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依据“建设用地地质灾害危险性评估技术要求”选择积分法对工程建设用地进行地质灾害危险性现状评估,结果认为：评估区的地质环境条件复杂程度属简单—中等类型,评估区现状地质灾害有崩塌灾害—种类型7处,属危险性小的级别,对其危险性起决定性作用的因素有：地形条件、地层岩性、构造与地震和人为活动。 相似文献
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建设用地地质灾害危险性评估中关键技术问题的探讨 总被引：6，自引：0，他引：6
根据“建设用地地质灾害危险性评估技术要求”中的原则,对建设项目(市政工程、铁路工程及其它)重要性进行了评估级别的划分。尝试确定了评估范围。提出危险性分区可根据评估区地质灾害危险性综合评价结果进行划分。 相似文献
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PRB技术在矿区地质填图及图件编绘中应用的几点尝试 总被引：2，自引：1，他引：1
运用PRB数字填图技术进行矿产地质填图及图件编绘的基本做法是:用手持GPS对地质点定位,并将坐标值及相关简单属性存于其中,用接收软件将存于GPS中的数据导出,然后在比较通用的软件如Excel.surfer8、Grapher4、CAD、Mapgis等软件中进行处理,最后在Mapgis中加挂属性,进行建库分析。实践过程中尚遇一些难题,如GPS的精度问题、地形图矢量化工作量大且各自为战、地质花纹及颜色填充混乱不统一等问题,有待于今后逐步完善。 相似文献
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海底地下水排放对典型红树林蓝碳收支的影响 总被引：1，自引：0，他引：1
海底地下水排放(Submarine Groundwater Discharge,SGD)是陆海相互作用的重要表现形式之一,其携带的物质对近岸海域生源要素的收支有重要影响。本文利用222Rn示踪技术估算了我国典型红树林海湾—广西珍珠湾在2019年枯季(1月)SGD携带的碳通量。调查发现,地下水中222Rn活度、溶解无机碳(DIC)和溶解有机碳(DOC)的平均浓度均高于河水和湾内表层海水。利用222Rn质量平衡模型估算得到珍珠湾SGD速率为(0.36±0.36) m/d,SGD输入到珍珠湾的DIC和DOC通量分别为(2.41±2.63)×107 mol/d和(1.96±2.20)×106 mol/d。珍珠湾溶解碳的源汇收支表明,SGD携带的DIC和DOC分别占珍珠湾总DIC和总DOC来源的91%和89%。因此,SGD携带的DIC和DOC是珍珠湾DIC和DOC的主要来源,是海岸带蓝碳收支和生物地球化学循环过程中的重要组成。 相似文献
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HOU Jianjun LAI Hongyan HUANG Bangqin CHEN Jixin College of Fisheries Huazhong Agricultural University Wuhan China College of Life Sciences Hubei Normal University Huangshi China State Key Laboratory of Marine Environmental Science Environmental Science Research Center Xiamen University Xiamen China Key Laboratory of Freshwater Fish Germplasm Resources Biotechnology Yangtse River Fisheries Research Institute Jinzhou China State Key La... 《海洋学报(英文版)》2009,28(2)
Partial rDNA sequences of Prorocentrum minimum and Takayama pulchella were amplified, cloned and sequenced, and these sequence data were deposited in the GenBank. Eight oligonucleotide probes (DNA probes) were designed based on the sequence analysis. The probes were employed to detect and identify P. minimum and T. pulchella in unialgal and mixed algal samples with a fluorescence in situ hybridization method using flow cytometry. Epifluorescence micrographs showed that these specific probes labeled with flu... 相似文献
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城市空间与居民行为不断交互,相互影响。探究城市空间中的群体活动分布及其时空变化能够帮助数据驱动的城市规划与城市治理。基于大数据的时空间群体活动研究是当前时空大数据研究的一个热点。本文以深圳市为例,基于约1000万手机用户在某一工作日的基站尺度的手机定位数据,识别用户停留位置和停留活动,重建活动语义信息,分析用户的停留点和停留活动的分布差异,研究群体活动的时空分布模式,探讨人群活动模式的多样分布特征。研究表明：停留位置和活动分布存在差异,每人每天平均的停留个数约为2.1个,而每人每天平均从事的活动约为3.4个;不同类型的活动在时间上存在波动;群体活动存在空间分异特征,整体上服从“空间幂律”。本研究揭示了城市空间中群体活动的多样性及其时空分布特征,对于城市居民活动研究、城市交通优化和城市规划具有重要的意义。 相似文献
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234Th is widely used to quantify the magnitude of upper ocean particulate organic carbon(POC)export in oceans.In the present work,the rates of particulate organic carbon export were measured based on the distribution patterns of234Th/238U disequilibrium in the water column within the continental slope of the East China Sea(ECS)during May 2011.The profiles of particulate and dissolved234Th activities at all three stations showed a relative deficit with respect to238U in the upper 100 m of the water column.The dissolved234Th scavenging rates and the particulate234Th removal rates and their residence times were calculated by a one-dimensional steady state model.The results showed that the dissolved234Th scavenging rates and the particulate234Th removal rates ranged from 12.4–61.4 dpm/(m3·d)andfrom3.8–21.8 dpm/(m3·d),respectively.The residence times of dissolved and particulate234Th were in the range of 3.4–158 d and 63.7–96.5 d,respectively.Combined with the measurement of POC/234Th ratios of suspended particles,POC export flux(calculated by carbon)from the euphotic zone was estimated in the study region,which ranged from 4.14–14.7 mmol/(m2·d),withanaverageof8.21mmol/(m2·d),occupying35%oftheprimeproductivity in the study area.The results of this study can provide new information for better understanding the carbon biogeochemical cycle within the continental slope of the ECS. 相似文献
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页岩气是一类非常规天然气聚集类型,在中国找页岩气的实践还处于初期阶段,如何合理评价其资源量目前还没有成熟的方法,尤其针对陆相页岩气评价更缺乏借鉴和参考。文中在分析海相、陆相页岩的差异和特点的基础上,明确陆相页岩资源评价的条件和标准。针对延长探区中生界三叠系延长组页岩开展研究,在样品测试、含气量初评的基础上,对陆相页岩气的资源进行初步评价。对不同勘探程度和地质条件采用不同的资源评价方法,综合不同方法获得的结果认为,延长直罗—下寺湾区中生界陆相页岩气资源量达到(626.4～6 037.2)×108 m3,具有很好的勘探开发价值。 相似文献
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Radionuclides (i.e., 7Be and 210Pb) can be used to trace particle and sediment dynamics and to quantify coastal oceanic processes with time scales ranging from a few days to a hundred years. Here, we study the settling dynamics of suspended particles and the implication by sedimentary heavy metals in the Wenjiao/Wenchang River and Wanquan River estuaries through the measurement of the particulate 7Be and 210Pb nuclides. Activity in the particulate phase had a range of 2.1–54.5 and 4.6–67.9 Bq kg−1 for 7Be and excess 210Pb (210Pbxs), respectively, in the Wenjiao/Wenchang River estuary. In the Wanquan River estuary, activity is in the range of 1.2–43.5 Bq kg−1 for 7Be and 6.2–194.5 Bq kg−1 for 210Pbxs. At the same time, activity in the dissolved phase had a range of 0.46–1.26 and 0.30–1.17 Bq m−3 for 7Be and 210Pb, respectively, in the Wenjiao/Wenchang River estuary; ranges of 0.10–2.31 and 0.09–1.87 Bq m−3 for 7Be and 210Pb, respectively, were observed in the Wanquan River estuary. The distribution coefficients (Kd) for the two nuclides decreased within increased in suspended particle matters (SPM) concentration and/or salinity in Wanquan River estuary. The residence times of particulate 7Be and 210Pbxs had ranges of 0.4–1.6 and 1.65–5.15 days, respectively, in the Wenjiao/Wenchang River estuary; and ranges of 0.02–3.2 and 0.61–4.44 days, respectively in the Wanquan River estuary. All residence times for the two nuclides increased in the seaward direction. In the Wenjiao/Wenchang River estuary, we found that 11.8–21.0% of Cu, 3.0–9.0% of Zn and 43.2–69.9% for Cd is removed from the water column and deposited into the estuary, and 24.2–34.8% for Cu, 7.2–23.8% for Zn, and 70.0–82.5% for Cd in the Wanquan River estuary, respectively. 相似文献