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101.
高硫煤矿闭坑后成为埋藏在地表以下深部的产酸污染场,对相邻含水层和周边环境造成了潜在危害,且因采动效应影响和矿井空间分布复杂导致相邻含水层的污染过程与污染程度评价困难。以某闭坑矿区为研究对象,选取SO4 2−作为特征污染物,考虑多煤层采动裂隙对含水层结构的破坏影响,运用数值模拟技术对闭坑矿区酸性矿井水中SO4 2−污染迁移特征进行研究,并分析流体扩散系数对含水层污染物运移的影响。结果表明:SO4 2−在二叠系童子岩组砂岩含水层中水平迁移面积随时间增大而增大,增大速率逐渐减小,垂向渗透系数扩大10倍,空间变异性增强;闭坑5、10、15 a后,最大水平迁移距离分别为215、414、612 m,最大垂向迁移距离分别达到50、65、70 m;而扩散系数越大,产酸时间越长,SO4 2−迁移距离和污染范围将随之增大,相较于水平方向,垂向上SO4 2−浓度变化对扩散系数的敏感度更高。基于模拟结果,结合闭坑矿区实际条件,针对性提出了“源头减量−过程阻断−末端治理”的综合防控与治理方案。研究结果将为该闭坑煤矿酸性矿井水污染治理与防控提供理论基础,也为其他同类矿井提供科学借鉴。
相似文献102.
Cropland cover change in Northeast China during the past 300 years 总被引:15,自引:0,他引:15
Land use/cover change induced by human activities has emerged as a “global” phenomenon with Earth system consequences. Northeast
China is an area where the largest land cultivation activities by migrants have happened in China during the past 300 years.
In this paper, methods including documentary data calibration and multi-sourced data conversion model are used to reconstruct
historical cropland cover change in Northeast China during the past 300 years. It is concluded that human beings have remarkably
changed the natural landscape of the region by land cultivation in the past 300 years. Cropland area has increased almost
exponentially during the past 300 years, especially during the past 100 years when the ratio of cropland cover changed from
10% to 20%. Until the middle of the 19th century, the agricultural area was still mainly restricted in Liaoning Province.
From the late 19th century to the early 20th century, dramatic changes took place when the northern boundary of cultivation
had extended to the middle of Heilongjiang Province. During the 20th century, three agricultural regions with high ratio of
cropland cover were formed after the two phases of spatial expansion of cropland area in 1900s–1930s and 1950s–1980s. Since
1930s–1940s, the expansion of new cultivated area have invaded the forest lands especially in Jilin and Heilongjiang Provinces.
Supported by National Natural Science Foundation of China (Grant No. 40571165) and Innovation Foundation of Chinese Academy
of Sciences (Grant No. KZCX2-YW-315) 相似文献
103.
Analyses (n = 525) of chloride (Cl−), bromide (Br−), nitrate as nitrogen (NO3-N), sodium (Na+), calcium (Ca2+) and potassium (K+) in stream water, tile-drain water and groundwater were conducted in an urban-agricultural watershed (10% urban/impervious, 87% agriculture) to explore potential differences in the signature of Cl− originating from an urban source as compared with an agricultural source. Only during winter recharge events did measured Cl− concentrations exceed the 230 mg/L chronic threshold. At base flow, nearly all surface water and tile water samples had Cl− concentrations above the calculated background threshold of 18 mg/L. Mann–Whitney U tests revealed ratios of Cl− to Br− (p = .045), to NO3-N (p < .0001), to Ca2+ (p < .0001), and to Na+ (p < .0001) to be significantly different between urban and agricultural waters. While Cl− ratios indicate that road salt was the dominant source of Cl− in the watershed, potassium chloride fertilizer contributed as an important secondary source. Deicing in watersheds where urban land use is minimal had a profound impact on Cl− dynamics; however, agricultural practices contributed Cl− year-round, elevating stream base flow Cl− concentrations above the background level. 相似文献
104.
Joseph M. Delesantro Jonathan M. Duncan Diego Riveros-Iregui Joanna R. Blaszczak Emily S. Bernhardt Dean L. Urban Lawrence E. Band 《水文研究》2021,35(9):e14339
Current land-use classifications used to assess urbanization effects on stream water quality date back to the 1980s when limited information was available to characterize watershed attributes that mediate non-point source pollution. With high resolution remote sensing and widely used GIS tools, there has been a vast increase in the availability and precision of geospatial data of built environments. In this study, we leverage geospatial data to expand the characterization of developed landscapes and create a typology that allows us to better understand the impact of complex developed landscapes across the rural to urban gradient. We assess the ability of the developed landscape typology to reveal patterns in stream water chemistry previously undetected by traditional land-cover based classification. We examine the distribution of land-cover, infrastructure, topography and geology across 3876 National Hydrography Dataset Plus catchments in the Piedmont region of North Carolina, USA. From this dataset, we generate metrics to evaluate the abundance, density and position of landscape features relative to streams, catchment outlets and topographic wetness metrics. While impervious surfaces are a key distinguishing feature of the urban landscape, sanitary infrastructure, population density and geology are better predictors of baseflow stream water chemistry. Unsupervised clustering was used to generate a distinct developed landscape typology based on the expanded, high-resolution landscape feature information. Using stream chemistry data from 37 developed headwater catchments, we compared the baseflow water chemistry grouped by traditional land-cover based classes of urbanization (rural, low, medium and high density) to our composition and structure-based classification (a nine-class typology). The typology based on 22 metrics of developed landscape composition and structure explained over 50% of the variation in NO3−-N, TDN, DOC, Cl−, and Br− concentration, while the ISC-based classification only significantly explained 23% of the variation in TDN. These results demonstrate the importance of infrastructure, population and geology in defining developed landscapes and improving discrete classes for water management. 相似文献
105.
106.
《Chemie der Erde / Geochemistry》2015,75(1):65-72
This study was conducted on recent desert samples—including (1) soils, (2) plants, (3) the shell, and (4) organic matter from modern specimens of the land snail Eremina desertorum—which were collected at several altitudes (316–360 m above sea level) from a site in the New Cairo Petrified Forest. The soils and shellE. desertorum were analyzed for carbonate composition and isotopic composition (δ18O, δ13C). The plants and organic matterE. desertorum were analyzed for organic carbon content and δ13C. The soil carbonate, consisting of calcite plus minor dolomite, has δ18O values from −3.19 to −1.78‰ and δ13C values −1.79 to −0.27‰; covariance between the two values accords with arid climatic conditions. The local plants include C3 and C4 types, with the latter being dominant. Each type has distinctive bulk organic carbon δ13C values: −26.51 to −25.36‰ for C3-type, and −13.74 to −12.43‰ for C4-type plants.The carbonate of the shellE. desertorum is composed of aragonite plus minor calcite, with relatively homogenous isotopic compositions (δ18Omean = −0.28 ± 0.22‰; δ13Cmean = −4.46 ± 0.58‰). Most of the δ18O values (based on a model for oxygen isotope fractionation in an aragonite-water system) are consistent with evaporated water signatures. The organic matterE. desertorum varies only slightly in bulk organic carbon δ13C values (−21.78 ± 1.20‰) and these values suggest that the snail consumed more of C3-type than C4-type plants. The overall offset in δ13C values (−17.32‰) observed between shellE. desertorum carbonate and organic matterE. desertorum exceeds the value expected for vegetation input, and implies that 30% of carbon in the shellE. desertorum carbonate comes from the consumption of limestone material. 相似文献
107.
108.
Climatological distribution of lightning density observed by satellites in China and its circumjacent regions 总被引:13,自引:1,他引:13
MA Ming TAO Shanchang ZHU Baoyou & LU Weitao School of Earth Space Sciences University of Science Technology of China Hefei China 《中国科学D辑(英文版)》2005,48(2):219-229
The 0.5°×0.5°grid resolution distribution of lightning density in China and its circumjacent regions have been analyzed by using the satellite-borne OTD (Apr 1995-Mar 2000) and LIS (Dec 1997-Mar 2003) databases. It is shown that: (i) Firstly, the variability of the lightning density (LD) is particularly pronounced over the different subareas, 9 times greater over the south than the north side of Himalayas Mountains, 2.5 times greater over the eastern than the western area of China. While the maximum and minimum LD are respectively 31.4fl/km2/a (in Guangzhou region) and less than 0.2fl/km2/a (in the desert of western China). Secondly, the LD of China's continent regularly varies with latitude and distance off coast, which is consistent with annual mean precipitation in varying trend. In conclusion, the Qinghai-Tibet Plateau, the China's three-step staircase topography and the latitude are three important factors affecting macro-scale characteristics of the LD distribution, (ii) The regional differences 相似文献
109.
LIU Xuhua WANG Jinfeng LIU Mingliang & MENG Bin . Institute of Geographic Sciences Natural Resources Research Chinese Academy of Sciences Beijing China . Graduate School of the Chinese Academy of Sciences Beijing China . College of Arts Sciences of Beijing Union University Beijing China . School of Forestry Wildlife Sciences Auburn University Auburn Alabama AL USA 《中国科学D辑(英文版)》2005,48(12):2231-2240
Along with the increasing problems of rapid popu-lation increase, resources scarcity and environment deterioration, the interaction between human devel-opment and natural environment changes, especially the Land-Use/Land-Cover, LUCC issue is becoming a frontier and hot field[1], in which investigation on the mechanisms of land use change is one of the three core issues. Deficient natural resources, in particular the shortage of cropland resource in China, are the important constraints to Ch… 相似文献
110.
用SPSS13.0单因素方差分析和均值比较方法,对浙江省不同城市化地区的农户农地收入比重进行比较分析。认为城市化不同,农户农地收入比重不同,城市化程度高的地区农户农地利用经济收入比值的平均值低于城市化程度低的地区,但城市化程度高的地区农户农地收入比值标准差大于城市化低的地区,其中主要原因是城市化不同导致农户兼业时间不同。提出要创造条件促进资源集中型农户兼业化,使农户农地利用经济效率得到提高,缩小城乡收入差距。 相似文献