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961.
US Federal law mandates that mined land be returned by mine operators to a condition capable of supporting its pre-mining use or a higher use. Previously forested lands have commonly been reclaimed to hayland/pasture or wildlife habitat, and most of these lands have been abandoned from management and rendered non-productive. This situation has left landowners in the position of converting these reclaimed mined lands to forests at a later date, if they choose to make them economically productive. Such land-use conversion, however, comes with a substantial up-front cost to the landowner, which makes the financial viability of such a conversion questionable. We examine the financial viability of reforestation of these previously reclaimed mine lands by calculating land expectation value (LEV) under a range of conditions that include forest type, site quality, and reforestation intensity. We find that conversion to white pine is viable on higher quality sites under low to moderate interest rates with low or high timber prices, but conversion to mixed hardwoods is only profitable under the high price scenario with low interest rates, and only on higher quality sites. We also consider the implications of a shift in reforestation burden from the landowner to the mine operator, and results suggest that including costs of reforestation as part of the mining operation creates a financially viable forest enterprise for landowners under all scenarios for both white pine and mixed hardwoods. Two forms of carbon payments that could encourage reforestation of previously reclaimed mined lands also are examined: an annual payment based upon the total accumulated carbon found on-site in a given year, and an annual payment based on only the increment of carbon storage each year. Our carbon payment results indicate that annual values of up to $5.17 per ton of carbon stored in hardwoods and $9.39 per ton of carbon stored in pines would be required to make reforestation profitable under the poorest conditions (high interest rates, low prices, and poor quality site) when the payment is based on accumulated on-site carbon, although lower values are required under more favorable scenarios. Payments that are based upon the annual increment of carbon must fall in the range of $8.66–$71.88 per ton of carbon stored in hardwoods and $0–$83.29 per ton of carbon stored in pines to make reforestation financially viable. 相似文献
962.
963.
964.
The floatability of seven plastics (POM, PVC, PET, PMMA, PC, PS and ABS) in the presence of methyl cellulose (MC) and separation of plastics mixtures were investigated in this paper. It was found that the seven plastics can be separated into three groups by using the wetting agent MC. Group one includes POM and PVC. They are depressed at very low MC concentrations. Group two, including PET, PMMA and PC, has an intermediate floatability. Group three (ABS and PS) has a high floatability. They are almost not depressed within the given MC concentration range. In order to understand the mechanism of selective flotation of plastics and the chemical conditioning process, surface chemical factors, such as wettability of plastics and surface tension of flotation medium, and gravity factors, such as particle density and shape, were studied. It was found that the depressing effect of MC on plastics is ascribed mainly to its adsorption on the plastics surfaces. The MC molecules absorbed on plastics expose some of their polar groups oriented towards the aqueous phase, hence making the plastics surfaces hydrophilic. In addition, flotation selectivity for the plastics is dominated not only by wettability of plastics, but also by particle size, density and shape. 相似文献
965.
966.
库车前陆盆地寒武系 -第三系流体分析显示 :寒武系 -奥陶系和侏罗系油田水与白垩系 -第三系有所差异 ,前者总矿化度相对较低 ,为 90g/L~ 1 1 0g/L ;相对富Ca2 + 和HCO-3 ;后者总矿化度介于 73g/L~ 3 1 0g/L,主要为 1 3 0g/L~ 2 90g/L,相对富K+ +Na+ 和Cl-;而大宛齐第三系油田水则相对富Ca。影响水化学演化的因素包括 :膏盐类、沸石类矿物溶解以及白云化作用和富镁绿泥石形成等。白垩系油田水δ18O、δD关系显示为淡水蒸发成因 ,且在轮台断隆带油田水87Sr/86Sr向西降低 ,指示了富87Sr的流体来自东部的碎屑泥岩 ,这与本区煤成油运移方向是一致的。而 2个寒武系 -奥陶系油田水87Sr/86Sr高达0 .71 71 6,并富Li、B、Sr元素和δ18O ,被认为来自结晶基岩 ,与氮气、氦气及部分甲烷的来源一致。 相似文献
967.
968.
上海市郊4种地表径流及稻田水中的污染物浓度 总被引:12,自引:2,他引:12
测定了水田、旱田、村、镇4种地表径流中的污染物浓度,以及稻田渗漏水和稻田水中的污染物浓度。测定的污染物种类主要有:总悬浮物,SS、总氮、总磷、CODcr,CODMn及微生物浓度等。测定结果表明,除稻田渗漏水以外,4种地表径流水中的污染物浓度均高于上海市郊环境地面水浓度,其中以村径流的污染物浓度最高,另外,施肥后的稻田水中氮浓度很高,施肥后的暴雨会导至严重氮污染。 相似文献
969.
高浓度氨氮废水处理试验 总被引:4,自引:0,他引:4
采用二级吹脱加生化的方法处理高浓度氨氮废水,试验在工况I(气、水温均为4℃)和工况Ⅱ(气温4℃,水温28℃,pH=10.5)条件下分别进行静、动态试验,结果表明在工况Ⅱ条件下,氧化铁废水(浓氨水)的静、动态试验怕氮去除率分别为82.67%和84.19%;综合废水的静、动态试验氨氮去除率一级吹脱分别为62.03%和74.16%,二级吹脱后氨氮浓度降至82.16mg/L和74.32mg/L。再接上后续的生化处理,该废水能达到规定的排放标准。 相似文献
970.
氢化物发生—ICP/AES法测定地面水中的痕量砷 总被引:1,自引:0,他引:1
采用氢化物发生-ICP/AES法测定地面水中痕量砷,进行了分析线、正向入射功率的选择氢化物发生系统和气动雾化系统的性能比较等实验,砷的测定波长选用188.979nm,正向入射功率为850W。采用氢化物生系统进样,其灵敏度比气动雾化系统进样高75-110倍。方法的检测限为0.4μg/L;加标回收率为92.4%-104.6%;精密度实验的变异系数为1.8%-8.0%。 相似文献