基于能值理论的长三角沿江城市群生态-经济-社会系统可持续发展态势研究

[目的]对长三角沿江城市群生态—经济—社会系统可持续发展态势进行研究,为该区域生态经济可持续发展提供科学支持。[方法]基于能值理论构建评价指标和评价体系,分析长三角沿江城市群生态—经济—社会系统的可持续发展态势。[结果] 2017年长三角沿江城市群中29%的城市资源过度开发,外部依赖性强;53%的城市环境负载率低,29.4%的城市环境负载率高;11.7%的城市废弃物循环再生能力低;47%的城市能值交换率低,经济竞争力强;35%的城市能值货币率高,经济产出效率低。上海、苏州单位面积能值密度高,23.5%的城市较低;29.4%的城市人均能值福利低;17.6%的城市人口负载率高;41.2%的沿江城市呈可持续发展态势,58.8%的城市呈过度发展态势。[结论] 2017年沿江城市群自给能力、环境压力、生态质量呈现上游城市强、小、优向中游基本协调,下游弱、高、差的渐变态势。上海、苏南城市经济竞争力强,但产出效率低;苏中、皖中地区除省会城市外其他城市竞争力弱;皖南城市经济发展滞后且呈沿江单边孤立发展态势。上海、苏南城市社会可持续发展优,形成人才、资源强吸引同时存在用地短缺问题;苏中城市较均衡并形成弱吸引;除合肥市、铜陵市外,皖中、皖南其他城市发展滞后,缺乏有效吸引。沿江城市群整体可持续发展态势严峻。     

黄河未来输沙量态势及其适用性对策

[目的] 探索黄河输沙预测的新思路，预估黄河未来输沙态势与输沙量水平，为黄河流域生态治理规划提供参考。[方法] 结合黄河流域水土保持生态修复现状，采用单累积曲线法、滑动平均及频率分析方法，分析1950—2019年黄河主要来沙区间的实测输沙量变化特征及其未来态势。[结果] 1950—2019年黄河输沙量呈现阶梯式减少。1950—2019年黄河中游各站累积实测输沙量随时间的变化可用“左半抛物线”表征。黄河输沙量自1997年以来已进入相对稳定态势，目前已达企稳状态；黄河潼关站未来年输沙量在90%频率下为1.00×10⁸ t左右，在10%频率下为5.00×10⁸ t左右，未来多年平均输沙量为1.40×10⁸ t。[结论] 为了维持黄河输沙量低稳状态，提升水土保持措施质量与标准，补齐“后水土保持”短板，构建完善的水沙关系调控体系，维持黄河下游河道冲淤平衡，是黄河流域生态保护与高质量发展的保障。     

1969-2018年黄河实测径流与天然径流的变化

[目的] 分析黄河实测径流与天然径流的变化规律，为探究人类活动对径流的影响提供依据。[方法] 基于1969—2018年黄河干流8个水文站的天然径流和实测径流数据，使用Mann-Kendall趋势检验与突变检验法，对比分析近50 a黄河干流实测径流和天然径流的变化规律。并结合近15 a各分区耗水数据探讨人类活动对于径流的影响。[结果] ①1969—2018年黄河上中下游实测径流整体呈降低趋势，兰州、花园口、利津3个代表站多年平均降低速率分别为5.10×10⁷，3.55×10⁸，4.13×10⁸ m³/a。②近50 a天然径流和实测径流趋势突变主要集中在1986和1990两个年份，结合前人研究和重要水事分析，1986年突变可能与1984年以来一系列水土保持措施实施以及1986年龙羊峡水库修建有关；而造成1990年径流突变的原因可能是80—90年代黄河流域用水量激增和流域下垫面改变。③天然径流与实测径流的差值从上游至下游水文站断面逐渐增大，这主要与近15 a平均耗水量也沿程增大相一致；另外多年平均实测径流在利津站仅占天然径流的42%。耗水量最大的两个分区为花园口以下和兰州—头道拐段，分别达到了1.06×10¹⁰和1.04×10¹⁰ m³。[结论] 人类活动中的各项耗水（尤其是农田灌溉）是造成兰州站以下地区天然径流与实测径流差值大的主要原因，因此，应进一步推进黄河流域节水农业的发展，合理分配各项耗水量。     

Performance and uncertainty analysis of a short-term climate reconstruction based on multi-source data in the Tianshan Mountains region,China

Short-term climate reconstruction, i.e., the reproduction of short-term(several decades) historical climatic time series based on the relationship between observed data and available longer-term reference data in a certain area, can extend the length of climatic time series and offset the shortage of observations. This can be used to assess regional climate change over a much longer time scale. Based on monthly grid climate data from a Coupled Model Inter-comparison Project phase 5(CMIP5) dataset for the period of 1850–2000, the Climatic Research Unit(CRU) dataset for the period of 1901–2000 and the observed data from 53 meteorological stations located in the Tianshan Mountains region(TMR) of China during the period of 1961–2011, we calibrated and validated monthly average temperature(MAT) and monthly accumulated precipitation(MAP) in the TMR using the delta, physical scaling(SP) and artificial neural network(ANN) methods. Performance and uncertainty during the calibration(1971–1999) and verification(1961–1970) periods were assessed and compared using traditional performance indices and a revised set pair analysis(RSPA) method. The calibration and verification processes were subjected to various sources of uncertainty due to the influence of different reconstructed variables, different data sources, and/or different methods used. According to traditional performance indices, both the CRU and CMIP5 datasets resulted in satisfactory calibrated and verified MAT time series at 53 meteorological stations and MAP time series at 20 meteorological stations using the delta and SP methods for the period of 1961–1999. However, the results differed from those obtained by the RSPA method. This showed that the CRU dataset produced a low degree of uncertainty(positive connection degree) during the calibration and verification of MAT using the delta and SP methods compared to the CMIP5 dataset. Overall, the calibrated and verified MAP had a high degree of uncertainty(negative connection degree) regardless of the dataset or reconstruction method used. Therefore, the reconstructed time series of MAT for the period of 1850(or 1901)–1960 based on the CRU and CMIP5 datasets using the delta and SP methods could be used for further study. The results of this study will be useful for short-term(several decades) regional climate reconstruction and longer-term(100 a or more) assessments of regional climate change.     

Time‐varying relationships between ocean conditions and sockeye salmon productivity

Environmental change is occurring at unprecedented rates in many marine ecosystems. Yet, environmental effects on fish populations are commonly assumed to be constant across time. In this study, I tested whether relationships between ocean conditions and productivity of North American sockeye salmon (Oncorhynchus nerka) stocks have changed over the past six decades. Specifically, I evaluated the evidence for non‐stationary relationships between three widely used ocean indices and productivity of 45 sockeye salmon stocks using hierarchical Bayesian models. The ocean indices investigated were the Pacific Decadal Oscillation (PDO), North Pacific Gyre Oscillation (NPGO), and sea surface temperature (SST). I found partial support for time‐varying salmon–ocean relationships. Non‐stationary relationships were strongest for the NPGO and weaker for the SST and PDO indices. Productivity–NPGO correlations tended to shift gradually over time with opposite trends for stocks in British Columbia (B.C.) and western Alaska; for B.C. stocks, the NPGO correlations shifted from significantly negative prior to 1980 to significantly positive after 1990, whereas for western Alaska stocks, the correlations shifted from positive to negative. Productivity–SST correlations showed declining trends for B.C. and Gulf of Alaska stocks, that is, correlations became more negative (B.C.) or less positive (Gulf of Alaska) over time. For the PDO, correlations weakened during the 1980s for western Alaska and B.C. stocks. Overall, these results provide evidence for time‐varying relationships between salmon productivity and environmental conditions over six decades, highlighting the need to recognize that historical responses of salmon populations to environmental change may not be indicative of future responses.     

Management of transboundary and straddling fish stocks in the Northeast Atlantic in view of climate‐induced shifts in spatial distribution

The introduction of 200 n.m. exclusive economic zones (EEZs) in the late 1970s required increased collaboration among neighbouring coastal states to manage transboundary and straddling fish stocks. The established agreements ranged from bilateral to multilateral, including high‐seas components, as appropriate. However, the 1982 United Nations Convention on the Law of the Sea does not specify how quotas of stocks crossing EEZs should be allocated, nor was it written for topical scenarios, such as climate change with poleward distribution shifts that differ across species. The productive Northeast Atlantic is a hot spot for such shifts, implying that scientific knowledge about zonal distribution is crucial in quota negotiations. This diverges from earlier, although still valid, agreements that were predominately based on political decisions or historical distribution of catches. The bilateral allocations for Barents Sea and North Sea cod remain robust after 40 years, but the management situation for widely distributed stocks, as Northeast Atlantic mackerel and Norwegian spring‐spawning herring, appears challenging, with no recent overall agreements. Contrarily, quotas of Northern hake are, so far, unilaterally set by the EU despite the stock's expansion beyond EU waters into the northern North Sea. Negotiations following the introduction of EEZs were undertaken at the end of the last cooler Atlantic Multidecadal Oscillation (AMO) period, that is, with stock distributions generally in a southerly mode. Hence, today's lack of management consensus for several widely distributed fish stocks typically relates to more northerly distributions attributed to the global anthropogenic signal accelerating the spatial effect of the current warmer AMO.     

Typical Travel Events and the Reversal of Modern Image of China

In order to open up the Chinese market,Britain sent two missions to China in 1791 and 1816.The most powerful colonial empire in the world met the most powerful feudal empire in the world.The two sides led the negotiations and exchanges with the concepts of "tribute" and "equal diplomacy",and the failure of the missions of Macartney and Amherst to China was inevitable.The travel texts completed by the members of the mission recorded the process of travel to China and their views on China in detail.Two typical travel events in China completely reversed the western image of China.     

鹅肠道微生物研究进展

肠道微生物是当前研究的热点,鹅肠道微生物的组成与丰富程度不仅和鹅的生长性能密切相关,而且在鹅机体生理活动中具有一定的调节作用,同时与疾病的发生和发展具有密切的联系。通过研究鹅肠道微生物的调节,从而达到促生长或者治疗疾病的目的,是目前鹅研究探寻的新方向。文章主要综述了鹅肠道微生物的组成及其变化规律,以期为鹅产业生物饲料的开发应用、研发推广新型安全高效饲料添加剂提供新思路。     

茂兰自然保护区森林景观格局变化分析

本文以2011年和2017的森林调查成果化数据为基础,依据不同优势树种组,采用景观格局指数法,从组成结构、斑块特征、景观异质性和空间分布4方面分析2011年和2017年茂兰自然保护区的森林景观格局及其变化。结果表明：林地面积增加了654.08 hm²；森林优势树种数量从15种增加至30种；景观面积(CA)最大的均为阔叶混交树种组,增加了1286.33hm²；斑块平均大小(MpS)最大的均为阔叶混交树种组,增加了471.80 hm²；面积加权的平均形状指数(AWMSI)和面积加权的平均分形指数(AWMPFD)最大值均为阔叶混交树种组；景观斑块边缘密度(ED)最大值均为阔叶混交树种组；阔叶混交树种组的平均最小距离(ENN)减少。从2011年2017年研究区的主要优势树种组阔叶混交树种组得以保护,这与人为干扰的减少有关。     

基于遥感数据的大尺度区域水田空间格局及生态服务价值变化分析

受经济和气候驱动，长江经济带水田空间格局发生了显著变化，影响区域粮食安全与生态安全。本研究基于1990-2015年土地利用遥感监测数据，利用GIS的空间分析功能，探究长江经济带水田空间格局动态变化特征，采用当量因子法计算生态系统服务价值（ESV），分析了水田变化的综合影响。结果表明：1）1990-2015年长江经济带水田规模持续缩减，共减少了17390km²，减幅呈增长态势具有显著地域差异，长江中上游与下游的水田减幅相差约为9.56%。其中下游减幅较大，水田占区域比例随之降低，中上游恰好相反。2）由于经济建设及水产养殖的发展，水田主要转化为建设用地和水系，水田主要由水系、旱地和湿地等转化而来。长江三角洲城市群、长江中游及成渝城市群的水田变化最为剧烈，建设用地侵占水田扩张的现象分布广泛，水田转为水系主要在两湖平原局部地区。3）水田与其他生态系统的转化对ESV是正影响，水田转为水系对此贡献最大，其转化规模决定了不同时期ESV净增量的大小，水系转化为水田损失的价值最多，建设用地侵占水田次之。不同市域的水田变化情况不一致，因此ESV增减情况具有明显差异。4）生态系统服务中水文调节、水资源供给增强的同时，食物生产、气体调节受到严重损害，与水资源规模扩大和水田资源大量流失有直接关系。研究结果有助于揭示长江流域水田的时空变化过程及其对各项生态系统服务的影响，可为区域土地利用规划、农业政策与生态可持续发展提供理论支持。