Size-dependent responses of zooplankton to submerged macrophyte restoration in a subtropical shallow lake

To explore the size-dependent responses of zooplankton to submerged macrophyte restoration, we collected macrophyte, zooplankton and water quality samples seasonally from a subtropical shallow lake from 2010 to 2012. Special attention was given to changes in rotifers and crustaceans(cladocerans and copepods). The rotifers were grouped into three size classes(200 μm, 200 μm–400 μm, 400 μm) to explore their size-related responses to macrophyte restoration. The results showed that during the restoration, the annual mean biomass and macrophyte coverage increased significantly from 0 to 637 g/m~2 and 0 to 27%, respectively. In response, the density and biomass of crustaceans and the crustacean-to-rotifer ratio increased significantly, while the rotifer density decreased significantly. Moreover, rotifers showed significant sizedependent responses to macrophyte restoration. Specially, rotifers 400 μm were significantly suppressed, while those ≥400 μm were significantly encouraged. Overall, the population of large-sized zooplankton tended to boom, while that of small rotifers was inhibited during macrophyte restoration. Redundancy analysis(RDA) revealed positive correlations between macrophytes and crustaceans, rotifers and COD or Chl-a, but negative correlations between macrophytes and COD or Chl-a, and between crustaceans and Chl-a. Moreover, the results indicate that increased predation on phytoplankton by large-sized zooplankton might be an important mechanism for macrophyte restoration during development of aquatic ecosystems, and that this mechanism played a very important role in promoting the formation of a clear-water state in subtropical shallow lakes.     

通衢广陌天地宽

正俯瞰中华大地,繁华的都市、喧闹的城镇、静谧的乡村……如同一颗颗散落的珍珠,而纵横交织的道路就像那精美的珠链,连接城市与农村,沟通梦想与现实,贯穿昨天与未来。从孤悬绝壁的秦蜀云栈,到通达四海的大秦驰道;从驼铃悠悠的丝绸之路,到马蹄阵阵的皇家驿道,陆地交通改变着人们的生存空间,深刻影响着五千年华夏文明的历史进程。     

“漫话土地”之二十七 地载万物鸟兽栖

正辽阔的平原、险峻的山岭、蜿蜒的河谷、茂密的森林、浩瀚的草原……中华大地幅员辽阔、物华天宝,万物生灵相依相伴、互惠互生,共同奏响一曲波澜壮阔的生命之歌。"植物斯生,动物斯止。"从创世神话到部落传说,从民族图腾到宗庙祭祀,从游牧渔猎到农耕家畜,从土木建筑到衣冠纹饰,动物文化伴随着华夏文明,走过悠悠五千年岁月历程。地载万物,生生不息自上古神话到民间传说,动物便是人类从未离开的伙伴。女娲拈土造物,相传也是初一造鸡、初二造狗、初三造猪、初四造羊、初五造牛、初六造马,初七     

A spectral mixture model analysis of the Kuroshio variability and the water exchange between the Kuroshio and the East China Sea

For understanding more about the water exchange between the Kuroshio and the East China Sea,We studied the variability of the Kuroshio in the East China Sea(ECS) in the period of 1991 to 2008 using a three-dimensional circulation model,and calculated Kuroshio onshore volume transport in the ECS at the minimum of 0.48 Sv(1 Sv ;106 m3/s) in summer and the maximum of 1.69 Sv in winter.Based on the data of WOA05 and NCEP,The modeled result indicates that the Kuroshio transport east of Taiwan Island decreased since 2000.Lateral movements tended to be stronger at two ends of the Kuroshio in the ECS than that of the middle segment.In addition,we applied a spectral mixture model(SMM) to determine the exchange zone between the Kuroshio and the shelf water of the ECS.The result reveals a significantly negative correlation(coefficient of-0.78) between the area of exchange zone and the Kuroshio onshore transport at 200 m isobath in the ECS.This conclusion brings a new view for the water exchange between the Kuroshio and the East China Sea.Additional to annual and semi-annual signals,intra-seasonal signal of probably the Pacific origin may trigger the events of Kuroshio intrusion and exchange in the ECS.     

日照茶树种植区表层土壤营养元素地球化学特征分析

对土壤中的营养元素进行分析,对于茶树种植及宜种性评价意义深远。该研究主要是利用1 km×1 km表层土壤采样数据,借助地统计学和GIS技术对日照茶树种植区表层土壤中主要营养元素的地球化学特征进行分析。结果表明,研究区N,P,K2O,S含量相对较丰富,而其他营养元素相对较贫乏;营养元素富集区大致以西湖、秦楼、岚山头3个镇为顶点呈三角分布。     

Blasius方程中临界值的分析估计

证明了流体力学边界层理论中著名的Blasius方程的一个新性质,它在二维平板流的研究中具有重要的作用,由此建立它的积分形式,并给出方程中的临界值βc的分析估计。     

内蒙古金厂沟梁金矿床成矿流体特征及稳定同位素研究

对金厂沟梁金矿床含金石英脉中流体包裹体进行了岩相学、显微测温、单个包裹体的激光拉曼测试以及O和S同位素组成等方面研究。结果表明,成矿流体气相成分主要为H2 O,属H2 O-NaCl体系,包裹体均一温度为148.7℃～352℃,盐度[ w （ NaCl ）/％]为1.05％～5.99％。δ18 O值为-1.1‰～3.0‰,说明成矿流体继承了变质流体的特征,仍以岩浆水和后期大气降水为主;δ34 SV-CDT组成为0.6‰～4.3‰,平均值0.817‰,极差为3.1‰,表明成矿流体中的硫主要来自于幔源,其次为围岩。综合分析认为,金厂沟梁金矿床是在燕山晚期太平洋板块俯冲导致岩石圈的快速减薄、拆沉的拉张环境下形成的浅成造山型金矿。     

帮扶村的“守护者”

“当前,新冠肺炎疫情防控阻击战正处于关键时期。疫情就是命令,防控就是责任,局驻村扶贫工作队积极响应号召,敢于担当,履职尽责,第一时间奔赴疫情防控第一线,组织贫困村党员群众筑起防控疫情的坚固防线。截至目前,贫困村均未发现确诊病例和疑似病例。”郸城县自然资源局负责人在新冠肺炎疫情防控会议上说。     

数字地球与跨学科研究浅析

对数字地球的应用模式、关键技术等方面进行了研究。基于数字地球日益成为信息建设的热点 ,本文讲述了数字地球与跨学科研究的关系 ,分析了数字地球的特征。     

珠江口盆地文昌A凹陷地层压力特征及演化史

应用钻井、测井、地震等资料及盆地模拟技术对珠江口盆地文昌A凹陷地层压力特征及演化史进行了研究。结果表明:凹
陷现今储层压力以常压-弱超压为主,深部珠海组三段-文昌组泥岩发育明显的欠压实现象;地层压力演化历经始新世(48~33.9
Ma)、早渐新世(33.9~28.4Ma)和晚渐新世—现今(28.4~0Ma)2个半“增压—泄压”旋回,欠压实作用导致早期超压的形成,晚期超
压则为文昌组和恩平组烃源岩生烃作用所致。压力演化的旋回性主要受控于构造运动的旋回性,断层是超压释放的主要通道。