底泥养分富集条件下11种水生植物的光合氮利用效率

为揭示水生植物对富营养化河涌底泥的生理生态适应性及其净化能力,选取11种水生挺水植物(包含6种本土植物和5种外来植物)结合河涌底泥进行试验。通过测定试验一年后植物叶片的光饱和光合速率(P_(sat),μmol m~(-2)s~(-1))、比叶面积(SLA,m~2/kg)、总氮含量(TN,mg/g)和光合作用氮利用效率(PNUE,μmol mol~(-1)s~(-1)),比较分析物种间生理与结构特性及其相互关系。结果表明:种间的SLA层次比较分明,最高的大叶皇冠草(20.31±0.30)与最低的鸢尾草(7.22±0.31)相差近3倍。种间的P_(sat)在(3.76±0.57)(鸢尾草)—(21.53±1.20)(水罂粟)之间,水罂粟比鸢尾草高81.79%。种间的PNUE从42.53±8.42(鸢尾草)至655.8±100.93(天使花),美人蕉、水罂粟、风车草和香蒲的PNUE值均较高,且差异不明显(P0.05),这些植物的PNUE显著高于较低PNUE的种类(包括菖蒲、蓝花草和鸢尾草)(P0.05)。种间SLA分别与PNUE和P_(sat)(μmol kg~(-1)s~(-1))呈显著的正相关,SLA和P_(sat)(μmol m~(-2)s~(-1))分别与TN(mmol/m~2)呈显著负相关(P0.05)。外来植物类群的PNUE、SLA、P_(sat)和TN均显著高于本地植物类群(T-test,P0.05),说明外来水生植物在养分富集化环境下能更有效地利用资源,具有潜在的高生长速率和种间竞争优势。     

基于水蚀预报模型的黄土高原水平阶减流阻蚀效应模拟

黄土高原是我国土壤侵蚀最严重的地区,如何合理开展坡改梯工程对防治水土流失具有重要意义。本研究应用WEPP模型模拟坡面尺度降雨—侵蚀过程,模拟分析径流小区(10 m坡长)在不同坡度的水土流失特征和二阶、三阶水平阶在不同台面宽度(1,1.5,2 m)的减流阻蚀效应。结果表明:1)坡面尺度上,径流量和侵蚀量随坡度增加而增加。坡度达到20°时,径流量随坡度增加保持稳定,产沙量增加趋势渐缓;2)与坡面小区对比,二阶和三阶水平阶随台宽增加对地表径流调控率分别从6.5%增加到61.2%,从10.1%增加到69.7%;二阶水平阶在中(1.0 mm/min)、大(1.5 mm/min)雨强下,台面宽度大于1.5 m时产沙量小于坡面,泥沙调控率从1.1%增加到68.8%,三阶水平阶泥沙调控率从1.4%增加到82.3%;3)依据单位台宽减沙量,合理设计水平阶,使其减沙效益最大化。小雨强(0.5 mm/min)时,二阶、三阶水平阶的台面宽度达到1.5 m和1 m时可发挥优良的水土保持效果;中雨强(1.0 mm/min)时,台宽1.5 m的三阶水平阶效果最佳;大雨强(1.5 mm/min)时,则以2 m台宽的三阶水平阶效果更好。应用WEPP模型为定量评价工程措施的水土保持效益提供技术支撑。     

Paleolimnology of a small oligotrophic lake on Wolin Island,Baltic Sea,Poland

Paleolimnological studies which included analyses of diatoms, fossil pigments and physico-chemical characteristics of bottom sediments have been used to describe the limnological history of Racze Lake. The influx of terrigenous material into the lake have been determined on the basis of stratigraphy of elements associated with mineral content. The successively eroded soils as well as process of chemical erosion caused increase leaching of metals Mg, Fe, Al into the lake basin. However the concentration of these metals finally deposited in bottom sediments was also effected by the oxygen regime at the sediment-water interface. Both ratios, chlorophyll derivatives to total carotenoids (CD:TC) and Fe:Mn indicated hypolimnetic oxygen depletion in the middle part of the profile. The development of blue-green algal population, estimated by the ratio epiphasic to hypophasic carotenoids (EC:HC) was correlated with periods of redox conditions in the lake. The pH changes ranged from 6.5 to 7.7. The most important factors effecting pH changes were inflow of mineral matter from the watershed and structural changes in the littoral biocenosis.     

Major element chemistry,weathering and element yields for the Caura River drainage,Venezuela

The Caura River, a major tributary of the Orinoco River, was sampled at bi-weekly intervals for two years. Because the watershed is covered with undisturbed forest overlying a Precambrian shield, the water of the Caura River has low conductivity (mean, 15 uS/cm), contains small amounts of particulate material (mean, 11 mg/1), and is slightly acidic (median pH, 6.8). Concentrations of total dissolved solids vary less than two-fold in response to the seasonal ten-fold variation in discharge; concentrations of particulate material vary more (ten-fold) and are lowest at the time of peak discharge. Seasonal changes in concentrations of Si, major metal cations, and hydrogen ion are complementary to each other and indicate regular seasonal changes in weathering rates. Measurements of bulk atmospheric deposition and the observed runoff yield of Cl and S were used in estimating the basin-wide atmospheric deposition of major elements, which were as follows (kg/ha/yr): Ca, 1.3; Mg, 0.29; Na, 8.2; K, 1.0; Cl, 12; S, 2.8; P, 0.14. Element ratios show that terrestrial sources contribute strongly to the atmospheric deposition of Ca, K, S, and P. From the atmospheric contributions and runoff yields, watershed retention was computed for major elements with reference to Si. The watershed accumulates Al, Fe, and P, whereas losses of Ca, Mg, Na, K, and S originating from non-atmospheric sources exceed the relative loss rates of Si. The rock weathering rate based on Si is 1.8 cm/ 1,000 years. Although significant amounts of Ca, Mg, Na, and K are found in atmospheric deposition, the dominant influence on the mass balances of these elements is weathering rather than deposition. Weathering has a trivial influence on the cycles of Cl and S. Both atmospheric deposition and weathering are important in the mass balance of P. The ecosystem does not effectively conserve most biologically active elements (Ca, Mg, Na, K). The ecosystem conserves significant amounts of phosphorus (31% of total input), but probably by abiotic mechanisms.     

Sedimentary records of carbonaceous particles from fossil fuel combustion

Carbonaceous particles produced by fossil fuel combustion can be found in considerable amounts in recent lake sediments. As these particles contain elemental carbon they are resistant to chemical decomposition and therefore both well preserved in sediments and possible to quantify. Sediment samples can be oxidized with H₂O₂ and digested with HF without the particles being destroyed. The pioneers in studying carbonaceous particles in lake sediments in relation to fossil fuel combustion were J. J. Griffin and E. D. Goldberg. They measured elemental carbon concentrations in Lake Michigan sediments, mainly by infrared assay. On the basis of these analyses, size distribution measurements and also morphological studies of single particles they concluded that the carbonaceous particle record reflected the onset of industrial activity and the increased intensities of fossil fuel combustion during the twentieth century. Similar results have been obtained from another lake in the USA by B. K. Kothari and M. Wahlen. We have counted spherical carbonaceous particles (larger than 5–10 µm), which are characteristic for oil and coal burning, in several lake sediments. In Swedish lakes, the annual accumulation of coarse carbonaceous spheres in varved sediments and the concentration stratigraphy in non-varved sediments, follow the same main pattern as statistical data for the Swedish coal and oil combustion over the last two centuries. Coarse carbonaceous spheres in two sediment profiles from Scottish lakes have also been counted. As for the USA and Sweden the sedimentary record was found to reflect the history of fossil fuel combustion.     

Chemical sediment stratigraphy of four high alpine lakes in Austria

Chemical sediment stratigraphy of four high alpine lakes is discussed with respect to atmogenic eutrophication as well as acidification. All lakes show more or less clearly paleoindications of atmospheric, anthropogenic impacts, mainly as slight eutrophication (Schwarzsee and Upper Plenderlesee, Tyrolia, and Gippersee, Carinthia). In Schwarzsee and Goaßelesee (Carinthia), there are weak but not yet significant indications of slight lake acidification, additionally.     

Rotifer sampling — a complete species list from one visit?

This paper describes a possible method of compiling a rotifer species list for any site from a single visit. Sediment samples collected from Loch Leven on one occasion in winter were exposed to light and a range of temperature conditions in the laboratory. Resting eggs in the sediment were induced to hatch. The resultant species list was very similar to that obtained from regular plankton collections over the previous six year period.     

Effects of wind on a shallow lake ecosystem: Resuspension of particles in the Loosdrecht Lakes

Horizontal variation of seston concentration in the shallow, eutrophic Loosdrecht Lakes (A=9.8 km²; =1.9 m) was studied in relation to windspeed and effective fetch. Simple wave theory was applied in order to predict resuspension using wind data from a nearby meteorological station. Most results were consistent with the theory, but a clear limit for the occurrence of resuspension could not be established. Generally, changes in epipelon—the particles at the sediment-water interface — were not directly related to computed frequency of resuspension at the sampling station. The frequency was estimated for 37 grid points over the entire lake. Resuspension was computed to affect high percentages of the lake area in winter. In summer the frequency was much lower, but in June and July 1984 there were days with nearly 50% of the lake area subject to resuspension. The resulting input of particulate organic carbon into the water column during these days was estimated to equal 12–25 times the daytime phytoplankton carbon fixation. Most of the resuspended matter appeared to be redeposited rapidly. The computed frequency of resuspension for the 37 locations of the lake varied between 7 and 48 days in 1984.     

NAPL mobility of OPA-containing sediments

ABSTRACT

In situ deposited non-aqueous phase liquid (IDN) sediments have unique characteristics that inherently mitigate the movement of separate phase liquids. IDN sediments are composed of oil-particle aggregates (OPAs). OPAs consist of an oil bead or globule with attached solid particles, such as clay platelets, silt and sand granules, and/or organic materials. IDN sediments develop at locations where a continual or near continual discharge of non-aqueous phase liquids (NAPLs) have occurred over a period of time. IDN sediments consist of an open network of small pores where fluids are retained. Although the pore structure is very open, the pore openings are relatively small, which appears to inhibit fluid movement. In particular, capillary pressure analyses indicate that NAPL was not generally released until pressures of at least 15 pounds per square inch (psi) were induced. In addition, centrifuge testing at 1,000 G shows that NAPL immobility is observed in samples at NAPL saturations as high a 12%. These data suggest that NAPL is retained within the smallest pores and is encapsulated within a network of larger pores filled with water. Although the sediment contains NAPL, this original OPA structure appears to inhibit the oil beads from coalescing, preventing NAPL flow.