金门岛红树林湿地海洋线虫群落结构的初步探究          下载免费PDF全文

肖月平  郭玉清  施宜佳 《应用海洋学学报》2023,42(3):402-408

本研究于2021年2月在金门岛红树林湿地设置2个断面4个采样站位进行沉积物样品采集,对小型底栖动物的类群组成,海洋线虫群落的优势属、优势种和摄食类型等方面进行研究。结果表明：共鉴定出10个小型底栖动物类群,包括海洋线虫、桡足类、寡毛类、多毛类、涡虫、有孔虫、腹足类、涟虫、双壳类和缓步类;其中海洋线虫为最优势类群,占小型底栖动物总数的93.93%。共鉴定出海洋线虫51种或分类实体,隶属于4目15科31属。建功屿断面JH站位鉴定出11属16种,其优势属（数量百分比≥5%）为Ptycholaimellus、Viscosia、Daptonema、Dorylaimopsis、Parasphaerolaimus、Anoplostoma,优势种为Ptycholaimellus sp.1、Viscosia sp.1、Daptonema ungula、Dorylaimopsis sp.1、Anoplostoma papaviviparum; JM站位鉴定出23属35种,其优势属为Metachromadora、Daptonema、Viscosia、Ptycholaimellus、Dorylaimopsis,优势种为Metachromadora sp.1、Viscosia sp.1、Dorylaimopsis sp.1、Daptonema baihaijiaoensis、Ptycholaimellus ocellatus; JL站位鉴定出18属30种,其优势属为Daptonema、Dorylaimopsis,优势种为Daptonema quattuor、Daptonema setihyalocella、Viscosia sp.1、Daptonema baihaijiaoensis、Ptycholaimellussp.1、Spilophorella candida。古宁头断面GH站位鉴定出21属35种,其优势属为Daptonema、Parasphaerolaimus、Ptycholaimellus、Viscosia、Ptycholaimellus,优势种为Daptonema aquattuor、Daptonema setihyalocella、Viscosia sp.1、Daptonema baihaijiaoensis、Ptycholaimellus sp.1、Spilophorella candida。从群落结构来言,4个采样站位仅Daptonema为共有优势属,其他无共有优势种。从摄食类型来看,除建功屿断面中潮位的海洋线虫群落以2A型为主以外,在其他3个采样站位均以1B型为优势,故本研究海洋线虫以非选择性沉积食性者为主。  相似文献   

不同混养模式下中华鲟养殖池透明度变化及其影响因素     

方磊  刘健  周升  吕昊泽  陈锦辉  吴建辉  徐嘉楠  郑跃平  张饮江  沈和定 《湖泊科学》2012,24(2):307-312

中华鲟与背角无齿蚌和鲢鳙混养的池水透明度(SD)对比试验表明,1#池(对照)、2#池(挂养背角无齿蚌)、3#池(混养鲢鳙)透明度平均值分别为11.92、16.45、17.45 cm,分别较试验本底值依次提高26.69%、56.67%、66.19%.2#、3#池的透明度显著大于1#池,最高可达1倍.3个池透明度与各水质指标关系的Panel Data模型分别为:SD1=-0.0072 TSS+0.8353 NH 4+-N-2.1711 TN+0.6195 TP-0.0405 COD+16.7815,SD2=0.0030 TSS+3.8864 NH 4+-N+0.1893 TN-12.4585 TP***-0.0104 COD+24.5306,SD3=0.0381 TSS*+3.7821 NH 4+-N+0.6003 TN-15.0444TP***-0.4078 COD**+34.2992(*、**、***分别表示显著、较显著、极显著相关).TP是影响中华鲟养殖池透明度的主要指标,NH 4+-N、TN、COD是影响透明度的间接指标,而TSS是影响透明度的直接指标.在悬浮物浓度较高、水体浑浊的中华鲟养殖池水体中,鲢鳙的放养对透明度的提高效果显著优于背角无齿蚌.  相似文献   

晋西黄土洞穴成因研究   总被引：1，自引：0，他引：1  

李滨  彭建兵  殷跃平  李喜安 《工程地质学报》2007,15(4):490-494

在野外调查、室内实验基础上,对晋西黄土洞穴的成因进行了分析,研究表明:晋西黄土洞穴的形成是多种内外因素综合作用的结果,主要因素包括黄土的土性、微观结构、节理裂隙、地层结构厚度、水文气候、地形地貌等,其中黄土土性和微观结构是黄土洞穴形成的内因,节理裂隙和地层分布状况为洞穴发育提供了空间和物质基础,水成为黄土洞穴形成的源动力,地形地貌则控制着黄土洞穴的分布。  相似文献   

管理信息系统中层次类编码数据的递归录入     

卢跃平 《成都信息工程学院学报》1998,(4)

介绍了用二维关系表存储树型结构的原理,在此基础上提出层次类型编码数据的递归录入法,并给出一个通用递归录入程序。  相似文献   

The Second World Landslide Forum, Rome, 2011 and the Third World Landslide Forum, Beijing, 2014     

Kyoji Sassa  Paolo Canuti  Claudio Margottini  Yueping Yin 《Landslides》2012,9(2):285-297

The Second World Landslide Forum was held at the headquarters of Food and Agriculture Organization of the United Nations on 3?C9 October 2011 in Rome, Italy. The Third World Landslide Forum (WLF3) is to be held at the China National Convention Center in Beijing, China from 2 to 6 June 2014. This article first outlines the aims and background of the World Landslide Forums, reports on the Second World Landslide Forum in Rome, and then announces the plans for the Third World Landslide Forum in Beijing. Finally, it calls for contributions for the organization of WLF3 and participation in the International Consortium on Landslides (ICL) and the International Programme on Landslides.  相似文献   

ADCP流量生成模型及相应计算方法研究          下载免费PDF全文

韩继伟  符伟杰  唐跃平  邵军 《水文》2014,34(6):9-13

如何快速准确监测河道流量,一直是水文学者研究的对象。ADCP是一种先进的流量测验仪器。本文分析ADCP流量测验机理,提出ADCP流量生成模型的概念,分析出ADCP流量生成模型的结构,构建了ADCP流量生成模型。根据流量生成模型研制的ADCP流量计算程序计算结果和目前应用广泛的Winriver软件计算结果极其相似。ADCP流量生成模型概念准确、结构合理,数据处理计算方法得当、研制的程序可靠。这为ADCP国产化奠定了坚实的基础。  相似文献   

Landslide Developmental Characteristics and Response to Climate Change since the Last Glacial in the Upper Reaches of the Yellow River,NE Tibetan Plateau     

YIN Zhiqiang  QIN Xiaoguang  YIN Yueping  ZHAO Wuji  WEI Gang 《《地质学报》英文版》2014,88(2):635-646

The upper reaches of the Yellow River in northeastern Tibetan Plateau are geohazards areas. The evolution of the Yellow River, chronology of some landslides, and spatiotemporal distribution characteristics of super large scale and giant landslides within the region are summarized using paleoclimate evidence, and the relationship between the intensive landslide period and climatic changes since the Last Glacial period is analyzed. It is concluded that(1) Super large scale and giant landslides are distributed widely within the region, particularly in the Qunke-Jianzha basin.(2) The chronological sequence of landslides is established by dating the slip zones of landslides and analyzing the relations between landslides and their overlying or underlying loess formations. Five landslide development periods are determined: 53–49 ka BP, 33–24 ka BP, 10–8 ka BP, 5–3.5 ka BP, and the present.(3) These correspond closely to warm and wet periods during the last 100,000 years, i.e., two weak paleosol development stages of Malan loess deposited during the last Glacial period in the Chinese loess Plateau, L1-4 and L1-2 that belong to the marine oxygen isotope stage 3, the last deglacial period, the Holocene Optimum, and the modern global warming period.(4) Landslide triggers may be closely linked to warm and wet periods related to rapid climatic transitions.  相似文献   

A physical similarity model of an impulsive wave generated by Gongjiafang landslide in Three Gorges Reservoir,China   总被引：3，自引：1，他引：2  

Bolin Huang  Yueping Yin  Shichang Wang  Xiaoting Chen  Guanglin Liu  Zhibing Jiang  Junzhe Liu 《Landslides》2014,11(3):513-525

Landslide-related impulse waves are catastrophic but accidental, so limited data on field measurements are available; scaled physical experiment is therefore a functional method to simulate and analyze this phenomenon. A large-scale physical Froude-similar model to produce impulse waves was constructed based on the Chinese Gongjiafang landslide, which occurred on the main stream of Three Gorges after the impounding in the reservoir in China. With a scale of 1:200, the model had the dimensions of 24, 8, and 1.3 m. Four water levels, 145, 156, 172.8, and 175 m, were modeled for the experiments, and marble coarse sands were used to imitate the actual cataclastic rock mass. Wave height gauges, high-speed cameras, and run-up measuring instruments were used to monitor wave fluctuations in the model. Among the experiments, the ones modeled using a water level of 172.8 m best confirmed the actual conditions in the Gongjiafang landslide, representing a good validation of the experiments. This study obtained, for the first time, specific data on the reproduced impulse waves’ convergence and superposition during propagation, and of the energy change between impulse waves and reflected waves. The test data describe a rapid decaying and gradual decaying rule for the wave heights and run-ups. The Froude-similar experiments presented in this article help us to understand the whole procedure of impulsive wave generated by cataclastic rock mass failure, and the results acquired contribute to studies of impulse waves caused by similar bank destabilizations worldwide.  相似文献   

贵州关岭大寨高速远程滑坡碎屑流研究   总被引：15，自引：1，他引：14  

殷跃平  朱继良  杨胜元 《工程地质学报》2010,18(4):445-454

2010年6月28日,贵州关岭因突降暴雨发生高速远程滑坡,滑程约1.5km,体积约174.9万m3,两个村组被毁,99人遇难。滑坡区位于西南地区常见的煤系地层区,上部为灰岩、白云岩,中部为相对较缓的砂岩地层,下部为页岩、泥岩地层,局部含煤,具有上硬下软的山体地质结构和上部富水下部隔水的水文地质结构,极易形成滑坡地质灾害。从地形上看,斜坡上陡下缓,形似靴状地形,上部陡峭地形导致山体易于失稳,而中下部开阔伸展良好的沟谷提供了远程的运动条件,较大的势能向动能的转化,容易形成高速远程滑坡碎屑流。6月27日和28日的降雨是触发此起特大灾害的主要原因,其24h降雨量达310mm,超过了当地近60a来的气象记录,分析表明,降雨产生的沟谷径流量是平时强降雨(100～150mmd-1)的沟谷径流的2倍之上,一是在滑源区砂岩裂隙岩体中形成静水压力和渗透压力,触使滑坡的失稳下滑; 二是在沟谷中产生地表径流,为碎屑流远程流动形成饱水下垫面,导致了碎屑流流动距离和速度的显著增加。近年来随着极端强降雨等灾害性天气的重现期缩短,高速远程滑坡造成的群死群伤特大地质灾害在我国呈逐渐增加趋势,应加强对这种灾害类型的调查与防范,特别是要进行滑坡安全避让范围和逃逸速度的研究。  相似文献   

ICL-CGS Seminar on Geo-hazards in Xi’an
February 20th–25th, 2011, Xi’an, Shaanxi, China     

Yueping Yin  Xiaochuan Li 《Landslides》2011,8(3):405

  相似文献