浑善达克沙地退化草地的封育效果调查

封育保护是促进退化草地自然恢复的有效方法之一,为了研究实施京津风沙源工程措施以来浑善达克沙地沙质草场的围封效果,我们特对浑善达克沙地南缘地段的围封草场进行了调查,并取得了一些结果。     

生态围隔对水源地水质的改善效果

采用渔网及土工布挂片双层材料以及填充的水花生构建了生态围隔,对藻类进行拦截,降低取水口藻类密度,同时通过水花生的吸收和拦截,以及土工布挂片形成的附着生物群落的降解和吸收作用,降低颗粒态以及溶解态营养盐,达到取水口水质的改善效果.生态工程实施后,取水口内悬浮颗粒物显著降低了29.8％,同时透明度提高了27.5％.对藻类的拦截效果研究表明,围隔对叶绿素a的去除率为23.0％,对总藻类数量的去除率为20.7％.通过对围隔内外蓝藻数量在藻类数量的比例分析,生态围隔对蓝藻的去除率高于总藻类的去除率,说明了对于藻类拦截的效果具有一定的选择性.对营养盐的改善效果主要体现在颗粒态物质上,其中颗粒态氮磷的去除率分别为48.4％和31.3％.     

围网养殖对洪湖水质的影响分析

文章从围网养殖对洪湖水质影响的角度出发,依据1990～2006年在洪湖实测的水质数据分析了洪湖水质的时空变化过程及趋势,并发现水质指标中总氮的超标量变化明显。利用环境污染综合指数法,通过围网内和围网外以及围网前和围网后不同水文期的水质情况对比,对洪湖水质变化进行综合评价。结果表明围网内的环境污染综合指数在枯水期要远大于围网外的,围网养殖对湖泊的局部污染严重;围网前水质基本可以达到Ⅱ类水质标准,开始围网后洪湖水质逐步恶化,且围网养殖面积与水质恶化的程度有着相同的变化趋势,总氮的含量变化尤为明显,随着围网养殖规模面积的扩大急速增加。     

基于PSR的围圩养殖区湖泊湖荡群水生态系统健康评价

以典型围圩养殖区江苏省里下河腹部地区的41个湖泊湖荡为研究对象,分析筛选了围圩养殖对生态系统影响的主要指标,基于PSR方法评价了湖泊湖荡群的水生态系统健康状况.结果表明,选取的养殖面积占比、斑块密度及退圩还湖政策规划等指标能够有效反映区域的围圩养殖特色,全面表征围圩养殖对生态系统压力、状态、响应的影响.评价结果显示,里下河腹部地区41个湖泊湖荡中综合指数等级健康的占比4.9%,亚健康的占比87.8%,不健康的占比7.3%.研究结果可为围圩养殖区湖泊水生态系统健康评价、退圩还湖及水生态修复规划提供重要的技术方法.     

Frontiers created by ‘the Others’

ABSTRACT

This paper highlights the colonized perspective, and aims to reflect on the consequences of a predominant perspective of land control and use for Amazonian indigenous people. The demarcation of indigenous territories has been presented by external public actors, the ‘Others’ to explicitly support indigenous people defend their territories. However, demarcation effectively creates a frontier and enclosure which contribute to alienate indigenous people within their new territories. Amazonian groups normally maintain that they belong to the Land, and their historical use of a determined land has been asserted by anthropological studies. But they belong to Land. In contrast, occupying a territory to generate profit allows the exploitation of everything inside it. Every form of extraction helps to reproduce the colonial logic. A key question we need to address is, therefore: Why do the ‘others’ not feel that belonging?     

云南剑川杂岩体岩石包体特征及成因

本文根据云南剑川杂岩体中岩石包体的分布、大小、形态、岩石类型、化学成分及矿物组成特征,探讨包体的成因,并推测寄主岩浆岩的性质、来源。认为剑川杂岩体中的岩石包体可分为捕虏体和同源包体,同源包体又可分为析离体和堆积岩。推测的岩体初始岩浆温度为1000—1125℃,形成深度约为20—30km。     

Microbial Fe(III) Reduction in Acidic Mining Lake Sediments after Addition of an Organic Substrate and Lime

To elucidate the role of Fe(III) reduction in mining lake sediments amended with organic substrates, we performed a large (10 m diameter) enclosure experiment in which sediments were amended with Carbokalk, a waste product from sugar industry containing organic carbon and lime. Fe(III) reduction rates were determined monthly by measuring the accumulation of Fe(II) in the sediments in the field. Fe(III) reduction rates were also determined by incubating sediment samples with synthetic Fe(III) oxyhydroxide under in situ temperature in the laboratory. Sulfate reduction was selectively inhibited in the Fe(III) reduction experiments by addition of sodium molybdate. Sulfate reduction was measured by accumulation of reduced inorganic sulfides in the field and by ³⁵S radiotracer using a core injection technique. Sediment incubation and determination of sulfate reduction rates with radiotracer showed that sulfate reduction and direct microbial Fe(III) reduction occured simultaneously in the upper centimeters of the sediments and that both processes contributed to alkalinity generation. However, Fe(III) reduction was the initial process and rates were at least 3.5 fold higher than sulfate reduction rates. The results indicate that the presence of suitable anions for Fe(II) precipitation as carbonate or sulfide is needed in order to prevent loss of potential alkalinity by Fe(II) diffusion and reoxidation in the water column.     

气密性高等级生物安全实验室的负压控制

提出漏风量换气次数的概念,并以此作为评价气流控制阀是否适用于生物安全实验室压差控制的指标;提出引入附加漏风量的气密性生物安全实验室压差控制策略。进行对比实验,研究实验室在无人为漏风量与引入人为漏风量这两种情况下启动、微扰动、关门等工况下实验室的压差波动情况,其结果显示在引入人为漏风量情况下实验间压差波动范围减小、稳定速度加快。从而说明引入附加漏风量的压差控制策略在气密性生物安全实验室的压差控制方面具有重要的实际应用价值。     

Emission of volatile organic compounds (VOC) from tropical plant species in India

Foliar emission of volatile organic compounds (VOC) from common Indian plant species was measured. Dynamic flow enclosure technique was used and the gas samples were collected onto Tenax-GC/Carboseive cartridges. The Tenax-GC/Carboseive cartridges were attached to the thermal disorber sample injection system and the gas sample was analysed using gas chromatography (GC) with flame ionisation detection (FID). Fifty-one local plant species were screened, out of which 36 species were found to emit VOC (4 high emitter; 28 moderate emitter; and 4 low-emitter), while in the remaining 15 species no VOC emission was detected or the levels of emission were below detection limit (BDL). VOC emission was found to vary from one species to another. There was a marked seasonal and diurnal variation in VOC emission. The minimum and maximum VOC emission values were < 0.1 and 87 microgg(-1) dry leaf h(-1) in Ficus infectoria and Lantana camara respectively. Out of the 51 plant species studied, 13 species are reported here for the first time. Among the nine tree species (which were selected for detailed study), the highest average hourly emission (9.69+/-8.39 microgg(-1) dry leaf) was observed in Eucalyptus species and the minimum in Syzygium jambolanum (1.89+/-2.48 microgg(-1) dry leaf). An attempt has been made to compare VOC emission from different plant species between present study and the literature (tropical and other regions).     

不同封育年限荒漠草原土壤呼吸日、季动态变化及其影响因子

围封禁牧措施可以改善退化草地生态环境,是我国退化草地植被恢复的主要措施.为探讨干旱区荒漠草原不同围封禁牧年限的土壤呼吸作用特征及影响因子,在生长季连续观测围封禁牧11 a、7 a、放牧不封育(CK)荒漠草原土壤呼吸速率及环境因子,结果表明:1在日、季尺度上,封育11 a、7 a和CK荒漠草原土壤呼吸速率均具有明显的单峰曲线变化规律,在日尺度上,最大、最小值分别出现在12:00~16:00和00:00~06:00;在季节变化尺度上,最大值出现在降水较多温度适宜的8月,土壤呼吸均值表现为11 a[0.143 g·(m2·h)-1]7 a[0.138 g·(m2·h)-1]CK[0.106 g·(m2·h)-1].2封育与未封育荒漠草原的土壤呼吸速率与空气、土壤温度均呈极显著的指数关系(P0.001),相关性大小为:地表温度(R2:0.408~0.413)空气温度(R2:0.355~0.376)5~20 cm土壤温度(R2:0.263~0.394);温度敏感性系数Q10随着土层的加深逐渐变大,不同封育年限Q10表现为11 a(2.728)7 a(2.436)CK(2.086).3封育11 a、7 a和CK荒漠草原土壤呼吸速率与空气湿度、土壤含水量一元二次模型达到显著水平(P0.05),与空气二氧化碳呈极显著线性负相关(P0.01),与风速呈显著线性正相关(P0.05),与光照强度呈极显著线性正相关(P0.01).4干旱区荒漠草原土壤呼吸作用随着围封禁牧年限的增加而增加,温度敏感性系数亦随之增加,0~20 cm土壤温度和水分是其土壤呼吸的主要影响因子.