基于沉积微相的野外露头剖面准层序分析——以鄂尔多斯盆地奥陶系临汾晋王坟剖面马家沟组为例

鄂尔多斯盆地奥陶系为广泛的陆表海碳酸盐岩沉积,其东部马家沟组岩相特征、岩石组合类型和旋回性丰富多样。通过对本区临汾晋王坟剖面的奥陶系马家沟组地层进行精细测量,笔者从剖面的沉积特征入手,进行沉积环境和沉积微相的分析,并以沉积微相的纵向演变规律为基础,结合准层序向上变浅的本质特征,识别划分野外露头剖面的准层序。研究区马家沟组共识别出32个准层序,可分为两种类型:准层序类型Ⅰ跨越若干微环境,相变向上为浅;准层序类型Ⅱ沉积于同一个微环境,向上有层厚的渐变趋势。两种类型准层序的形成取决于沉积物供给、短周期海平面升降和地层沉降三者之间的关系和相互作用。研究区内的准层序类型Ⅰ发育广泛,较为常见,类型Ⅱ则发育较少。     

Variation of groundwater hydrochemical characteristics in the plain area of the Tarim Basin,Xinjiang Region,China

Groundwater hydrochemistry could reveal the interaction mechanism between groundwater and the environment, which provides a scientific basis for environmental resources management. In this study, Shukaliefu’s classification method and Piper diagram were adopted to determine the hydrochemical types of groundwater in the Tarim Basin of Xinjiang, China. The method of “one^-vote veto” was applied to evaluate the quality of groundwater. Phreeqc software was used to calculate the saturation indices of calcite and fluorite in groundwater. By comparing groundwater quality data of 2003 and 2011, we characterized the variations in hydrochemical types and water quality types, salinization of groundwater and fluoride geochemistry of the plain area of the Tarim Basin. Results show that the primary anion in phreatic water in the plain area of the Tarim Basin changed from HCO₃ ^? to SO₄ ^2? or Cl^?. On the contrary, the primary anion in confined water changed from SO₄ ^2? or Cl^? to HCO₃ ^?. In 2003, 63.1 % of the sampling points in the study area exceeded the Class III water quality standard of China. In 2011, the proportion increased to 82.5 %. In addition, severe groundwater salinization was found at 19.7 % of the sampling points. Some of the deep groundwater samples were salinized as well. In the Aksu area at the north-west part of the Tarim Basin, F^? concentration exceeding the standard limit (1 mg/L) was found to be 55.0 % of the groundwater samples tested. Based on these findings, it is concluded that the phreatic water in the study area was severely influenced by the industrial wastewater and domestic sewage related to human activities, while the confined water was less affected. The general quality of groundwater was in an aggravation trend, and the groundwater salinization was in a severe condition in this area. The Ca²⁺–Na⁺ ionic exchange, the unsaturated fluorite and oversaturated calcite in the aquifer of the Aksu area are proposed to cause F^? enrichment in groundwater of this area.     

Characteristic of water chemistry and hydrodynamics of deep karst and its influence on deep coal mining

The mining depth of main coal mines could reach around 600 m in eastern North China, and extends to the dept with speed of around 12 m/a. As the basement of eastern North China-type coal mine, the Ordovician karst aquifer is the main water source that influences the carboniferous coal seam mining. As the deep karst water has large buried depth and high water pressure (8–12 MPa), with10–30 m space between high pressure aquifer and coal seam, the geological area of deep coal occurrence is often forbidden for mining. Environmental damage, to a greater or lesser degree, is caused by coal mining. On the basis of analyzing the hydrogeological conditions of mining areas, this paper introduces the hydrogeological survey work of ultra-high confined karst water deep in the coal seam floor within researched region for preventing and controlling water disaster of the mine. After researching into the hydrogeological investigation data in the researched region, we explored the hydrodynamic and water chemical characteristics of deep karst water by using pumping test, dynamic observation, and dewatering test. Finally, this study suggests that the hydraulic pressure of deep mining could be mined, on the circumstances that reasonable and effective of water prevention measures are taken based on a detailed survey on water abundance of deep karst.     

Development and calibration of the Moon-based EUV camera for Chang'e-3

The process of development and calibration for the first Moon-based extreme ultraviolet(EUV) camera to observe Earth's plasmasphere is introduced and the design, test and calibration results are presented. The EUV camera is composed of a multilayer film mirror, a thin film filter, a photon-counting imaging detector, a mechanism that can adjust the direction in two dimensions, a protective cover, an electronic unit and a thermal control unit. The center wavelength of the EUV camera is 30.2 nm with a bandwidth of 4.6 nm. The field of view is 14.7° with an angular resolution of 0.08°, and the sensitivity of the camera is 0.11 count s-1Rayleigh-1. The geometric calibration, the absolute photometric calibration and the relative photometric calibration are carried out under different temperatures before launch to obtain a matrix that can correct geometric distortion and a matrix for relative photometric correction,which are used for in-orbit correction of the images to ensure their accuracy.     

Water vapor transport and cross-equatorial flow over the Asian-Australia monsoon region simulated by CMIP5 climate models

The summer mean water vapor transport (WVT) and cross-equatorial flow (CEF) over the Asian-Australian monsoon region simulated by 22 coupled atmospheric-oceanic general circulation models (AOGCMs) from the World Climate Research Programme’s Coupled Model Intercomparison Project Phase 5 (CMIP5) were evaluated. Based on climatology of the twentieth-century simulations, most of models have a reasonably realistic representation of summer monsoon WVT characterized by southeast water vapor conveyor belt over the South Indian Ocean and southwest belt from the Arabian Sea to the East Asian. The correlation coefficients between NCEP reanalysis and simulations of BCC-CSM1-1, BNU-ESM, CanESM2, FGOALS-s2, MIROC4h and MPI-ESM-LR are up to 0.8. The simulated CEF depicted by the meridional wind along the equator includes the Somali jet and eastern CEF in low atmosphere and the reverse circulation in upper atmosphere, which were generally consistent with NCEP reanalysis. Multi-model ensemble means (MME) can reproduce more reasonable climatological features in spatial distribution both of WVT and CEF. Ten models with more reasonable WVT simulations were selected for future projection studies, including BCC-CSM1-1, BNU-ESM, CanESM2, CCSM4, FGOALS-s2, FIO-ESM, GFDL-ESM2G, MRIOC5, MPI-ESM-LR and NorESM-1M. Analysis based on the future projection experiments in RCP (Representative Concentration Pathway) 2.6, RCP4.5, RCP6 and RCP8.5 show that the global warming forced by different RCP scenarios will results in enhanced WVT over the Indian area and the west Pacific and weaken WVT in the low latitudes of tropical Indian Ocean.     

Intercomparison between observed and simulated variability in global ocean heat content using empirical mode decomposition, part I: modulated annual cycle

This study proposes a new more precise and detailed method to examine the performance of IPCC AR4 models in simulation of nonlinear variability of global ocean heat content (OHC) on the annual time scale during 1950–1999. The method is based on the intercomparison of modulated annual cycle (MAC) of OHC and its instantaneous frequency (IF), derived by Empirical Mode Decomposition and Hilbert-Huang Transformation. In addition to indicate the general agreement in gross features globally between models and observation, our results point out the problems both in observation and in modeling. In the well observed Northern Hemisphere, models exhibit extremely good skills to capture nonlinear annual variability of OHC. The simulated MACs are highly correlated with observations (>0.95) and the IF of MACs varies coherently with each other. However, in sparsely observed Southern Hemisphere (SH), even though the simulated MACs highly correlate with observations, the IF shows significant difference. This comparisons show that the models exhibit coherent variability of IF of MACs in SH with each other, but not with observations, revealing the problems in the objective analyzed dataset using sparse observations. In the well observed tropic region, the models lack the coherence with the observations, indicating inadequate physics of the models in the tropical area. These results illustrate that the proposed method can be used routinely to identify problems in both models and in observation of the global ocean as a critical component of global climate change.     

城市热岛斑块遥感识别及空间扩张路径研究——以北京市为例

研究利用MODIS地表温度数据产品,引入概率阈值算法提升城市热岛斑块空间识别精度。在此基础上,构建城市热岛扩张指数将城市热岛斑块时空变化过程分解为飞地型、边缘型、填充型扩张模式和缩减型模式。基于土地利用变化过程,开展城市热岛斑块空间扩张模式的路径分析,准确识别城市热岛斑块空间扩张路径的来源和归趋。研究表明：2020年北京市夏季昼夜城市热岛斑块总面积分别为3932 km²和2 266 km²,占北京市总面积比例23.96%和13.81%。2005―2020年夏季昼夜城市热岛斑块面积比例分别增加43.40%和24.44%。增长型城市热岛斑块面积大于缩减型城市热岛斑块面积。边缘型扩张模式是增长型城市热岛斑块最主要的模式。耕地、城市建设用地、农村居民点是增长型城市热岛斑块主要的空间扩张路径。研究结果为揭示城市热环境形成过程和精细化管理提供理论依据和数据支撑。     

Intensity of competition for forage between livestock and wild herbivores based on grassland carrying capacity北大核心CSCD

放牧家畜与食草野生动物争草(畜兽冲突)是人兽冲突在草原放牧业中的具体体现,其涉及面广,对牧民生计影响明显。畜兽冲突强度研究对完善野生动物损害补偿制度、促进人与自然和谐共生具有重要意义。论文通过地面调查与模型模拟,考虑草地牧草产量、家畜存栏量和食草野生动物种群数量,提出了放牧家畜与食草野生动物争草冲突强度量化方法,评价了三江源国家公园玛多县牧草地畜兽争草强度。结果表明：(1)据2022年样线调查和随机森林模型估计,玛多县藏野驴(Equus kiang)、藏原羚(Procapra picticaudata)种群密度分别为0.2157头/km2、0.1655只/km2,种群数量分别为5307头、4073只,折合23264羊单位(SU),2018年末各类家畜存栏量34.2万SU,畜兽争草相对强度为1/14.7。(2)玛多县高寒草甸、高寒草原的可食牧草产量分别为118.7 g/m2、88.3 g/m2,可承载密度分别为0.2710 SU/hm2、0.1532 SU/hm2,理论承载力52.85万SU。家畜承载率、食草野生动物承载率、家畜+食草野生动物承载率分别为64.7%、4.4%和69.1%。(3)国家公园内的乡镇,草地承载力盈余,家畜承载率低、野生动物承载率高,但畜兽争草相对强度较大,建议完善移民搬迁、野生动物损害补偿制度,强化国家公园体制建设;国家公园外的乡镇,草地超载严重,家畜承载率高,畜兽争草强度不高,建议减畜增效、绿色发展。     

Cenozoic structural deformation and dynamic processes of the Bohai Bay basin province,China

Cenozoic structures in the Bohai Bay basin province can be subdivided into eleven extensional systems and three strike-slip systems. The extensional systems consist of normal faults and transfer faults. The normal faults predominantly trend NNE and NE, and their attitudes vary in different tectonic settings. Paleogene rifting sub-basins were developed in the hanging walls of the normal faults that were most likely growth faults. Neogene–Quaternary sequences were deposited in both the rifting sub-basins and horsts to form a unified basin province. The extensional systems were overprinted by three NNE-trending, right-lateral strike-slip systems (fault zones). Although the principal displacement zones (PDZ) of the strike-slip fault zones are developed only in the basement and lower basin sequences in some cross sections, the structural deformation characteristics of the upper basin sequences also indicate that they are basement-involved, right-lateral strike-slip fault zones. According to the relationships between faults and sedimentary sequences, the extensional systems were mainly developed from the middle Paleocene to the late Oligocene, whereas the strike-slip systems were mainly developed from the Oligocene to the Miocene. Strike-slip deformation was intensified as extensional deformation was weakened. Extensional deformation was derived from horizontal tension induced by upwelling of hot mantle material, whereas strike-slip deformation was probably related to a regional stress field induced by plate movement.     

Distribution of phosphine in the offshore area of the Southwest Yellow Sea,East Asia

Phosphine is a natural gaseous compound in the phosphorus biogeochemical cycle. This paper studies the spatial and temporal distributions of matrix-bound phosphine (MBP) and gaseous phosphine in the offshore area of the Southwest Yellow Sea, East Asia. The results show that MBP concentrations in marine surface sediments range from 0.69 ± 0.06 ng/kg (dry) to 179 ± 29 ng/kg (dry). Higher seasonal MBP concentrations in sediments are found in fall than in spring or winter in most sites. High MBP contents are observed in two fish-breeding areas. MBP concentrations decrease with distance to the coast, except in the southeast of the sampling area. MBP levels in marine sediments are found to be higher than those at several other places: freshwater sediments and soil, except eutrophic lakes. Gaseous phosphine contents in fall range from 0.14 ± 0.00 ng/m³ to 9.83 ± 0.97 ng/m³. No correlation is observed between MBP and gaseous phosphine.