基于空间位置的属性数据连接及对不依比例地物统计的应用研究

本研究着眼于土地利用现状调绘不依比例地物的精确统计,围绕着基于空间位置的属性连接方法的应用,利用MapGIS、AutoCAD、CASS和MapGIS土地利用数据库管理系统等软件展开了分析。探讨了空间位置的属性连接方法的理论基础与实施步骤,并提出了空间数据的质量控制与检查的对策。在此基础之上,通过对同一测绘对象分别使用传统方法和基于空间位置的属性连接方法进行了统计,对两种方法的统计结果进行了对比。证实了基于空间位置属性连接方法能够更有效地提高空间数据统计的精度和速度。     

Higher reactivity of allochthonous vs. autochthonous DOC sources in a shallow lake

Dissolved organic carbon (DOC) reactivity in aquatic systems is essentially dependent on DOC precursor material and on the processes regulating its bioavailability, especially photodegradation and microbial activity. We investigated temporal changes (from hours to weeks) in the reactivity of allochthonous and autochthonous DOC sources in a macrophyte-dominated shallow lake using a set of incubation experiments. Changes in DOC fluorescence and absorbance properties due to biodegradation (BD) and to the combined effect of photo- and biodegradation (UV + BD) were traced. Allochthonous DOC was more reactive than autochthonous DOC (AutoDOC), showing higher DOC losses (between 22 and 36 %) and faster changes in DOC properties than AutoDOC. The effect of UV + BD was larger than BD alone for both sources of DOC. The rates of change of DOC properties were stronger during the first days of incubation and showed no regular pattern for any of the treatments or DOC sources. Our findings highlight the relevance of the timescale when assessing changes in DOC quality under different degradation pathways, as well as the need of discussing the labile character usually attributed to autochthonous DOC in systems dominated by submerged vegetation, as many shallow lakes or lagoons.     

高密度电阻率法在四川高川茶园沟滑坡勘察中的应用

将高密度电阻率法用于四川省高川乡茶园沟滑坡地质勘察中,结合钻孔资料确定了滑坡体主滑动面的位置、基岩的埋深及含水程度,为滑坡治理提供可靠的地球物理依据。     

Sequence stratigraphic evolution of The post-rift MEGASEQUENCE in The northern part of The Nile Delta basin,Egypt

The stratigraphic succession of the subsurface Pliocene-Quaternary post-rift megasequence in the north-central part of the Nile Delta includes the rock units; Kafr El-Sheikh Formation (Early-Middle Pliocene), El- Wastani Formation (Late Pliocene), Mit-Ghamr and Bilqas formations (Quaternary). These rock units were analyzed according to the sequence stratigraphic principles to construct their stratigraphic architecture and discuss the depositional events influencing their evolution. Accordingly, seven 3rd order depositional sequences were encountered, of which six 3rd order seismic depositional sequences (sequences 1–6) are found in the Early–Middle Pliocene Kafr El-Sheikh Formation, whereas sequence-7 includes the Quaternary rock units. Sequences 1 and 7 were further subdivided, on the basis of high-resolution sequence stratigraphy into 8 and 11 4th order subsequences respectively. The results of the sequence stratigraphic analyses suggested that the depositional evolution of the examined Pliocene-Quaternary megasequence represents a complete prograding depositional phase during the Nile Delta history. The lower part of Kafr El-Sheikh Formation (sequences 1, 2, 3 and 4) was deposited as a thick outer marine shelf succession over which the younger rock units were deposited. However, the depositional sequences 5 & 6 of Kafr El-Sheikh Formation and the lower parts of El-Wastani Formations may indicate a deposition within active prograding prodelta sub-aqueous deltaic-subenvironments. The upper parts of El-Wastani Formation were deposited as a constructive delta-front pushing its way northward. The Pleistocene Mit-Ghamr Formation was evolved as a direct result of a huge fluvial input, organized as coalescing laterally extensive sand-rich bars. These were laid-down by active fluvial distributary streams that dominated the delta plain as the final phases of the present deltaic subaqueous environments.     

热释汞量法在山东牟平金矿成矿预测中的应用

简要介绍了汞及其化合物的地球化学性质和RG-1型热释测汞仪，以山东省牟平金矿为例，介绍了矿区地质特征，运用热释汞量法圈出了主要的控矿构造，就主要控矿地段进行了成矿预测。结果表明：热释汞量法方法简单，快速，成本低，重现性好，具有很好的应用前景。     

东海多环旋沟藻的形态特征和系统进化分析

本文首次对分离自我国东海海域的多环旋沟藻(Cochlodinium polykrikoides Margalef)藻株进行了详细的分类学报道。通过运用光学显微镜、荧光显微镜、电子扫描电镜和分子生物学方法,对多环旋沟藻的形态和显微特征进行了详细的描述,并对其核糖体大亚基序列(LSU rDNA)进行了系统进化分析。该藻以单细胞或链状细胞形态存在。通常链状包括2、4、8和16个细胞。横沟宽且深围绕细胞近2圈,内含鞭毛。纵沟窄并浅紧挨着横沟延伸。具有U形顶沟,细胞核大而圆,分布在上锥的前端。叶绿体棒状,数量较多并呈簇状分布。测序获得核糖体大亚基D1—D3区序列为870bp,通过构建系统发育树和Jukes-Cantor遗传距离矩阵可知东海多环旋沟藻藻株为东亚型。