木质居室环境综合评价

采用模糊数学理论研究人们对木质居室环境的综合评价,并将其与传统建筑物的室内环境进行了比较。通过调查研究表明,专家们对木质复合墙体结构住宅的室内环境的评价较高,这种结构的住宅在人们的主观意识中能得到认可。     

Review on the roles and effects of growing media on plant performance in green roofs in world climates

Growing media (substrate) is a fundamental part of a green roof, providing water, nutrients and support to plants. However, little research has reviewed how it affects plant performances in different climatic regions. This study aims to analyse published research on green roof growing medium across world’s climate zones. Findings are structured according to Köppen–Geiger climate classification, aiming to investigate the prevalence of research conducted in different climate zones. Results from full-scale studies and laboratory or greenhouse experiments were reviewed. The later were included as they provide systematic knowledge on the effect of individual factors on system performances although cannot provide climate specific information. Studies discussed effects of major substrate components and depths on plant survival and establishment using standard test procedures. Results showed that most research in the subject were in temperate (group C climate classification), continental (group D) and dry climates (group B), respectively. Considerable number of investigations was conducted in controlled laboratory or greenhouse environments. Based on the results, future green roof research and guidelines should consider climate specifications of the region in designing growing medium, depths and attribute of green roof substrates in order to ensure enhanced plant performance. Especially, for more fragile but less investigated dry climate, considerations should be made to tackle heat fluctuations and drought stress by enhancing water holding capacity and thermal isolation of the substrate. To move forward, sustainable building solutions as a part of future urban forms, climate-adaptive green roof systems should be included into future research, practice and guidelines.     

青藏高原东北部牧区气候暖干化趋势及对环境和牧草生长的影响

对20世纪80年代以来青藏高原东北部青南牧区和甘南牧区气候变化的统计分析表明,该地区呈现出气温升高、降水量减少和蒸发量增大的明显趋势。两个牧区年平均气温升高的边际倾向分别为0 3℃/10年和0 5℃/10年,年降水量减少的边际倾向分别为-28 6mm/10年和-23 5mm/10年。90年代该地区主要牧业县多年平均气温普遍比60～70年代升高了0 4℃～0 8℃;多年平均降水量减少的趋势尤以甘南牧区明显,最多可减少87 5mm。同时牧草返青期和枯黄期气温升高,使牧草生长期天数增多。气温升高导致地面蒸发量增多,两个牧区气温升高1℃时,年蒸发量分别增多99mm和114mm。气候变暖干旱,造成天然草地产草量下降。曲麻莱县年降水量减少1mm时,0 0667hm2草地产草量将减少1 6kg;夏河县年平均气温升高1℃时,0 0667hm2草地产草量将减少122 6kg。气候暖干化,已经造成该地区干旱缺水,草地退化、沙化和鼠害猖獗,使草畜矛盾不断加剧,已严重威胁到牧区的生存和发展,也影响到长江、黄河中下游地区的可持续发展,对此应予高度重视。     

中国水土流失问题的初探

长期以来,水土流失直接威胁着人们赖以生存的环境,在所有的生态破坏中,水土流失称之为“环境破坏第一杀手”。针对我国山地丘陵面积大、地质条件复杂、人为破坏加速、水土流失严重的实际情况,通过丰富的历史资料和整治经验及野外工作所积累的大量数据分析,以生态恢复学为指导,总结了水土流失的基本特点,研究了水土流失治理与经济可持续发展的关系,探讨了水土流失给生态安全造成的巨大危害,展望了水土保持的预期目标,根据中国的实际情况,提出了综合治理的基本思路。     

基于GIS的蒲江县生态环境综合评价研究

针对龙门山区域生态环境受到了"5·12"汶川大地震重创的现实问题,选取蒲江县为例,构建目标层、制约层、要素层的三级评价体系,建立了生态环境综合评价模型,并运用层次分析法及GIS技术开展生态环境综合评价。结果表明:蒲江县生态环境良好率(第Ⅲ分类区以上)达到了87.6%,总体生态环境状况良好,同时提出了生态保护对策。     

基于YOLOv5s-ESTC的肉苁蓉检测

为了解决因梭梭和红柳等宿主遮挡、样本分布密集、样本大小不均衡等造成人工种植肉苁蓉检测精度低以及模型参数量过大难以向嵌入式设备移植等问题,该研究提出一种基于改进YOLOv5s的人工种植肉苁蓉轻量化检测方法。首先,将YOLOv5s的主干网络替换为EfficientNetv2网络,以减少模型参数量和计算复杂度进而实现模型轻量化,便于后期将模型向嵌入式设备部署;其次,为了增强模型对小目标肉苁蓉特征信息的提取能力,将C3模块与Swin Transformer Block进行整合,得到C3STR模块,将其引入主干网络,并将其输出的特征图与Neck网络中的特征图进行融合;最后,在检测头前端与颈项加强网络之间添加CA注意力机制,以弱化背景信息、聚焦目标特征,提高网络检测性能。试验结果表明,该模型对于肉苁蓉的检测精度和准确率分别为89.8%和92.3%,模型的参数量和计算量分别为5.69×10⁶ MB和6.8 GB,权重文件大小为11.9 MB,单幅图像推理时间为8.9 ms,能够实现实时性检测。同其他主流模型相比,改进后的模型的检测精度分别比SSD、Faster R-CNN、YO...     

水资源联合调度模型在额济纳绿洲生态环境建设中的应用

对日趋缺水的额济纳绿洲,进行河水与地下水进行联合运用的目的是:减少水资源浪费,恢复生态水位,保护绿洲。按照国家水利部(1997)496号文件:《现状工程条件下黑河干流水量分配方案》(简称“97甘蒙分水方案),不同保证率下分配给内蒙古的水量。根据狼心山水文断面入境水量丰枯变化的分析结果,建立水资源联合调度模型,对四种不同来水方案进行计算。结果表明,执行“甘蒙分水”,采用内蒙长衬砌渠道输水,当保证率P=50%时,入境狼心山水量为7.527×108m3,到2020年地下水位埋深回升到2.35m,相应绿洲面积将扩大到5005.01km2,绿洲植被总盖度可达到58%。基本满足天然非灌溉林草的需水,逐步回补到生态要求的限定水位,使绿洲逐步得到恢复。     

塔里木河流域水量变化对生态环境影响分析

本文以塔里木河流域的10个水文站1961~2000年观测资料为基础,对塔里木河流域的径流变化及其对下游生态环境影响进行了分析。分析得出:(1)20世纪60年代以来,塔里木河各源流的出山口径流量增加23.82×108m3,增幅达14.97%,但是,能汇入塔里木河干流的水量并没有增加,而且比60年代减少了8.8×108m3,减幅达17.41%。(2)近40年以来,由于塔里木河干流上中游地区的耕地面积急剧扩大,用水量剧增,使下游的来水量比60年代减少7.72×108m3,减幅达76.13%。(3)由于塔里木河上中游耗水量的增加,塔里木河下游来水量逐年减少以至断流,由此造成下游生态环境出现较大的变化,主要表现有:河水盐化严重,灾害性天气出现的次数大幅增加,河道断流,地下水位下降,天然植被严重衰败,沙漠化过程加重。(4)实施塔里木河流域水资源的统一管理,统筹分配上、中、下游水量,调整大农业生产方向,完善流域节水改造配套工程,发展节水型农业,是塔里木河下游受损生态环境恢复与重建的关键。     

乌鲁木齐都市圈投资环境分析

随着我国同中亚五国经济合作的不断升温,加上乌鲁木齐都市圈优越的自然条件和独特的区位优势,其面临着经济发展前所未有的机遇。因此,如何尽快改善该区的投资环境,吸引更多资金,是一个亟待解决的课题。本文从地理、经济、政治、社会等方面全面分析了整个都市圈的投资环境,在分析其优势和劣势的同时,提出了可行性的建议和对策,目的在于发挥优势,减小劣势,提高综合投资环境水平,促进经济的快速发展。     

DMPP mitigates N2O and NO productions by inhibiting ammonia-oxidizing bacteria in an intensified vegetable field under different temperature and moisture regimes

Vegetable soils with high nitrogen input are major sources of nitrous oxide (N₂O) and nitric oxide (NO), and incorporation of the nitrification inhibitor 3, 4-dimethylpyrazole phosphate (DMPP) into soils has been documented to effectively reduce emissions. However, the efficiency of DMPP in terms of soil N₂O and NO mitigations varies greatly depending on soil temperature and moisture levels. Thus, further evaluations of DMPP efficiency in diverse environments are required to encourage widespread application. A laboratory incubation study (28 d) was established to investigate the interactive effects of DMPP, temperature (15, 25, and 35 ℃), and soil moisture (55% and 80% of water-holding capacity (WHC)) on net nitrification rate, N₂O and NO productions, and gene abundances of nitrifiers and denitrifiers in an intensive vegetable soil. Results showed that incubating soil with 1% DMPP led to partial inhibition of the net nitrification rate and N₂O and NO productions, and the reduction percentage of N₂O production was higher than that of NO production (69.3% vs. 38.2%) regardless of temperature and soil moisture conditions. The increased temperatures promoted the net nitrification rate but decreased soil N₂O and NO productions. Soil moisture influenced NO production more than N₂O production, decreasing with the increased moisture level (80%). The inhibitory effect of DMPP on cumulative N₂O and NO productions decreased with increased temperatures at 55% WHC. Conversely, the inhibitory effect of DMPP on cumulative N₂O production increased with increased temperatures at 80% WHC. Based on the correlation analyses and automatic linear modeling, the mitigation of both N₂O and NO productions from the soil induced by DMPP was attributed to the decreases in ammonia-oxidizing bacteria (AOB) amoA gene abundance and NO^-₂-N concentration. Overall, our study indicated that DMPP reduced both N₂O and NO productions by regulating the associated AOB amoA gene abundance and NO^-₂-N concentration. These findings improve our insights regarding the implications of DMPP for N₂O and NO mitigations in vegetable soils under various climate scenarios.