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61.
湖滨带芦苇恢复过程中沉积物氮赋存形态及含量变化:以巢湖为例 总被引:1,自引:0,他引:1
水生植被对于维持水生态系统结构和功能稳定性具有举足轻重的作用,而重建水生植物被认为是污染湖泊生态修复的重要手段.氮素是水生态系统重要的限制性元素之一,根着挺水植物生长发育无疑将深刻地影响着沉积物氮的迁移转化过程,但水生植物不同生长阶段对沉积物氮的需求和植物代谢强度均不同,目前对挺水植物完整生长过程中沉积物氮组分及含量变化认识仍十分不足.本研究通过为期120d的沉积物柱芯培养和水槽模拟试验,探究巢湖芦苇恢复完整生长过程中沉积物总氮(TN)、无机氮(TIN)与可转化态氮(TF-N)的变化及其关键调控因子.结果表明,芦苇完整生长过程将持续激发沉积物氮活性,沉积物TIN与TF-N含量逐渐增加,而沉积物TN和非可转化态氮(NTF-N)含量显著降低.模拟试验期间,指数型增长的芦苇生物量提高了沉积物铵态氮(NH_4~+-N)和硝态氮(NO_3~--N)含量,但亚硝态氮(NO_2~--N)含量却逐渐降低;与第0天相比,第120天沉积物离子交换态氮(IEF-N)、碳酸盐结合态氮(CF-N)、铁锰氧化态氮(IMOF-N)和有机态及硫化物结合态氮(OSF-N)含量分别增加了 1.10、3.40、3.60和1.40倍,这主要受芦苇吸收利用、根系代谢强化根际沉积物氧化还原电势和改变pH微环境共同驱动.在第120天,沉积物NH_4~+-N和NO_3~--N含量急剧升高,分别是第90天的9.43和2.22倍,表明芦苇衰亡凋落过程将向沉积物释放大量的TIN,故需要综合采取湖泊物理—生态工程手段来有效管控芦苇枯落物,从而提升水生植被修复效果并构建长效稳态机制. 相似文献
62.
H.F. Aristizábal 《水文科学杂志》2019,64(8):885-899
Wetlands are vulnerable to groundwater extraction, which has proven detrimental to aquatic ecosystems around the planet. As wetlands rank among the world’s most endangered ecosystems, versatile strategies are required to protect them. This paper provides a modelling-based method to delineate protection buffers in wetlands subject to groundwater extraction. The technique is sufficiently flexible to cater to a wide variety of conditions, and simple enough to underpin management decisions on a daily basis. A numerical model is used to obtain a map of the critical rate of groundwater abstraction, based on the distance between wetlands and suitable discharge thresholds. The outcomes determine the allowed pumping rate at any point under steady and transient-state conditions. A new iteration is developed every time a new pumping allowance is made. This procedure is demonstrated by means of hypothetical scenarios, as well as by a case study application in the Valle del Cauca region, Colombia. 相似文献
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A natural decay of plant and animal biomass in aquatic environments results in the release of different simple structured organic substances into water. In our laboratory experiments we investigated whether some of them, e.g., starch or peptone, and also a complex yeast biomass can be transformed into humic-like substances by natural assemblages and some pure cultures of aquatic microorganisms. After a 6 months incubation most of the cultural media enriched with those natural organic substrates turned dark in color and humic-like substances (HS) could be isolated. However, the original substrate organic carbon was mainly mineralized in microbial cultures, and only about 3 % C was converted into HS. Total yields of HS differed in dependence of the individual substrate used (peptone > yeast > starch), the origin of inoculum (river > lake > groundwater), and the incubation temperature (20°C > 10°C). According to their elemental composition, and their spectroscopical and electrophoretic characteristics the microbially formed HS resembled natural aquatic humic matter, but were higher in aliphatic constituents (carbohydrates, peptides) and lower in aromatic structures. HS-like substances were also obtained from pure cultures of a bacterium Bacillus sphaericus and a fungus Cladosporium cladosporioides. The 13C and 15N isotopic contents of the microbially produced HS differed in dependence on the microbial inoculum and the type of organic substrates used, but in general they indicated anabolic processes to be mainly responsible for the humification of the simple organic substrates used in our experiments. 相似文献
65.
AbstractThe hydrology of water-dependent ecosystems around the world has been altered as a result of flow regulation and extraction for a variety of purposes including agricultural and urban water supply. The flow regime of the Murray-Darling Basin in Australia is no exception, with attendant impacts on the health of the environment. Restoration of parts of the flow regime is a key feature of environmental flow delivery. However, environmental flow delivery in a system that is managed primarily to provide a secure and stable supply for irrigation presents challenges for managers seeking to return more natural flow variability in line with ecosystem requirements. The institutional arrangements governing releases of water from storage can influence the ability of managers to respond to natural cues, such as naturally rising flows in a river. As such, the legal and governance aspects of environmental flow delivery are likely to be important influences on the outcomes achieved.
Editor Z.W. Kundzewicz; Guest editor M. AcremanCitation Banks, S.A. and Docker, B.B., 2014. Delivering environmental flows in the Murray-Darling Basin (Australia)—legal and governance aspects. Hydrological Sciences Journal, 59 (3–4), 688–699. 相似文献
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The physico‐chemical characteristics and microbial composition of the final effluents of two municipal wastewater treatment plants in South Africa were assessed between July and September 2009. The impact of the treated final effluents on the receiving water bodies was also evaluated. The temperature across all sampling points ranged between 14 and 22°C, while pH varied from 6.9 to 7.6. High levels of turbidity, chemical oxygen demand (COD), ammonia, nitrate, nitrite and orthophosphate (PO4) were observed in many cases. Turbidity of the samples was in the range of 2.2–288.6 NTU. The concentrations (mg/L) of other physico‐chemical parameters are as follows: COD (9.33–289); ammonia (0.000340–45.4); nitrate (0.062–539); nitrite (0.021–22.6); PO4 (5.3–33.2). The microbial quality of the effluents discharged from the plants did not comply with the limits set by the South African guidelines with respect to pathogens such as Salmonella, Shigella, Escherichia coli, total coliform, faecal coliform, enterococci, faecal streptococci, and viral particles for effluents intended for discharge into receiving watersheds. This study revealed an undesirable impact on the physico‐chemical and microbial qualities of the receiving water bodies as a result of the discharge of inadequately treated effluents from the wastewater treatment facilities. This poses a health risk to several rural communities which rely on the receiving water bodies primarily as their sources of domestic water and recreational purposes. There is therefore a need for the intervention of appropriate regulatory agencies in South Africa to ensure compliance of treatment facilities with wastewater effluent quality standards. 相似文献
70.
The geomorphic function and characteristics of large woody debris in low gradient rivers, coastal Maine, USA 总被引:1,自引:0,他引:1
F.J. Magilligan K.H. Nislow G.B. Fisher J. Wright G. Mackey M. Laser 《Geomorphology》2008,97(3-4):467-482
The role, function, and importance of large woody debris (LWD) in rivers depend strongly on environmental context and land use history. The coastal watersheds of central and northern Maine, northeastern U.S., are characterized by low gradients, moderate topography, and minimal influence of mass wasting processes, along with a history of intensive commercial timber harvest. In spite of the ecological importance of these rivers, which contain the last wild populations of Atlantic salmon (Salmo salar) in the U.S., we know little about LWD distribution, dynamics, and function in these systems. We conducted a cross-basin analysis in seven coastal Maine watersheds, documenting the size, frequency, volume, position, and orientation of LWD, as well as the association between LWD, pool formation, and sediment storage. In conjunction with these LWD surveys, we conducted extensive riparian vegetation surveys. We observed very low LWD frequencies and volumes across the 60 km of rivers surveyed. Frequency of LWD ≥ 20 cm diameter ranged from 15–50 pieces km− 1 and wood volumes were commonly < 10–20 m3 km− 1. Moreover, most of this wood was located in the immediate low-flow channel zone, was oriented parallel to flow, and failed to span the stream channel. As a result, pool formation associated with LWD is generally lacking and < 20% of the wood was associated with sediment storage. Low LWD volumes are consistent with the relatively young riparian stands we observed, with the large majority of trees < 20 cm DBH. These results strongly reflect the legacy of intensive timber harvest and land clearing and suggest that the frequency and distribution of LWD may be considerably less than presettlement and/or future desired conditions. 相似文献