异重流沉积动力学过程及沉积特征

异重流(hyperpycnal flows)是指在汇水盆地水深足够条件下,由于携带大量沉积物颗粒,导致流体密度大于稳定环境水体的密度,流体受浮力影响小,沿盆地底部流动的高密度流体,在海水环境中形成异重流的临界沉积物密度为36~43 kg/m~3(体积浓度1.3%~1.7%)。异重流主要受洪水触发形成;从河口到汇水盆地经过回流区、深度有限流区、潜入区的演化,最终形成异重流;主要经历"早期沉积—侵蚀过路—晚期沉积"的沉降过程,在沉积近端以侵蚀充填沉积为主,远端以持续沉积为主;异重流的形成及其沉积主要受地形、气候、物源的控制,地形高差大、半干旱气候条件、丰富的细粒悬浮沉积物供给有利于异重流形成。异重流沉积特征及沉积序列受"源—汇"系统的控制,以流水成因交错层理、层内突变接触面或侵蚀接触面、碳质碎屑和植物碎片为区别于其他深水重力流沉积的典型沉积构造;沉积序列由沉积近端到沉积远端可能依次发育厚层序列、逆正粒序序列、薄层细粒序列。异重流研究具有十分重要的意义,能够丰富和完善深水重力流理论、探究古气候变化和古洪水作用规律、合理解释深水重力流沉积和砂体分布特征、指导深水常规和非常规油气的勘探。     

The Baker Creek Research Watershed: Streamflow data highlighting the behaviour of an intermittent Canadian Shield stream through a wet–dry–wet cycle

Baker Creek drains water from subarctic Canadian Shield terrain comprised of a mix of exposed Precambrian bedrock, lakes, open black spruce forest and peat filled depressions. Research in the catchment has focused on hydrological processes at the hillslope and catchment scales. Streamflow is gauged from several diverse sub-catchments ranging in size from 9 to 155 km². The period of record (2003–2019) of streamflow from these sub-catchments extends from 12 to 17 years, and these data are the focus of this note. Such data are unique in this remote region. 2003–2019 was a period that included both historic wet and dry conditions. Observations during such a diversity of conditions are helping to improve understanding of how stream networks that drain this landscape expand and contract in response to short and long hydroclimatic cycles. These data from a distinctly cold and dry region of low relief, thin soils, exposed bedrock and permafrost are a valuable contribution to the global diversity of research catchment data.     

Using isotopes to understand landscape-scale connectivity in a groundwater-dominated,lowland catchment under drought conditions

The Demnitzer Millcreek catchment (DMC), is a 66 km² long-term experimental catchment located 50 km SE of Berlin. Monitoring over the past 30 years has focused on hydrological and biogeochemical changes associated with de-intensification of farming and riparian restoration in the low-lying landscape dominated by rain-fed farming and forestry. However, the hydrological function of the catchment, which is closely linked to nutrient fluxes and highly sensitive to climatic variability, is still poorly understood. In the last 3 years, a prolonged drought period with below-average rainfall and above-average temperatures has resulted in marked hydrological change. This caused low soil moisture storage in the growing season, agricultural yield losses, reduced groundwater recharge, and intermittent streamflows in parts of an increasingly disconnected channel network. This paper focuses on a two-year long isotope study that sought to understand how different parts of the catchment affect ecohydrological partitioning, hydrological connectivity and streamflow generation during drought conditions. The work has shown the critical importance of groundwater storage in sustaining flows, basic in-stream ecosystem services and the dominant influence of vegetation on groundwater recharge. Recharge was much lower and occurred during a shorter window of time in winter under forests compared to grasslands. Conversely, groundwater recharge was locally enhanced by the restoration of riparian wetlands and storage-dependent water losses from the stream to the subsurface. The isotopic variability displayed complex emerging spatio-temporal patterns of stream connectivity and flow duration during droughts that may have implications for in-stream solute transport and future ecohydrological interactions between landscapes and riverscapes. Given climate projections for drier and warmer summers, reduced and increasingly intermittent streamflows are very likely not just in the study region, but in similar lowland areas across Europe. An integrated land and water management strategy will be essential to sustaining catchment ecosystem services in such catchment systems in future.     

Northern landscapes in transition: Evidence,approach and ways forward using the Krycklan Catchment Study

Improving our ability to detect changes in terrestrial and aquatic systems is a grand challenge in the environmental sciences. In a world experiencing increasingly rapid rates of climate change and ecosystem transformation, our ability to understand and predict how, when, where, and why changes occur is essential for adapting and mitigating human behaviours. In this context, long-term field research infrastructures have a fundamentally important role to play. For northern boreal landscapes, the Krycklan Catchment Study (KCS) has supported monitoring and research aimed at revealing these changes since it was initiated in 1980. Early studies focused on forest regeneration and microclimatic conditions, nutrient balances and forest hydrology, which included monitoring climate variables, water balance components, and stream water chemistry. The research infrastructure has expanded over the years to encompass a 6790 ha catchment, which currently includes 11 gauged streams, ca. 1000 soil lysimeters, 150 groundwater wells, >500 permanent forest inventory plots, and a 150 m tall tower (a combined ecosystem-atmosphere station of the ICOS, Integrated Carbon Observation System) for measurements of atmospheric gas concentrations and biosphere-atmosphere exchanges of carbon, water, and energy. In addition, the KCS has also been the focus of numerous high resolution multi-spectral LiDAR measurements and large scale experiments. This large collection of equipment and data generation supports a range of disciplinary studies, but more importantly fosters multi-, trans-, and interdisciplinary research opportunities. The KCS attracts a broad collection of scientists, including biogeochemists, ecologists, foresters, geologists, hydrologists, limnologists, soil scientists, and social scientists, all of whom bring their knowledge and experience to the site. The combination of long-term monitoring, shorter-term research projects, and large-scale experiments, including manipulations of climate and various forest management practices, has contributed much to our understanding of boreal landscape functioning, while also supporting the development of models and guidelines for research, policy, and management.     

Brixenbach research catchment: Quantification of runoff process proportions in a small Alpine catchment depending on soil moisture states and precipitation characteristics

The Brixenbach valley is a small Alpine torrent catchment (9.2 km², 820–1950 m a.s.l., 47.45°, 12.26°) in Tyrol, Austria. Intensive hydrological research in the catchment since more than 12 years, including a hydrogeological survey, pedological and land use mapping, measurements of precipitation, runoff, soil moisture and infiltration as well as the conduction of rainfall simulations, has contributed to understand the hydrological response of the catchment, its subcatchments and specific sites. The paper presents a synthesis of the research in form of runoff process maps for different soil moisture states and precipitation characteristics, derived with the aid of a newly developed Soil-hydrological model. These maps clearly visualize the differing runoff reaction of different subcatchments. The pasture dominated areas produce high surface flow rates during short precipitation events (1 h, 86 mm) with high rainfall intensity, whilst the forested areas often develop shallow subsurface flow. Dry preconditions lead to a slight reduction of surface flow, long rainfall events (24 h, 170 mm) to a dominance of deep subsurface flow and percolation.     

煤层顶板导水裂缝带发育高度探测研究——以黑龙江省双鸭山双阳煤矿为例

煤层顶板导水裂缝带发育高度是煤矿设计部门在留设防、隔水煤柱时必须考虑的一个重要参数,对煤矿水体下采煤、顶板防治水具有重要意义。基于双阳煤矿水文地质补充勘探项目,在8#煤层采空区上方施工两个地面钻孔,采用地面钻孔钻井液漏失量实测法、钻孔电视摄像技术及传统经验公式法相结合的方法,综合确定8#煤层顶板导水裂缝带发育高度为43.7~45.7m,为地质条件相似矿区在合理确定开采上限、留设防（隔）水煤柱等问题提供方法和数据支持。     

长三角区域创新集群的技术创新联系特征及影响探究——以新材料产业为例

基于区域创新集群的相关概念辨析,提出基于长三角一体化战略的区域创新集群概念,并通过IncoPat网站获取2000—2017年长三角新材料产业已获授权的发明专利,在刻画新材料区域创新集群技术创新联系特征的基础上,利用二步系统广义矩阵估计（Generalized Method of Moments,GMM）模型测度融入区域创新集群的深度与广度对地方创新集群的影响,得到如下结论：第一,区域创新集群的发展符合“点-轴”发展理论的观点,以上海、南京、杭州等发达地方创新集群为增长极,在空间上率先形成以增长极为节点的发展轴,成为区域创新集群的核心组团。第二,区域创新集群技术创新联系具备“全球-地方”创新网络阐述的多种类型知识交互耦合的特征,在同质性知识交互的基础上,异质性知识的交互同样占据重要地位。第三,当前阶段长三角区域创新集群中核心组团的极化效应大于扩散效应,更易在区域创新集群的建设中获益,并且知识基础的正向调节作用明显。区域创新集群研究尚处于起步阶段,相关研究亟待经济地理学者进一步展开。     

关于学风与创新文化的几点认识

本文从5个方面叙述了笔者对当今部分地理界学风与创新文化的观察与认识。第一,基于地理学方法论,阐述了地理学的理论观点与概念判断都是来自对地球表层实际存在的客体的运动特征与空间投影的变化轨迹的观察、分析与概括;第二,结合实际,指出了“博观而约取、厚积而薄发”的知识积累与运用观对学者们的重要性;第三,对科学创新及如何实现创新提出了新的观点;第四,探讨了如何正确处理科研个人与集体的关系;第五,提出人文与经济地理学研究要面向咨询。     

中国社会文化地理学研究的发展与反思：基于2015—2020年中英文文献分析

作为一个在中国发轫较晚的人文地理学分支,社会文化地理学逐渐成为人文地理学的重要分支。随着研究话题的日新月异以及研究方法和理论的推陈出新,中国社会文化地理学的理论和应用研究在近年（2015—2020年）得到越来越多学者的关注和参与,同时涌现出一系列新的学科现象和值得反思的问题,如话题的多样性、研究方法的交叉性、研究科学性的反思和质疑等。因此,从延续学科自省的视角出发,有必要坚持从中、西对比的角度,不断度量中国社会文化地理学的发展趋势,定位学科的特点,以期为国内社会文化地理研究提供一定的方向和启示。借助文献分析工具对2015—2020年中、英文领域主要学术期刊的社会文化地理学文献进行采集和分析,辅以德尔菲法对学科专家进行咨询,尝试结合客观和主观数据,综合辨析当前中外社会文化地理学的研究特色,以及未来中国社会文化地理学研究可能的发展方向和潜力所在。从分析结果上看,国外社会文化地理研究话题涵盖：1）从移民研究到流动性研究;2）从文化景观研究到超越人类的地理学研究;3）弱势人群研究与关怀地理学等方面。中国社会文化地理研究话题包括：1）理论引介与反思;2）城镇化、流动性与多元移民;3）旅游与地方;4）乡村转型与乡愁等方面。综合国内外社会文化地理研究成果可知,西方国家（尤其是英国）作为社会文化地理学的重要发源地,在学科知识“生产—消费”循环中保持优势地位;西方社会文化地理学研究重点关注国际大政治和日常政治话题,而中国社会文化地理研究与旅游和乡村话题结合紧密,与西方形成明显区别,反映中国社会发展需要;中国社会文化地理学国际化趋势明显,但中、西方知识交换程度不高,知识边界依然明显。另外,专家咨询意见也凸显社会文化地理研究者的学科归属感有待加强、研究范式系统化不足与共识不充分等问题。未来中国社会文化地理学需要不断推进学科交叉和方法创新,探索其地理学本质,在国际化进程中讲好中国故事,总结中国经验,发展中国理论,服务国家,对话世界。