首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 15 毫秒
1.
The contradiction between the rapid development of aviation market and supply of airspace resources has increased the environmental damages of aviation carbon emission. The conversion and application of environmental damage assessment method of aviation carbon emission were summarized, and the characteristics of the assessment methods for air and ground transportation were compared. We found out the followings: The evaluation method has been transformed from static assessment to dynamic evaluation, and focused on four key problems, average and total carbon emissions, airspace resource utilization, LTO stage emission, and reduction practice; Airport terminal area as well as LTO are becoming the focus in the study of aviation carbon emission assessment method, while the former is the main area and the latter is the main stage of aviation carbon emission. The practice of emission reduction is mainly reflected in the optimization of emission reduction measures in economic field; Based on the situation and total assessment methods, environmental damage assessment and comparative advantage of aviation carbon emission and ground transportation carbon emission are reflected in the distance by using distance factor and energy consumption; Improving the smoothness of airspace resource traffic network, optimizing flight schedule structure and airspace resource allocation are more conducive to promoting aviation emission reduction.  相似文献   

2.
With the intensification of urbanization and global warming, the problems of urban thermal environment are increasingly prominent. On the basis of the remote sensing, geographic information system, geostatistics and multiscale spatial pattern, the spatial-temporal variation characteristics of land surface temperature in urban thermal environment were quantitatively analyzed. The results are as follows: Dramatic changes in land use/land cover had occurred from 1993 to 2016 in the study area. The net increase area of construction land was 1 231.04 km2, with a change rate of 295.33%. Cultivated land was occupied by construction land. The area of middle, sub-high and high temperature zones spread to the surrounding areas gradually with the Minjiang River. The area of sub-low and low temperature zones decreased markedly. From 1993 to 2016, the contribution of land surface temperature in different urban districts had the characteristics of uneven spatial and temporal distribution. Meanwhile, there was a positive contribution in the process of land surface temperature rise in Fuzhou while there was a negative contribution in Minqing and Yongtai. Forest/grassland, cultivated land, water body and wetland had a negative contribution during land surface temperature rise while construction land contributed positively. According to the multi-distance spatial cluster analysis (Ripley's K function), there was a certain scale in the aggregation and dispersion of land surface temperature, in which the aggregation range and degree of aggregation increased in the study area in 24 years.  相似文献   

3.
Groundwater, as a drinking water source for nearly one third of the world’s urban population, plays a strategic role in the development of urbanization. The object of this study is urban areas with the largest demand for water resources, the heaviest load of groundwater pollution and the most intense development of underground projects. This study sorted out the eco-hydrological problems such as the variation of the groundwater hydrological process, the groundwater pollution, and the urban heat island of groundwater in urban areas under the background of urbanization. Furthermore, the mechanism of changes in the quantity, quality and heat of groundwater was also systematically analyzed, and the intrinsic interaction among these three factors was revealed. The study showed that changes in land use and land cover caused by the urbanization are the main reasons for the variation of groundwater hydrological process. The pollution load of urbanization construction and domestic production waste has aggravated the deterioration of groundwater quality. The increase in vertical heat flux caused by urbanization gives rise to the warming of groundwater. By summarizing the eco-hydrological problems and causes of groundwater in urbanized areas, several suggestions were proposed: Establishing the evaluation method and system of urban groundwater resources; Speeding up the technological breakthroughs of groundwater pollution control; Improving the regional control strategies for groundwater pollution; Optimizing the allocation of groundwater resources. This study will provide the theoretical basis and technical support for ensuring urban water safety, building ecological civilized cities and further promoting the sustainable development of economy and society.  相似文献   

4.
Rice paddies are an important anthropogenic source of methane (CH4) to the atmosphere, which aggravate the global warming greatly. CH4 fluxes from a rice paddy in Central China were continuously measured with the eddy covariance method in 2018. The characteristics, dynamics and drivers of the observed CH4 fluxes from this paddy field were subsequently analyzed. The results indicated that a distinct seasonal variation of daily CH4 fluxes was found over the whole observed period. Daily CH4 fluxes were the highest in the vegetative period, then decreased gradually, and became the lowest in the fallow period; observed CH4 fluxes had a clear single-peak diurnal pattern during the vegetative and reproductive periods, and reached daily peaks at about 14:00-16:00. However, no obvious diurnal variation in CH4 fluxes was observed during the fallow period; air temperature was the most important drivers that controlled the seasonal variation of CH4 fluxes from this paddy field, and Vapor Pressure Deficit (VPD) was also found related to the CH4 emissions; the largest daily CH4 flux was 0.69 μmol/(m2·s), occurred in the late of vegetative period, and the total amount of CH4 emissions over the whole observed period was about 28 g C/m2.  相似文献   

5.
Based on the particle size test results of 36 surface sediment samples from the Cibi Lake, the spatial distribution characteristics and rules of components were discussed by the combination of natural geographical factors with statistical analysis methods in the basin, which provides scientific evidence and basic data for the study of paleoclimate environment in this region. The results show that: The samples mainly include clay, silty and sand, among which silty is the main type in the study area and has the widest distribution due to the disturbance caused by groundwater recharge without obvious spatial variation law; The clay distribution is somewhat smaller, and its locality affected by the slope alluvial fan is in the northwest and near the center of the lake, where the sedimentary environment is stable and is the best selected location for the borehole core so that the reconstruction of the paleoclimate environment can be carried out; Sand is mainly distributed in the southwest corner and near the north shore of the lake, which is influenced by the rivers entering the lake and human activities, and these two locations have a great influence on the source of surface sediment. Therefore, the management of the north and southwest regions should be strengthened to prevent a large number of pollutants from entering the lake; The grain size frequency curve shows that the sediments include suspended and saltant components. Besides the formation by their own biochemistry, other materials come from the aeolian sediments in the basin, and the coarse particles transported over a long distance have a great impact on the grain size components. Section CB-1 indicates that transport process and distribution are significantly affected by the southwest monsoon and more attention should be paid to the prevention and control of pollution at the river inlet and upwind area.  相似文献   

6.
The study on vegetation cover changes based on remote sensing data sources is an important component and frequent topic of earth surface process research. In order to review and summarize the remote sensing data sources and the spatio-temporal pattern of the study areas for vegetation cover changes in China from the perspective of bibliometrics and GIS spatial presentation, the information of remote sensing data sources and study areas were extracted from 1 021 papers on vegetation. Then the composition of remote sensing data sources and their temporal changes in heat which is termed as study frequency, the spatio-temporal scale characteristics of remote sensing data sources and study areas, and the distributions and change characteristics of hot study regions were analyzed. The results show that the number of papers is increasing gradually, and the frequency of each remote sensing data source is basically consistent with its available timing; the average period length of the remote sensing data used is gradually elongated, and the spatial resolution of remote sensing data is positively correlated with the size of study areas stably; the hot study regions are concentrated in the Loess Plateau area, and the core of the northern arid and semi-arid areas. These results can provide a basic reference for understanding the spatio-temporal pattern and the change trend on the utilization of remote sensing data sources and hot regions for vegetation change studies.  相似文献   

7.
Simulating the temporal-spatial distribution of areas suitable for crops is an important part of analyzing the effects of climate change on crop growth, reducing the vulnerability of crop growth, and assessing the adaptability of crop growth to climate change. This study selected climate factors that affect the growth of wheat, maize and rice, and it combined surface soil and ground elevation factors as environment variables, as well as data from agricultural observation stations as species variables. The MaxEnt ecological model was used to identify suitable areas for these three crops during the period of 1953-2012. The areas suitable for the three crops were analyzed to determine the temporal-spatial distribution of major food crops and to estimate the difference in crop growth adaptability under climate change. The results showed the following: The response to climate change of the areas suitable for food crops could be ranked from strongest to weakest as follows: wheat, rice, and maize. On the same space-time scale, for the growth of wheat and rice, the southern agricultural regions, mountainous areas and plateaus were relatively unsuitable for a wider variety of crops than the northern agricultural regions, plains and basins. The adaptability of wheat increased in the major agricultural regions slightly. The adaptability of maize increased in the northern agricultural regions and decreased in the southern agricultural regions, respectively. The adaptability of rice was stable in the southern agricultural regions, and it decreased in the Huang-Huai-Hai region and increased in the northeastern region. Over 60 years, the ability of the major food crops to adapt to climate change increased in the northeast region, Gansu-Xinjiang region, Southwest region and Loess Plateau region, but the adaptability of major food crops decreased in the Huang-Huai-Hai region and the Mid-and-Lower Reaches of the Yangtze River. The suitable areas of maize and rice were significantly correlated with planting areas and yields, respectively, which provided feasibility for simulating the distribution of suitable areas on maize and rice in different climate scenarios in the future. The suitable area of wheat is not significantly related to the planting area and yield. In the future, we will take more factors to model the suitable area of wheat accurately.  相似文献   

8.
The Qinghai Tibet Plateau (QTP) is an important ecological security barrier region and strategic resource reserve base in China. It is of great significance to explore the construction and impact of its transportation facilities. Through combing the relevant research, we found that: With the construction of macro regional policies and major transportation facilities, the relevant research has been growing rapidly since 2000, and the contribution of Chinese Academy of Sciences, transportation universities and research institutions is outstanding; The key research of QTP's transportation facilities construction includes the constraints and countermeasures of permafrost melting, sandstorm, erosion and geological disasters, the development process of modern comprehensive transportation system and its spatial characteristics, and the evolution of multi-scale regional traffic connection and accessibility; The regional impact assessment of traffic facilities mainly focuses on ecological environment and social economy. The former results are mainly negative effects such as disturbing ecosystem, cutting landscape pattern, destroying vegetation cover and disturbing the normal living habits of wild animals, while the latter ones are mainly positive effects like promoting macro regional development, changing the spatial structure of regional development, and driving the development of tourism and other related industries. In general, the positive and negative effects of multi-dimensional and multi-scale show the characteristics of differentiation and multiple feedbacks. With the implementation of the Second Comprehensive Scientific Investigation on the QTP and the construction of Third Pole National Park Group, Sichuan-Tibet Railway and Qinghai-Tibet Expressway, we should further focus on the breakthroughs in key relevant technologies, the balance of transportation system with national strategies and regional functions, the combination of travel perception and comprehensive traffic accessibility, combing the comprehensive impact mechanism from the perspective of coupling and the construction of analysis framework that is in line with regional reality, etc.  相似文献   

9.
For decades of exploration, geologists have made great achievements in the exploration of lacustrine carbonate rocks. By dissecting four typical cases of lacustrine carbonate rocks, such as Lucaogou Formation of Permian in Junggar Basin, Da'anzhai Section of Jurassic in Sichuan Basin, Cretaceous in Yin'e Basin and Oligocene in Qaidam Basin, the reservoir characteristics, hydrocarbon generating capacity and reservoir forming model of source rocks were analyzed. The results show that: Lacustrine carbonate reservoirs are generally dense, with nano-micron reservoir space as the main reservoir space, including dolomite intergranular pore, organism cavity and accumulation pore, micro-fracture system and its corrosion expansion pore. Saline environment is beneficial to dolomitization and can improve the reservoir capacity of lacustrine carbonate rocks, but most of the permeability is less than 0.1 mD. Lacustrine carbonate rocks have not only reservoir capacity, but also can be used as source rocks. The abundance of organic matter is not high and the maturity is generally low. However, dispersed soluble organic matter in source rocks can generate and expel hydrocarbons in large quantities at low maturity stage, which has high liquid hydrocarbon yield. Oil and gas reservoirs are characterized by "high initial production, large reduction of production and long-term low and stable production", and are typical "fracture-pore" reservoirs. Fracture networks provide migration pathways in the process of primary migration and accumulation of oil and gas in geological history and oil and gas exploitation nowadays. Oil and gas reservoirs are "continuous" unconventional reservoirs, which often form regional oil and gas field groups together with conventional reservoirs in adjacent areas. The research results lay a theoretical foundation for re-evaluating the exploration potential of lacustrine carbonate rocks.  相似文献   

10.
The interactions among surface water, groundwater and seawater are closely related in the coastal area with complex hydrological conditions. A series of impacts from human activities and climate change are also more significant in this region. In order to understand the key knowledge and research status of surface water and groundwater interaction in coastal area, it is a useful method to analyze literatures in this research scope in the core database of Web of Science by using CiteSpace. The research achievements in this field were systematically sorted and potential research hotspots were explored, which may provide references for subsequent researches. The results show the following. The number of highly cited articles and highly burst articles in this research field has increased significantly since 2010. At present, this field is still in the development stage and has a broad research prospect. The United States, Australia, China and Germany have done plenty of researches on this issue and achieved a lot. At present, the number of research achievements supported by National Natural Science Foundation of China is in the lead over the world. Seawater intrusion, submarine groundwater discharge, the relationship between tide and hydrological conditions are the main research direction in this field. Hydrochemistry and isotopic analysis, and numerical simulation are the most important research methods in this field. The potential development directions and breakthroughs in this field include submarine groundwater discharge, the evolution of coastal mangrove wetlands, the migration and transformation of nutrients, the influences of different hydrological factors on coastal areas, and the impact of climate change on coastal areas. Overall, the future development of surface water and groundwater research in coastal areas is inseparable from the cross-integration of various disciplines, mutual verification of multiple methods and the introduction of new technical means.  相似文献   

11.
Establishing an effective hydrological model is important for guiding the design of small-scale drainage systems. The simulation principle and the sensitivity of key parameters of DRAINMOD model were summarized from four aspects:Hydrological characteristics, nitrogen transport, salt transport and model cooperation. The research application progresses of DRAINMOD model and its coupled model at home and abroad were systematically reviewed, and the limitations and development trends of the model were discussed. It is pointed out that DRAINMOD model has good simulation performance in the fields of agricultural drainage, nitrogen removal and stain reduction. In the simulation of cold area or urban stormwater regulation, domestic research needs to reference from foreign research results. The research suggests that the key research directions of DRAINMOD model could be summarized as the following aspects:Simulating the migration of phosphorus, organic micro-pollutants and heavy metal elements and their impacts on soil and crops; Mechanism research on the freezing-thawing of snow and application in cold regions; Application in the construction of urban stormwater regulation facilities.  相似文献   

12.
Alluvial fans can preserve historical records of sediment transport to middle and lower river systems or piedmont basins, which are considered to be sensitive recorders of climate change and tectonic activity. In this paper, the morphological characteristics, control factors and future development trend of alluvial fan are summarized and described. The main understanding is as follows: According to the gravity flow and traction flow process, fan can be divided into debris flow alluvial fan and fluvial fan. The former is formed under the action of debris gravity flow deposits, which is related to the occasional flood and burst flow in a short time. The latter is braided tributaries depositions which are gradually shallower and spread radially in the direction of fan toe under the traction water transport. The erodibility of underlying bedrock can affect the scale of downstream alluvial fan, which depends on the sediment production and store factors in the catchment. The easily eroded bedrock may produce more sediment, making the alluvial fan area larger. In the contrast, the erodibility of rocks in the source area can also affect the slope and hydrological characteristics of the valley so that more sediment is deposited in the upstream basin and the alluvial fan formed in the downstream is smaller. Tectonic activity is the pre-condition for the development of alluvial fans, which provides a space for alluvial fans depositions. Faulting in the piedmont can change the position and morphology of the ancient alluvial fan, and also cause deformation or distortion of the thick sedimentary sequence to record the regional tectonic activity. The quaternary alluvial fan sequence corresponds well to the climate change during the glacial-interglacial period. However, the influence of the flood events caused by extreme meteorological events on alluvial fan deposition should be focused on. The application of a series of new techniques and methods will help to carry out deep research on alluvial fan in the future, such as high-resolution observation technique, physical simulation experiment, and precise dating.  相似文献   

13.
The distribution of frozen soil in our country is very broad, and the area of permafrost alone accounts for 22. 4% of the total land area. As a special kind of soil, frozen soil has many properties that thawing soil does not have due to the influence of ice cement in the soil. Among the many properties of frozen soil, the deformation and strength of frozen soil are the basic problems affecting engineering construction in frozen soil areas. The spherical template indenter test is widely used in the test of the mechanical properties of frozen soil because of its simple test process and relatively accurate test results. Compared with the conventional triaxial test or direct shear test, the test process of the spherical template indenter test is simple and easy to implement, the test period is short, and the sample preparation requirements are low. The advantage of effective cohesion is more significant. Therefore, based on the spherical template indenter test of the frozen soil, this paper estimates the strength and mechanical index of the soil through the indentation depth of the spherical template indenter test, and establishes the relationship between the force of the sample and the indentation depth of the indenter test. The specific test method is as follows:take the water-saturated frozen sandy soil made of different particle size groups(the moisture content of the sample is affected by the particle size in the saturated state)as the research object, study the variation law of the depth of the frozen soil sample pressed into the soil by the spherical indenter with time under the conditions of different fixed loads. By comparing and referring to the frozen sands of each particle size group, the long-term equivalent cohesion of the frozen sands of different particle size groups is summarized. The change law of force(long-term shear strength)with time, and the research method of elastic mechanics to solve space problems, summed up the mutual conversion between the depth St of spherical template indenters pressed into frozen sand samples under different fixed load test conditions relation. The research results show that the long-term shear strength of frozen sand based on the spherical mold test is positively correlated with its particle size. At the same time, since the ice content of frozen soil samples is proportional to its particle size, the long-term shear strength of frozen sand is also proportional to the test. The ice content of the sample increases year-on-year;the long-term shear strength of the frozen sand is related to the maximum contact pressure on the contact surface between the frozen soil and the indenter during the test, which can be expressed as Ct = γq0. The size of the relationship coefficient γ is inversely proportional to the diameter of the spherical indenter. In this paper, the spherical indenter is selected as 22 mm, and γ=3. 82×10-3. By establishing the relationship between the maximum contact pressure q0 and the long-term shear strength Ct When the maximum contact pressure q0 is the same under different fixed loads, the long-term shear strength Ct is also the same. According to this, the depth curve and the freezing depth of the frozen sand pressed into the soil by the spherical indenter over time under different fixed loads can be converted. Long-term shear strength curve of frozen sandy soil with time. It has been verified by experiments that the conversion curve of the depth of the indenter pressed into the soil with time under a fixed load of 7. 0 kg is highly consistent with the measured curve of the depth of the indenter pressed into the soil with time under a fixed load of 5. 1 kg and 7. 0 kg. © 2022 Nanjing Forestry University. All rights reserved.  相似文献   

14.
The Glycerol Dialkyl Glycerol Tetraethers (GDGTs) occur ubiquitously in a wide range of environments, such as loess, peat, lake, soil, and ocean, which vary compositionally in response to environmental changes, and provide a series of biomarker proxies for paleoenvironmental reconstruction. This paper introduced the structures and biological sources of GDGTs, and reviewed the recent progresses of the application of the GDGTs proxies in the paleoenvironmental reconstruction of loess deposits. The main progresses include: The GDGTs proxies have been widely used in reconstructing the climate changes in loess deposits, and have established the temperature changes of last 800 ka for the Chinese Loess Plateau; Temperature variations in Chinese Loess Plateau displayed significant correlation with the Northern Hemisphere insolation, which may be also regulated by the surface vegetation conditions; and In the Chinese Loess Plateau, the increase in monsoon precipitation during the last deglaciation significantly lagged behind the rise of temperature. However, problems still exist in the current studies. For instance, the GDGTs-based temperature is likely overestimated, probably reflecting the temperature of warm season, and relationships between GDGT indices and climate factors are still unclear. In the future, the development of new proxies and more accurate regional calibrations based on the separation of 6- methyl GDGTs are expected to provide more reliable paleoenvironmental information, and will provide essential evidence for the evolution of hydrothermal pattern and mechanisms behind climate changes in different regions.  相似文献   

15.
As the turning point of the Yellow River flowing from the Tibetan Plateau to the Loess Plateau, the valley evolution of Lanzhou Basin is of great significance to the study of the evolution of the Yellow River system in different geomorphic units. The evolution of the Yellow River Valley in Lanzhou has been studied for nearly 100 years. In the process of research, important research results and understandings have been obtained as follows: The denudation surface develops above the Yellow River Valley in Lanzhou Basin, and the broad and continuous 9-level terrace develops in the valley. The age of the denudation surface and 9-level Yellow River terrace was systematically determined by using a variety of dating techniques. The development pattern of the strath terraces of the Yellow River in Lanzhou was put forward. Under the background of long-term ground uplift, climate change controls the age of terrace formation, and the rate of uplift affects the number of terrace. The age of the highest terrace of the Yellow River in the basins from Lanzhou to the upper reaches of the Yellow River is gradually younger. It is revealed that the formation of the present pattern in the upper reach of the Yellow River is the result of the headward erosion from Lanzhou Basin and the drainage intergration of the internal flow basin. At the same time, the chronology of terrace sequence still needs to be deepened, the characteristics of regional tectonic uplift and deformation are lack of direct evidence, the development pattern of terrace needs to be verified by model simulation, the geomorphic response of drainage change is not clear, and the river process recorded by the deposition of terrace flood plain is lack of attention. All those issues will be the focus of future research.  相似文献   

16.
Cherts contain important information of paleogeography, paleostructure and paleo-ocean, which is the important means of studying petrotectonics. With regard to the major disputes on the sedimentary environments, origin and source of Gufeng Formation bedded cherts in the northern margin of middle-lower Yangtze area, demonstrations from both forward and reverse aspects from the perspective of the sedimentary-tectonic evolution were given. By summarizing previous views on the genesis of bedded cherts in Gufeng Formation, and extensively collecting published original geochemical data, in the forward demonstrations we created the database of the cherts about rare earth elements to systematically identify the sedimentary environments, origin and source of cherts. By sorting out the time and cause of the main geological events in the middle Permian in south China, in the reverse demonstrations we established the sequence of tectonic evolution to verify or explain the current series of disputes. The results show that: Except some areas, such as Guichi-Tangtian, Tongling-Huashupo and Chaohu-Pingdingshan in Anhui province, which were affected by volcanic activities and faults, the bedded cherts of Gufeng Formation in the northern margin of middle-lower Yangtze area are mainly of non-hydrothermal origin or biological origin, and deposited in the passive continental margin deep water environments. Paleocontinental uplift in cathaysian and sea level eustacy controlled the input of some terrestrial materials in the the Gufeng Formation bedded cherts in the study area, but the contribution of terrestrial materials to cherts is not obvious. The study of cherts in Gufeng Formation is of great significance to the eruption time and dynamic mechanism of Emeishan basalts.  相似文献   

17.
The notion of Resilience of Social-Ecological Systems (ReSES) in balancing and sustaining development are increasingly breeding more multidisciplinary attentions from world scientists and government managers. However, with the tremendous growing in theoretical system, certain problems hinder the integration of theory and practice, such as the low degree of research recognition, lacking of unified paradigm, unevenly development of research topics, etc. Thus, it is an urgent need to sort out the construction, source and development in theory, and its gaps with practices. To identify the hotspot in current research, including the fundamental theories and methods, current focus and future trends, a bibliometric analysis integrating Citespace and TDA tools were made. Using searching queries on “system resilience”, 10 315 articles in Web of Science database were retrieved. Then, a series of contents were examined on these publications, including: topics division on co-occurrence network of keywords; journal and co-citation analysis of highly cited papers; trends by keyword burst analysis; changing of high-frequency categories and keywords. Several findings were achieved through scientometric analysis. Firstly, research on system resilience were summarized into five basic theoretical issues, namely, research objects, changes incentives, spatial and temporal scale, and adaptive measures. Secondly, by analyzing the knowledge atlas, it is found that the theory has developed for nearly 45 years since 1973. In the past 20 years, ecosystem resilience driven by climate changes has been one of the earliest and consistent research topics, and formed a well-developed theoretical framework. Over the past ten years, research on the system resilience on community and urban scale has rapidly become a hot topic. In the past five years, adaptation strategies such as social learning and knowledge dissemination have attracted increasing attentions. Overall, improving system simulation and scenario based adaptive management analysis can build the bridge of theoretical research and adaptive management practice.  相似文献   

18.
Daily routine observation data from 274 meteorological stations in the Qinghai-Tibetan Plateau and its surrounding areas from 1970 to 2017 were utilized to examine the spatial patterns and abrupt changes of potential evapotranspiration with the formula of FAO Penman-Monteith, in consideration of China’s eco-geographical divisions. The results showed that annual and seasonal average potential evapotranspiration, except for summer and winter, displayed a distinct spatial pattern in the Qinghai-Tibetan Plateau and its surrounding areas, with higher values in the north and south but lower values in the middle; the time when monthly potential evapotranspiration reached its maximum or minimum showed clearly zonal differences, namely earlier in the south and later in the north. The prevailing mean and trend abrupt changes of potential evapotranspiration were observed in the study area, while there were large differences in the abrupt change time in different regions and seasons. Specifically, the mean abrupt change was dominated by positive mutation, with generally the earliest abrupt change time occurring in spring and the latest appearing in winter; the trend abrupt change pattern was mainly described as the process shifting from a downward trend to an upward trend, the trend change points in year, spring, autumn and winter were postponed gradually from the northeast to the southwest with a delay of about 20, 10, 20 and 5 years, respectively. Comparatively, the abrupt change time of potential evapotranspiration trend in the whole plateau was later than that in the whole buffer zone, with a respective lag of 5, 1, 12, 5 and 4 years. Corresponding to the periodic change of potential evapotranspiration, significant evaporation paradox only scattered through the study area during the period before the trend change point (2007), but it was absent afterwards and would not appear in the future. The above findings will provide a scientific basis for further understanding the climate change and eco-hydrological process of the Qinghai-Tibetan Plateau and its surrounding areas in global warming.  相似文献   

19.
于璐  郑天元  郑西来 《现代地质》2022,36(2):563-573
地下水硝酸盐污染已成为世界范围内最严重的环境地质问题之一。全面并准确识别硝酸盐污染源,对地下水的有效管理及污染防治具有重要的指导意义。从地下水硝酸盐来源、同位素检测方法、污染源同位素特征、定量解析模型构建、硝酸盐主要转化过程及同位素分馏效应等方面进行总结,比较不同解析方法在硝酸盐溯源中的应用与发展,建议采用多学科、多方法相结合的方式,提高对硝酸盐污染源的全面理解。同位素富集系数是定量解析硝酸盐污染源的重要参数,在源解析过程中探讨硝酸盐转化及同位素分馏机制,能够更好地诠释地下水硝酸盐来源和迁移转化过程,提高源解析的准确性,为地下水硝酸盐污染的准确溯源与有效防治提供参考。  相似文献   

20.
梁凯旋  刘菲  张莉 《地学前缘》2022,29(3):207-216
高氯酸盐( ClO 4 -)是一种小分子量、有毒的无机络阴离子,普遍存在于环境中。由于其分子大小与碘离子相似,会干扰人体甲状腺的正常功能,因此其环境污染问题引起了广泛的关注。本文选取污染场地的天然河沙为试验材料,主要通过柱实验对地下水中 ClO 4 -自然衰减过程进行研究,考察了铁氧化物、 NO 3 - ClO 4 -自然衰减过程产生的影响。结果表明,高氯酸盐自然衰减过程主要由微生物驱动,天然河沙可去除2 mg/L的 ClO 4 -,但其过程缓慢且还原量有限,长期去除率不超过10%,其限制因素为缺乏电子供体;铁氧化物可以促进 ClO 4 -自然衰减,但当溶解性铁的浓度低于5.5 mg/L时,衰减过程开始受到影响;地下水中的 NO 3 -会抑制 ClO 4 -的降解,当 NO 3 -低至10 mg/L或以下时, ClO 4 -才开始明显降解。  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号