市陈村镇。AMS14C及OSL测年结果显示,剖面自晚更新世中晚期以来开始沉积,结束于全新世晚期,由老至新经历了河流相—河口湾相—三角洲相沉积环境。根据有机碳同位素曲线变化特征,结合孢粉、有孔虫等鉴定结果及沉积环境综合分析,将剖面划分为4个演化阶段:1晚更新世,34.15~24.5ka BP,属河流相沉积环境,δ13Corg平均值为-28.13‰,对应MIS 3期冷—稍湿气候,期间小幅波动;2晚更新世—全新世早期,24.5~9ka BP,属河流相沉积环境,δ13Corg平均值为-29.8‰,对应MIS 2期干冷气候及全新世早期温—干气候,YD事件得以记录;3全新世早—中期,9~6.7ka BP,属于河口湾—三角洲相沉积环境,δ13Corg平均值为-27.97‰,变化幅度小,对应暖—湿气候;4全新世中—晚期,6.7~0.44ka BP,属于三角洲相沉积环境,δ13Corg平均值为-26.94‰,变化幅度大,冷暖变化显著,气候特征为热湿—偏凉—暖干。     

Piezomagnetic In-situ Stress Monitoring and its Application in the Longmenshan Fault Zone

The relative change of in-situ stress is an inevitable outcome of differential movement among the crust plates. Conversely, changes of in-situ stress can also lead to deformation and instability of crustal rock mass, trigger activity of faults, and induce earthquakes. Hence, monitoring real-time change of in-situ stress is of great significance. Piezomagnetic in-situ stress monitoring has good and longtime applications in large engineering constructions and geoscience study fields in China. In this paper, the new piezomagnetic in-situ stress monitoring system is introduced and it not only has overall improvements in measuring cell＇s structure and property, stressing and orienting way, but also enhances integration and intelligence of control and data transmission system, in general, which greatly promotes installing efficiency of measuring probe and quality of monitoring data. This paper also discusses the responses of new piezomagnetic system in large earthquake events of in-situ stress monitoring station at Qiaoqi of Baoxing and Wenxian of Gansu. The monitoring data reflect adjustments and changes of tectonic stress field at the southwestern segment of and the northern area near the Longmenshan fault zone, which shows that the new system has a good performance and application prospect in the geoscience field. Data of the Qiaoqi stress-monitoring station manifest that the Lushan Earthquake did not release stress of the southwestern segment of the Longmenshan fault zone adequately and there still probably exists seismic risk in this region in the future. Combined with absolute in-situ stress measurement, carrying out long-term in-situ stress monitoring in typical tectonic position of important regions is of great importance for researchers to assess and study regional crust stability.     

Stable C and N isotope record of short term changes in water level in lakes of different morphometry: Lake Anastazewo and Lake Skulskie,central Poland

We present the stable C isotope record of the changes within the past 20 yr in water level of two morphologically different lakes in central Poland. The aim was to explain the relationship between lake water level and the δ¹³C signature of bulk sedimentary organic matter (δ¹³C_TOC) and to assess the potential of δ¹³C_TOC as a paleolimnological proxy of lake level change. This was done by comparison of the fossil δ¹³C_TOC record with instrumental data for lake level change in a shallow and small lake as well as in one large and deep basin. In both lakes the water table varied greatly between 1980 and 2000 AD. The δ¹³C_TOC data were supplemented with δ¹⁵N and bulk geochemistry data, as well as paleoecological data. We show that δ¹³C_TOC reacted to short term and low amplitude fluctuation in water level, but the response was highly dependent on the morphometry of the lake. In the shallow and small basin, δ¹³C_TOC decreased along with lake level drop due to oxidation and greater input of organic matter from macrophytes colonizing the lake bottom. On the contrary, in the deep/large lake δ¹³C_TOC decreased with increasing water level due to enhanced delivery of soil-derived OM to the lake during highstands. Our results have broad paleolimnological implications as they show that δ¹³C_TOC cannot act as a universal paleohydrological proxy. Its interpretation for a particular lake can be ambiguous and must be supported with additional geochemical and paleocological information.     

海洋沉积物细菌群落结构对芘和苯甲酸钠胁迫的响应

应用分子生态学方法, 研究在不同芳香族化合物胁迫下海洋沉积物中细菌群落结构的演替 规律。在实验室建立驯化系统, 在海洋沉积物中分别添加芘和苯甲酸钠, 采用Illumina MiSeq 高通量 测序技术分析实验组和对照组细菌群落16S rRNA 基因V3-V4 可变区数量的组成及变化, 研究沉积物 中添加芘、苯甲酸钠后, 微生物群落多样性和群落结构的变化。实验结果表明: 芘、苯甲酸钠极大地 降低了海洋沉积物中菌群丰度和多样性; 在添加苯甲酸钠的实验组, 变形杆菌门中海杆菌属 (Marinobacter)、假海源菌属(Pseudidiomarina)的细菌显著富集; 在添加芘实验组中拟杆菌门中的 Balneola 属、碳酸噬胞菌属(Aequorivita)极大富集。初步分析了在海洋沉积物环境中不同多环芳烃胁迫 下细菌群落结构的演替特征, 实验结果为海洋环境中针对不同芳香烃的微生物修复提供理论依据。     

Potential of future seismogenesis in Hebei Province (NE China) due to stress interactions between strong earthquakes

Northeast China, a densely populated area, is affected by intense seismic activity, which includes large events that caused extensive disaster and tremendous loss of life. For contributing to the continuous efforts for seismic hazard assessment, the earthquake potential from the active faults near the cities of Zhangjiakou and Langfang in Hebei Province is examined. We estimate the effect of the coseismic stress changes of strong (M ⩾ 5.0) earthquakes on the major regional active faults, and mapped Coulomb stress change onto these target faults. More importantly our calculations reveal that positive stress changes caused by the largest events of the 1976 Tangshan sequence make the Xiadian and part of Daxing fault, thus considered the most likely sites of the next strong earthquake in the study area. The accumulated static stress changes that reached a value of up to 0.4 bar onto these faults, were subsequently incorporated in earthquake probability estimates for the next 30 years.     

The structure and material composition of ossified aortic valves identified using a set of scientific methods

Degenerative aortic stenosis has become a common and dangerous disease in recent decades. This disease leads to the mineralization of aortic valves, their gradual thickening and loss of functionality. We studied the detailed assessment of the proportion and composition of inorganic and organic components in the ossified aortic valve, using a set of analytical methods applied in science: polarized light microscopy, scanning electron microscopy, X-ray fluorescence, X-ray diffraction, gas chromatography/mass spectrometry and liquid chromatography–tandem mass spectrometry. The sample valves showed the occurrence of phosphorus and calcium in the form of phosphate and calcium carbonate, hydroxyapatite, fluorapatite and hydroxy-fluorapatite, with varying content of inorganic components from 65 to 90 wt%, and with phased development of degenerative disability. The outer layers of the plaque contained an organic component with peptide bonds, fatty acids, proteins and cholesterol. The results show a correlation between the formation of fluorapatite in aortic valves and in other parts of the human bodies, associated with the formation of bones.