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51.
绿洲演化与自然和人为因素的关系初探——以克里雅河下游地区为例 总被引:13,自引:0,他引:13
以位于塔里木盆地的克里雅河下游地区绿洲为例 ,论述了自然环境要素演变及人类活动对绿洲发育的重要作用。克里雅河下游地区的现代绿洲包括沿河岸分布的带状绿色走廊和河流终端干三角洲上的扇形牧业绿洲。依据对河流沉积物及古河道分析得出的结论是 ,在末次冰期晚期时 ,由于来自昆仑山的大量消融水的出现 ,克里雅河的绿色走廊横穿塔克拉玛干沙漠。类似的情况在距今约2 0 0 0年和小冰期时都出现过。这种大的变化是自然环境演变的结果。但是 ,近百年来特别是近 5 0年克里雅河下游牧业绿洲的严重退化是中游地区集中发展农业绿洲而增加引水量及下游地区过度砍伐所造成的。 相似文献
52.
53.
红壤退化中的土壤质量评价指标及评价方法 总被引:97,自引:4,他引:93
土壤质量评价与监测是评价土壤退化的重要工作,也是重新设计持续性的土壤管理系统的基础。目前缺乏统一的评价指标以及将各项土壤性质与土壤管理措施结合起来的评价方法。本文首先提出了选择红壤质量评价指标的原则,并从化学、物理学和生物学三个方面初步探讨了评价红壤质量动态变化可资采用的指标体系,综述了国内在南方丘陵区红壤质量演化的研究中应用的指标;最后从土地评价方法中选择了可用于红壤质量评价的方法,并简要综述了国际上最新的土壤质量评价方法。 相似文献
54.
Hydrocarbon degraders from tropical marine environments 总被引:1,自引:0,他引:1
Analysis of 20 samples of marine mud and water around Mumbai resulted in the isolation of 17 bacteria and yeasts all of which were able to degrade more than 10% of the supplied crude oil. The yeasts strains were important degraders of the aliphatic fraction of crude. All the isolated yeasts belonged to the genus Candida. Using biochemical tests these were identified as Candida parapsilosis, C. albicans, C. guilliermondii, Yarrowia lipolytica, C. tropicalis and C. intermedia. Y. lipolytica was the best degrader utilizing 78% of the aliphatic fraction of Bombay High crude oil. None of these isolates degraded the aromatic or ashphaltene fractions. All the isolates required aeration, nitrogen and phosphate supplementation for optimal degradation. Four out of the six yeasts are human pathogens. 相似文献
55.
Relationship between structures of substituted indolic compounds and their degradation by marine anaerobic microorganisms 总被引:1,自引:0,他引:1
Degradation of selected indolic compounds including indole, 1-methylindole, 2-methylindole, and 3-methylindole was assessed under methanogenic and sulfate-reducing conditions using the serum-bottle anaerobic technique and marine sediment from Victoria Harbour, Hong Kong as an inoculum. Our results showed that indole degradation was achieved in 28 days by a methanogenic consortium and 35 days by a sulfate-reducing consortium. During degradation under both conditions, two intermediates were isolated, purified and identified as oxindole and isatin (indole-2,3-dione) suggesting that both methanogenic and sulfate-reducing bacteria use an identical degradation pathway. Degradation processes followed two steps of oxidation accomplished by hydroxylation and then dehydrogenation at 2- and then 3-position sequentially prior to the cleavage of the pyrrole ring between 2- and 3-positions. However, none of 1-methylindole or 2-methylindole was degraded under any conditions. 3-Methylindole (3-methyl-1H-indole, skatole) was transformed under methanogenic conditions and mineralized only under sulfate-reducing conditions. It is clear that methyl substitution on 1- or 2-position inhibits the initial attack by hydroxylation enzymes making them more persistent in the environment and posing longer toxic impact. 相似文献
56.
Permafrost on the Qinghai-Tibet Plateau (QTP) is widespread, thin, and thermally unstable. Under a warming climate during the past few decades, it has been degrading extensively with generally rising ground temperatures, the deepening of the maximum summer thaw, and with lessening of the winter frost penetration. The permafrost has degraded downward, upward and laterally. Permafrost has thinned or, in some areas, has totally disappeared. The modes of permafrost degradation have great significance in geocryology, in cold regions engineering and in cold regions environmental management. Permafrost in the interior of the QTP is well represented along the Qing-hai-Tibet Highway (QTH), which crosses the Plateau through north to south and traverses 560 km of permafrost-impacted ground. Horizontally, the degradation of permafrost occurs more visibly in the sporadic permafrost zone in the vicinity of the lower limit of permafrost (LLP), along the margins of taliks, and around permafrost islands. Downward degradation develops when the maximum depth of seasonal thaw exceeds the maximum depth of seasonal frost, and it generally results in the formation of a layered talik disconnecting the permafrost from the seasonal frost layer. The downward degrada- tion is divided into four stages: 1) initial degradation, 2) accelerated degradation, 3) layered talik and 4) finally the conversion of permafrost to seasonally frozen ground (SFG). The upward degradation occurs when the geothermal gradient in permafrost drops to less than the geothermal gradients in the underlying thawed soil layers. Three types of permafrost temperature curves (stable, degrading, and phase-changing transitory permafrost) illustrate these modes. Although strong differentiations in local conditions and permafrost types exist, the various combinations of the three degradation modes will ultimately transform permafrost into SFG. Along the QTH, the downward degradation has been proceeding at annual rates of 6 to 25 cm, upward degradation at 12 to 30 cm, and lateral degradation in the sporadic permafrost zone at 62 to 94 cm during the last quarter century. These rates exceed the 4 cm per year for the past 20 years reported for the discontinuous permafrost zone in subarctic Alaska, the 3 to 7 cm per year reported in Mongolia, and that of the thaw-stable permafrost in subarctic Yakutia and Arctic Alaska. 相似文献
57.
王万春 《矿物岩石地球化学通报》2007,26(3):269-275
微生物降解使有机化合物的稳定碳、氢同位素发生不同程度分馏的研究在有机污染物来源和微生物环境修复等领域取得了长足进展,并对原油和天然气微生物降解研究有借鉴意义。微生物作用下的同位素分馏为动力同位素分馏,导致重同位素在残余物中富集。影响微生物降解有机物同位素分馏的主要因素有微生物的降解代谢途径、辅酶作用、降解类型与程度、同位素质量差异和有机物碳数等。不同的微生物代谢途径代表不同的生物化学反应,造成了同位素分馏的显著差异;辅酶对反应的催化作用使微生物作用造成的同位素分馏更加复杂。低碳数正构烷烃遭受微生物降解程度越高,碳、氢同位素的分馏也越大,同位素变重与降解程度之间有明显的相关性。但对于复杂化合物,由于降解的多级反应,同位素分馏与降解程度间的相关性并不明显。在同样降解程度下,氢同位素分馏大于碳同位素分馏,低碳数正构烷烃的同位素分馏大于高碳数正构烷烃的同位素分馏。 相似文献
58.
The development and utilization of water and land resources in the Shiyang River basin are the highest among the inland rivers
in northwestern China. Using GIS and the landscape structure analysis program FRAGSTATS, landscape metrics of a study area
in the lake-district in Minqin Oasis in the lower reaches of Shiyang River basin were calculated and analyzed based on TM
images from 1987 to 2001 at class level and landscape level, respectively. Transformation matrix of the landscape mosaics
was also examined. The driving forces of landscape changes were analyzed, including the dynamics of runoff and groundwater
resources and their exploitation, and influences of policies and market economy. The results showed that: (1) Patch number
of farmland and desert decreased, but their mean patch area increased, indicating that reclamation and desertification was
very serious in the study area. Contagion index for oasis increased and edge density and landscape diversity were reduced.
(2) Farmland and desert areas have enlarged by 1,520.46 and 4,941.27 hm2, respectively. This increase was at the cost of woodland and grassland, which shrank by 1,520.46 and 4,941.27 hm2, respectively. (3) The net utilization of surface water decreased by 50% in the last 10 years, and dropped to 22.3 × 106 m3 in the later 1990s. Exploitation of groundwater increased remarkably, up to 80 × 106 m3 per year in the last 5 years. (4) The capability of the economic structure to withstand pressures of the market economy has
depressed distinctly because of the simplified planting pattern, which is dominated by salinity-enduring cash crops, such
as cotton. Based on the above analysis, strategies of ecological reconstruction in the lake-district were suggested. 相似文献
59.
王克林 《中国地理科学(英文版)》1998,(3)
I.INTRODUCTIONItisgeneralyacceptedthatthedegradationofrenewableresourcesandfragileenvironmentsindevelopingcountriesisbecomin... 相似文献
60.
黑河下游额济纳绿洲环境退化及综合治理* 总被引:64,自引:13,他引:51
黑河下游的额济纳绿洲是内蒙西部阿拉善高原的主要天然绿洲。近半个世纪特别是近10年来,由于不合理人类活动和自然因素的双重作用,黑河下泄水量不断减少,生态环境恶化,严重影响到本地区乃至周围广大地区的持续发展。通过分析生态环境恶化的现状和原因,提出了生态环境的治理必须以水为中心,加快中游地区节水农业的发展步伐,保证下游一定量的供水,并严格控制不合理的人为活动,力争在10~15年内实现生态环境的良性循环。 相似文献