Monitoring water level and volume changes of lakes and reservoirs in the Yellow River Basin using ICESat-2 laser altimetry and Google Earth Engine

Monitoring the water level and volume changes of lakes and reservoirs is essential for deepening our understanding of the temporal and spatial dynamics of water resources in the Yellow River Basin, with a view to better utilizing and managing water resources. In recent years, there have been many studies on monitoring water level and volume changes in inland waters, but they were mainly focused on radar altimetry and the full waveform LiDAR ICESat, which was retired in 2010. Few studies based on the latest photon-counting LiDAR ICESat-2 have been reported. Compared with previous sensors, ICESat-2 has great advantages in footprint size, transmitting frequency, pulse number, etc, but its performance in monitoring water level and volume changes in inland waters has not been fully explored. Here we investigated the spatial distribution of water level and volume changes of 11 lakes and 8 reservoirs in the Yellow River Basin based on ICESat-2 and Google Earth Engine, and analyzed the factors affecting the measurement uncertainties. In-situ validation of lake level in Lake Qinghai indicates that the Root Mean Square Error (RMSE) of our result is only 7 cm after the reference coordinate system conversion. We found that the water level trend of the natural lake shows significant seasonal variations, while the water level trend of the reservoir shows a sharp rise and fall. In addition, precipitation plays a decisive role in the changes in natural lake levels and indirectly affects the artificial control of reservoirs’ water discharges. The uncertainty of water volume change monitoring is mainly affected by water level measurement uncertainty for lakes, while for reservoirs, that is affected by the combination of water level and area measurement uncertainties. The stability of lake level measurement increases with the increase in photon counts. The introduction of ICESat-2 ATL13 Significant Wave Height might lead larger standard deviation in water level measurement. According to the law of propagation of uncertainty, the uncertainty of the water volume change estimation by the combination of ICESat-2 and GEE is less than 9 %.     

茅洲河污染来源分析及治理对策研究

茅洲河作为深圳、东莞界河,水污染问题一直备受关注。污染来源不明导致上下游治理不同步、治污存在争议问题长期存在。根据现场监测,分析水质现状,核算污染通量,明确了深圳光明新区、宝安区、东莞长安镇对茅洲河的污染贡献分别为27.3%、31.5%、41.2%,并提出了整治对策,为茅洲河水污染治理提供依据。     

“长株潭”地区湘江底泥重金属含量调查研究

通过调查分析湘江＂长株潭＂段表层底泥的锌、铜、镉、铬、铅、汞、锰等重金属含量,将底泥样品中重金属的含量分别与土壤环境质量标准、污水排入城市下水道水质标准、以及生活饮用水卫生标准中重金属含量进行比较,从而发现重金属在湘江＂长株潭＂段的污染严重程度。根据调查结果分析,对湘江＂长株潭＂段底泥重金属污染问题提出减排含重金属废水,有关部门应关注底泥重金属含量变化,和修复河床表层重金属含量高的底泥等建议。     

四川色曲河流域植被分布特征的研究

通过对色曲河流域植被的实地考察,结合基于3S技术的遥感解译技术,对该流域植被的分布特征进行了初步探究。从水平分布、垂直分布、林线与雪线的分布规律等方面分析了色曲河流域植被的分布特征。主要表现在:(1)研究区雪线高度为海拔4800m,林线:阴坡为海拔3600m左右;阳坡在3800m左右;(2)研究区山地垂直自然带谱可分为5个,分别为山地常绿硬叶阔叶林地带、山地暗针叶林带/山地落叶阔叶林地带、高山灌丛草甸带、高山草甸带、高寒荒漠带;(3)水平分布的地域性特征比较明显,主要原因为各地的海拔不同所导致;(4)流域植被随坡向变化的规律比较明显,阳坡植被与阴坡植被具有明显的差异性。     

Investigation report of geotechnical disaster on river area due to typhoon landfall three times on Okhotsk region,Hokkaido, Japan

For one week from August 17 to 23, 2016, three consecutive typhoons made landfall in Hokkaido for the first time on record. These typhoons and the front they stimulated brought record-breaking torrential rain over the eastern part of Hokkaido. To investigate the damage to grounds and rivers resulting from this rainfall, the Japan Society of Civil Engineers (JSCE) and the Japanese Geotechnical Society (JGS) formed a disaster research group to conduct an investigation. This report provides the results of the investigation into damage to the grounds of areas along the Tokoro River of the Okhotsk region, Hokkaido, that suffered from this tremendous and diverse disaster. Specifically, the report describes the situation of the levees which were broken and eroded by the overflowing water, the shape of the levee bodies, the levee body soil properties examined by observation of the sections, as well as the occurrence of sand boiling and air blows. The washout of road embankments as well as damage to road bridge mounting fills and abutment backfills were also investigated. The investigation has demonstrated the need to clarify the resistance of the abutment backfills and levee bodies to flowing water as well as the geotechnical predominant factors in order to clarify the mechanisms behind erosion and washout, the need to review new measures that allow for the scale of sand boiling and resultant changes in levee body stability, and the fact that the existing embankments were able to temporarily suppress the flooding water which had spilled over from the river. Furthermore, although it has been identified that the findings of a study on an embankment washout associated with a tsunami can be applied to measures taken against the overflowing water, it has also been found necessary to clarify the predominant geotechnical factors using model tests and to use a more sophisticated analytical approach to establish a geotechnical stability review as soon as possible in order to prevent the levees and embankments from being eroded and washed out due to overflowing water.     

从珠江三角洲到粤港澳大湾区演变看规划响应

采用实证研究方法,以规划响应的演变印证规划的本质。前半部分对珠江三角洲乃至粤港澳大湾区的历版规划进行高度概括梳理凝练,解读了规划演变历史背景,揭示规划响应是一个由局部到整体、层级由低到高的演变过程,既是国家意志体现,亦是经济规律使然,此观点具首创性。后半部分主要阐述《粤港澳大湾区发展规划纲要》的出台及粤港澳三地聚焦科技创新走廊的规划响应,通过描述粤港澳三地在空间上和政策上各自作出的规划响应,以地区的特殊性再次重申“体现国家意志,顺应社会经济发展规律”的规划本质。     

大数据监测平台下的长江流域典型城市房间空调器温度设置分析

房间空调器是中国长江流域地区改善室内热环境的重要措施,然而,在以往的房间空调器的行为研究中,只能通过现场实测、问卷调查等方式获取其使用行为,由于数据获取方式本身所存在的局限性,无法对空调的使用行为进行可靠且深入的挖掘,尤其是对于空调的设置温度。为了研究长江流域地区房间空调器的设置温度行为,包括设置温度的分布、设置温度调节习惯、设置温度与一天中不同时间段的关系、设置温度与室外温度的关系,依托于大数据平台下的房间空调器监测数据,针对长江流域地区的3个典型城市（重庆、武汉、上海）的房间空调器的设置温度习惯,对重庆地区575台房间空调器、武汉地区430台房间空调器、上海地区540台空调器的夏季上万次运行数据、冬季上千次运行数据进行了基本的统计与相关分析,结果表明：空调器的设置温度及其调节习惯在不同城市之间存在一定差异性,夏季用户在一次空调使用过程中存在对较低设置温度（低于26℃）的短时需求情景,同时,设置温度与1 d中的不同时刻以及室外温度也有明显关联。     

松辽盆地南部青一段页岩油甜点评价

松辽盆地南部发育青山口和嫩江两期大规模湖侵,形成青一、二段,嫩一、二段四套广泛发育的页岩层系,其中青一段勘探面积广,暗色泥、页岩厚度大、有机质丰度高、已成熟、是松南页岩油发育的主力层系。笔者以甜点评价为核心,以岩心观察、分析化验、测井评价等为手段,初步认为松南青一段页岩油发育区岩性组合以页岩、泥岩互层为主,局部夹薄层砂岩,其中页岩占地层厚度50%以上,相比泥岩,有机质丰度高,孔隙度、饱和度条件好,页岩与薄砂岩夹层为主力储层;同时,页岩脆性矿物含量较高,且本区普遍存在超压,页岩油成藏条件有利。在此基础上,结合沉积特征,划分两种类型页岩油,初步明确纵向有利层段及平面分布特征,针对两种类型页岩油分别部署探井,试油均获得突破,展现了松辽盆地南部青一段页岩油良好的勘探潜力。     

鄂尔多斯盆地北部地下水铀水文地球化学特征研究

为获得鄂尔多斯盆地北部区域地下水铀水文地球化学特征,运用铀水文地球化学知识,通过调查取样,分析数据,整理资料等进行研究。结果表明,区内第三系含水亚组水中铀含量平均值最高,12. 62μg/L;以区内铀含量滑动平均值1. 65倍均方差值为界限,将研究区划分成1个铀水文地球化学低背景场、10个偏高背景场、3个高背景场;铀水文地球化学场与潜水矿化度、潜水阴离子场、潜水阳离子场的分布特征相吻合。     

澳大利亚布罗肯希尔CUSIN溪矿区地质特征及找矿分析

澳大利亚布罗肯希尔地区是世界上最主要的多金属成矿区之一,仅位于其市内的主铅锌矿体累计开采及探明储量矿石超过2.5亿吨。除此之外,域内还有其他超大型、大型铅锌银金铜多金属矿床、铁矿床、钴矿床、银铅矿床、钨矿床等,小型矿床(点)无数。区域主要出露含矿地层古元古界威利玛超群,是由一套连续的变质程度不同的且多期变形的沉积岩和火山岩形成。位于其内的CUSIN溪矿区成矿地质环境及条件与本区其他矿床基本类似,在勘查中对其矿床(点)地质特征认识分析,发现矿区有热泉型矿床特征,结合区域地质背景、物探及探矿成果,认为本区具有潜在找矿潜力。