冰川区积雪中NO3-与粉尘记录的对比研究——以天山乌鲁木齐河源1号冰川为例

为研究山岳冰川积雪中NO3-与粉尘记录之间的联系,利用2003~2005年间新疆天山乌鲁木齐河源1号冰川东支积累区的雪样,分析了雪层中NO3-与不溶微粒的对应关系.研究发现,沙尘活动季节初期,表层雪中NO3-浓度与不溶微粒浓度呈正相关,而与其平均粒径呈负相关,表明NO3-可以通过吸附在粉尘细颗粒表面远距离传输.雪层剖面中NO3-浓度峰值与污化层之间的相对位置在冬半年可基本保持稳定,但夏半年以淋溶作用为主的后沉积过程,会强烈改造NO3-与粉尘记录之间的联系.     

2016~2018年采暖季太行山沿线城市PM2.5污染特征分析

对2016年、2017年采暖季太行山沿线传输通道城市大气中PM_2.5的OC、EC和水溶性离子进行分析,并利用特征组分比值和元素富集因子变化研究该传输通道的污染特征.结果表明,2017年采暖季通道整体较2016年同期空气质量改善良好,PM_2.5浓度由2016年的171.86μg/m³下降为123.90μg/m³.太行山中部城市2017年采暖季较2016年同期PM_2.5浓度下降显著,2a采暖季SNA离子（SO^2-,NO₃^-,NH₄⁺ 3种离子总称）浓度与占比呈现\"北低南高\",加之SNA/EC比值\"北低南高\",表明南部城市二次无机生成较为严重.而OC、EC浓度与占比呈现\"北高南低\",Cl^-/K⁺比值和元素Zn、Ba的富集因子北部均高于南部,表明北部城市可能受燃煤和机动车源等一次排放影响较大;各城市2017年采暖季SO₂、NO₂、CO浓度有所下降,且均呈现\"北高南低\"趋势,进一步表明北部城市一次排放较为严重.     

国外大尺度生态廊道保护进展与秦岭国家公园建设

大型山脉在其走向上往往是生物扩散和分布的天然廊道。然而,由于人类干扰引起的生境碎片化,山地廊道的连通性已大为降低。20世纪以来,人们普遍意识到当前或过去的自然保护措施往往规模太小,无法维持许多物种的长期生存及其所依赖的生态过程。因而,山地廊道的连通性保护日益受到关注,大尺度生态廊道被认为是长远意义上保护气候变化下生物多样性的最优策略。综述连通性保护和生态廊道的概念、发展历程及国外大尺度生态廊道建设实践的经验,并从连通性保护的角度对秦岭国家公园建设提出一些建议,强调大尺度的连通性保护和生态廊道建设对于国家公园自然生态系统的长远保护具有重要意义。     

秦岭地区生态环境质量时空变化及驱动力分析

秦岭被誉为中国的“绿芯”,拥有丰富的生物多样性和重要的生态服务价值. 基于GEE平台,结合MODIS遥感影像数据,采用主成分分析法构建了遥感生态指数（RSEI）,并综合运用Theil-Sen趋势分析、Mann-Kendall检验、Hurst指数模型和地理探测器,研究秦岭地区2002~2022年RSEI的变化趋势及持续特征,并探究其驱动因素. 结果表明：①时间尺度上,秦岭地区RSEI稳定增长,2002~2022年中增长区面积占比达到75.96%,且整体水平较高,多年均值为0.59. ②空间尺度上,秦岭地区RSEI呈现出“中部高,南北低”的分布特征,山麓地带受城镇化发展影响深刻. ③动态角度分析表明,秦岭地区RSEI变化以增长趋势为主. 结合Hurst指数,44.04%的秦岭地区的RSEI在未来会继续保持良好的状况. ④地理探测器分析表明,年平均气温和土地利用类型对秦岭地区RSEI的空间分异影响最大,且人类活动加快了城市化的进程,同时对生态环境的影响也越来越剧烈.     

热带增宽及其对中国东部亚热带森林植被的影响

全球气候变暖已是不争的事实,现今气候变暖的趋势已由每百年（1901--2000）增加0．6℃的记录升高为0．74℃（1906—2005）。其中高纬度地区增温特别显著,成为世界关注的热点。与之对比,热带地区的气候变化以及热带森林对它的反应报道甚少。事实上,自1970s中期以来,热带温度是每lO年升高0．26oC;同时气候模型预测到本世纪末热带地区温度将上升2．1-4．5℃。这些预测是有根据的,但究竟不是直接的证据。因此,本文综合了许多专家对热带地球物理学和大气层特性的多年观测、分析和研究的成果,其结论认为：至少自1979年以来许多热带大气层固有的特征发生变化并向地球极地推进和位移,这些根据是：（1）热带高空的哈德利环流增强并向极地扩展;（21位于热带边缘的亚热带射流向极地移动;（3）热带亚热带对流层顶高度和位置的变化;（4）热带高空平流层臭氧柱总量浓度的变化。据上述特征的变化证明数十年来热带向极地增宽纬度2°～5°（～8°）,一般确认为2．5°。由于热带增宽的驱动,广东50年的气温记录表明气候持续变暖,按增暖趋势推算,预估到2020年,现在的雷州半岛南部可能变成中热带;广东东南沿海将由目前的南亚热带变为北热带（占全省面积约1／3）;其余大部分地区为南亚热带;中亚热带基本上将退出广东（仅剩下东北角一偶）。此预测意味着南岭地区将成为南亚热带的边缘地。     

祁连山区亚高山灌丛土壤含水量的空间分布与月份变化规律

为了探究祁连山区不同灌丛类型的土壤水分时空变异规律,论文以祁连山排露沟小流域的箭叶锦鸡儿（Caragana jubata）、吉拉柳（Salix gilashanica）、金露梅（Potentilla fruticosa）、鲜黄小檗（Berberis diaphana）、甘青锦鸡儿（Caragana tangutica）5种灌丛为对象,建立固定样地,进行了一个生长季的分层（0~10、10~20、20~30、30~40、40~60 cm）土壤含水量监测。结果表明：1）在各灌丛类型样地之间,土壤含水量差异很大,由大到小依次为：箭叶锦鸡儿>吉拉柳>金露梅>鲜黄小檗>甘青锦鸡儿。2）在小流域内空间尺度上,地形（海拔、坡向）、气象（降水、温度）、植被、土壤等作为主要因素共同影响着土壤含水量的差异,导致土壤含水量的空间分布具有随海拔（降水）升高而增大、随地形遮荫作用增强而增大（阴坡高于阳坡）的变化规律。3）不同灌丛类型样地土壤含水量在生长季内各月的变异程度均为弱变异或中等变异,相同土层含水量变异系数大小顺序基本为：鲜黄小檗>箭叶锦鸡儿>吉拉柳>金露梅>甘青锦鸡儿。     

Watershed factors affecting stream acidification in the White Mountains of New Hampshire,USA

The streams tributary to acidic Cone Pond, pH 4.5–4.8, and circumneutral Black Pond, pH 5.3–6.4, in the White Mountains of New Hampshire, USA, were monitored for a year. The watersheds of these two ponds were characterized in terms of geology and stream hydrology. Chemical gradients and patterns in rock weathering and groundwater discharge explain many of the differences in mineral content and acidity of the streams. The rocks of Black watershed produced an average of ten times the equivalent of basic cations as rocks from Cone watershed. This is on the same order as the difference in acidity of the two streams. Down-stream changes in stream chemistry follow differing patterns, but reflect the same principle of residence time and water path length controlling chemical evolution of streamwater. Watershed and aquatic managers may use these parameters in an inexpensive and simple assessment of the susceptibility of individual streams and ponds to acidification. A method is recommended to determine quickly the potential influence of bedrock type to aquatic chemistry.     

Sustainability Assessment for Agriculture Scenarios in Europe’s Mountain Areas: Lessons from Six Study Areas

Sustainability assessment (SA) is a holistic and long-range strategic instrument capable of assisting policy-making in electing, and deciding upon, future development priorities. The outcomes of an SA process become more relevant and strengthened when conducted with multi-stakeholder engagement, which provides for multiple dialogues and perspectives. This was the object of research of the SA team in the context of BioScene (Scenarios for Reconciling Biodiversity Conservation with Declining Agriculture Use in Mountain Areas in Europe), a three-year project (2002–2005) funded by the European Union 5th Framework Program, which aimed to investigate the implications of agricultural restructuring and decline for biodiversity conservation in the mountain areas of Europe, using three distinct methodological streams: the ecological, the socio-economic, and the SA approaches. The SA approach drew on the previous two to assess the importance for biodiversity management of different scenarios of agri-environmental change and rural policy in six countries (France, Greece, Norway, Slovakia, Switzerland, and the United Kingdom), develop causal chains, include stakeholder views, and identify potential contributions for, or conflicts with, sustainability. This article tells how SA was used, what sustainability meant in each study area through different objectives of sustainability considered, discusses the methods used in SA, and the benefits arising. The SA was conducted by a team independent of any study area, who developed and oversaw the application of the SA methodology, assisting national teams, and developing a cross-country understanding of the sustainability of proposed scenarios in the different geographical and social contexts, and their implications for policy-making. Finally, it reflects on the persistent challenges of interdisciplinary research, compounded by multi-cultural teams, and concludes on the BioScene’s lessons for the further development and application of SA.

Grassy balds of the Great Smoky Mountains: Their history and flora in relation to potential management

The origin of the grassy balds of the Great Smoky Mountains is examined. Some of the areas were cleared by settlers. Grazing by sheep and cattle and the cutting of trees were probably the most important factors in maintaining the grass sward; fire apparently was not used.Vegetation survey plots indicated that little of the original balds' area was still grassy and that most of the invading trees and shrubs could be expected to sprout if cut or burned. Areas presently trampled or mowed had a flora similar to a bald that was still grazed. High-elevation burn scars had many species in common with the grassy balds but had dissimilar community structures; therefore, a policy favoring natural fires would be unlikely to encourage maintanence or formation of grassy balds.The management of open grassy areas on National Forest lands was investigated. Burning was the favored technique, although hand cutting, mowing, and grazing were used. The results of testing various management practices on Gregory Bald are reviewed in terms of cost, impact, and historical authenticity. Implications for park management are discussed.     

Trail erosion patterns in Great Smoky Mountains National Park

All the maintained trails in Great Smoky Mountains National Park were surveyed for width, depth, and a variety of types of erosion. Trail erosion is related to a number of environmental variables, including vegetation type, elevation, trail slope, and section of the park. Open grass balds and spruce-fir forest are the most erosion-sensitive plant communities, and the xeric oak and pine types are the least sensitive. Trails in virgin or mature forest tend to be in poorer condition than those in successional areas. The most important physical factor is the slope of the trail.Trails in the Tennessee district are in slightly poorer condition, on the average, than those in the North Carolina district, but the Appalachian Trail is more eroded than either. A poor section of the park may have ten times the erosion of a good section. On an allpark basis, water erosion is the most important problem, with 15% of the trail surface affected.A comparison of visitation patterns with trail condition indicates that redistribution of use would help to mitigate some erosion problems. Because trail condition is correlated to physical environmental factors, however, some sites will require intensive maintenance, even if visitation is low.The data from this survey have already been used in environmental analysis of proposed developments within the park and can be applied to long-range planning for the park trail system as a whole.