秸秆还田对汉中盆地稻田土壤有机碳组分、碳储量及水稻产量的影响

为探索稻麦或稻油轮作制下,小麦、油菜秸秆还田对汉中盆地稻田土壤碳库组分的变化,设置小麦秸秆不还田(WSN)、小麦秸秆常规还田(WS)、小麦秸秆促腐还田(WSM)、油菜秸秆不还田(RSN)、油菜秸秆常规还田(RS)、油菜秸秆促腐还田(RSM),共6个处理,通过大田试验研究了不同秸秆类型及还田方式对稻田0—5,5—10,10—15,15—20,20—25cm 5个土壤层次中的土壤容重、总有机碳(TOC)、活性有机碳(LOC)、活性有机碳效率(ACL)、碳储量(SCS)、碳库管理指数(CPMI)及水稻产量的影响。结果表明:秸秆还田显著降低0—15cm土层容重,对15—25cm并未产生显著影响。与不还田相比,秸秆还田明显增加了各层次土壤有机碳库指标含量,但TOC和LOC含量均随土壤深度的增加而减少,两者在0—15cm土层含量较高,具有明显的表层富集现象;与不还田相比,小麦及油菜秸秆还田后可明显增加稻田0—25cm土层中的土壤碳储量(SCS),增幅可达21.9%~23.5%和1.7%~6.7%。不同土层中的LOC、ACL、CPIM对秸秆类型的响应不同,具体表现为小麦秸秆还田(WS、WSM)对0—15cm土层具有显著促进作用,而油菜秸秆还田(RS、RSM)对15—25cm土层中的有显著促进作用。产量方面,秸秆促腐还田模式下(WSM、RSM)水稻产量最高,常规还田模式(WSN、RSN)次之,而不还田时产量最低。相关分析显示0—10cm土壤活性有机碳有效率与水稻产量显著相关。秸秆还田是提高汉中盆地稻田土壤有机碳和产量较为有效的农田管理措施。两种轮作模式下,小麦秸秆全量旋耕还田更有利于固持稻田土壤有机碳和增加水稻产量增加。     

基于集对分析的区域水资源开发利用综合评价

基于集对分析方法建立了区域水资源开发利用程度的评价模型，并应用该模型对汉中盆地水资源的开发利用程度进行了综合评价。评价结果表明，汉中盆地水资源利用处于中、低级阶段，还有很大的开发潜力。通过与模糊模式识别、模糊综合评判、属性识别方法、人工神经网络方法进行对比分析，可以看出集对分析模型不仅理论严谨、方法简便，而且评价结果精确可靠，从而验证了该方法的合理性和可行性。因此，集对分析理论为区域水资源开发利用程度的综合评价提供了一种新的思路。     

苏南河网水污染控制系统规划优化研究

以苏南某地二级树状河网为例,在运用S-P水质模型模拟河网水质的基础上,构建了以河网污水处理费用及引水稀释费用之和最小为目标函数的水污染控制最优化模型,采用遗传算法,对各引水口的引水量及河网中各排污口的污水处理率进行优化计算,供苏南地区水系规划与管理参考。     

近50年来黄河源区水文要素周期性分析及模拟

寒区水文过程是寒区生态系统中的重要环节之一,水热状况将直接决定高寒地区的生态环境状况.用滑动趋势法和墨西哥帽状小波变化分别获取了研究区域近50年来气候变化的年际年代变化及其周期分析,基于青藏高原太阳辐射平衡已有成果,结合联合国粮农组织推荐的彭曼-蒙蒂斯模型,对于达日县可能蒸散发进行了数值模拟.得出以下主要结论:近50年来达日县降水年增加率为0.557 mm/a,而该县最大可能蒸散发量的年增加率为0.132 mm/a,气候总体趋势是由干旱向湿润方向发生转变;达日县年气温序列主要呈现20 a、15 a、7 a和5 a的周期振荡,年降水序列表现为15～20 a和7～8 a的周期振荡;近20年来可能蒸散发呈递减的趋势,汛期序列递减率为0.046 7 mm/a,冬春序列递减率为0.108 4 mm/a.     

基于遥感的疏勒县植被覆盖时空变化研究

【目的】评价疏勒县生态环境质量及生态环境演变过程。【方法】基于Landsat遥感影像数据,利用归一化植被指数NDVI、像元二分模型、中心迁移模型等方法分析了1996-2017年疏勒县植被覆盖时空演化。【结果】①疏勒县植被覆盖分布总体以高植被覆盖为主成大面积片状分布,中、低植被覆盖主要以盖孜河和克孜河为轴线,相对围绕高植被覆盖分散分布;②1996-2017年疏勒县植被覆盖面积和覆盖度均呈增加趋势。2017年的植被覆盖面积比1996年增加了456.4 km²,增加率为38.3%;③疏勒县植被覆盖空间变化上存在一定的区域性和时段性差异。区域上,南部乡镇覆盖度明显增加;时段上,2009-2013年植被覆盖面积增加最明显;④1996-2017年疏勒县植被覆盖中心整体往东南迁移;⑤气候变暖对疏勒县植被覆盖度变化有一定的影响,但短期内人类活动影响更大。灌区改造高效节水、耕地开垦、农作物的种植及林带面积的增加是植被覆盖面积增加的主要因素。【结论】综上可知,气候变暖和生态治理工程等人类活动因素可能是疏勒县植被覆盖面积与覆盖度呈增加的主要原因,这表明疏勒县生态环境保护与治理是科学合理的。     

The significance of meandering channel morphology on the diversity and abundance of macroinvertebrates in a lowland river in Japan

• 1. Many rivers and streams across the world have been channelized for various purposes. Channel cross‐sections of meandering rivers are asymmetrical and have cross‐sectional diversity in their physical environment; cross‐sections of a channelized river are typically trapezoidal and have little cross‐sectional diversity, both in physical and ecological conditions. Several programmes to restore stream meanders have been undertaken to improve river ecosystems degraded by channelization. However, the association between diversification in the physical environment due to meander restoration and the macroinvertebrate community structure is poorly known.
• 2. This study of a lowland river in Japan assessed how the cross‐sectional diversity of the physical environment changed with restoration of a meander in a channelized river, and how the macroinvertebrate communities responded to the changes in physical habitat variation. Comparisons were made between the macroinvertebrate communities of a channelized reach, the restored meandering reach, and a natural meandering reach.
• 3. Natural meandering and restored meandering reaches showed higher cross‐sectional diversity in physical variables and total taxon richness across a reach than did the channelized reach. Almost all taxa observed in the natural and restored meandering reaches were concentrated in the shallowest marginal habitats near the banks. Shear velocity increasing with water depth had a negative association with macroinvertebrate density and richness.
• 4. This study demonstrated that the shallow river bed along the inside of bends formed point bars that provided a highly stable substrate, a suitable habitat for macroinvertebrates in a lowland river. It is concluded that meander restoration could be an effective strategy for in‐stream habitat restoration in lowland meandering rivers.

Copyright © 2007 John Wiley & Sons, Ltd.     

Condition assessment of lamprey populations in the Yorkshire Ouse catchment,north‐east England,and the potential influence of physical migration barriers

• 1. River lamprey (Lampetra fluviatilis) and sea lamprey (Petromyzon marinus) are designated features of the River Derwent Special Area of Conservation (SAC) and the Humber Estuary (a possible SAC). This study determined the condition of lamprey populations in the Yorkshire Ouse catchment by assessing the species composition, distribution, abundance and size‐structure of larval (ammocoete) populations in five major tributary rivers (Derwent, Swale, Ure, Nidd and Wharfe).
• 2. According to EU condition assessment criteria, Lampetra populations (assumed to be mostly river lamprey) are at present in favourable condition, with site mean (±SE) densities ranging from 2.7 (±1.2) to 160.3 (±50.5) individuals m^?2 (all river means >2 individuals m^?2), and at least two size (≈age) classes present in optimal microhabitats. By contrast, no sea lamprey larvae were recorded, suggesting that populations of this species are in unfavourable condition.
• 3. Actions to protect and enhance nationally or internationally important stocks must be implemented from at least a catchment perspective, because many of the issues affecting such species are not localized. With respect to lampreys, particular attention should be given to protecting spawning and nursery habitats, improving water quality, reducing impingement at abstraction points, preventing exploitation at spawning grounds and increasing passage at potential physical obstructions.

Copyright © 2007 John Wiley & Sons, Ltd.     

沈阳市河流生态建设项目实施建议

近年来,因干旱少雨等自然灾害影响及人类生产活动对环境的破坏,致使一些中小河流生态功能遭到不同程度的破坏。结合沈阳市近年来河流生态建设的实施情况,从工程措施和生物措施两方面详细介绍了针对不同河流状况的生态建设措施,对今后类似工程建设提供借鉴。     

小型自排沉沙池沉沙工况的水力学特性试验研究

首先介绍了小型自排沉沙池的工作原理与工作过程,然后以物理模型对小型自排沉沙的水力学特性进行试验研究,通过试验资料深入分析了小型自排沉沙池内水流的流态特征,流速分布等水力特性。试验研究旨在为进一步研究小型自排沉沙池沉沙工况提供依据。     

河道淤泥气泡混合轻质土剪切流变特性及模型

利用剪切流变试验对以水泥为固化剂的河道淤泥气泡混合轻质土的流变特性进行了试验研究。试验结果表明,经固化处理的河道淤泥气泡混合轻质土在荷载作用下具有类似于硬粘性土的流变特征。剪切流变可以分为3个阶段：在剪应力水平较低时,剪切流变曲线呈衰减稳定型;随着剪应力水平的提高,剪切流变曲线呈非稳定的等速型;当剪应力水平增大到一定程度时,剪切流变曲线呈加速型。河道淤泥气泡混合轻质土的流变性随着混合轻质土强度的提高而降低。根据试验所呈现的剪切流变规律,可以发现河道淤泥气泡混合轻质土的剪切流变符合七元件黏弹塑性剪切流变模型,模型能够比较好地描述河道淤泥混合轻质土在各种剪应力水平下的衰减、等速以及加速流变过程。