Wood ant nests as potential hot spots for carbon and nitrogen mineralisation

Red wood ants (the Formica rufa group) build large nests which can last for many years. The ants often bring large quantities of conifer litter to their mounds. In this study we compared chemical properties of the forest floor and ant-nest materials of red wood ants at two different sites in Sweden. We also did an incubation study in the laboratory to determine C and N mineralisation rates of soil and nest materials at two moisture levels. Some chemical properties, e.g. pH and C/N ratio, differed between sites. Nests were always drier, had a higher C/N ratio and often had higher NH₄⁺ concentrations than the surrounding forest floor. This indicates that the nests increase spatial heterogeneity of the forest floor not only because they contain large amounts of organic matter but also because of qualitative differences in nest composition. In the incubation study, experimentally increased moisture levels in the nest material resulted in net N immobilisation, while surrounding litter and humus materials showed net N mineralisation. The CO₂ evolution was clearly increased by increased moisture. Dry conditions in the nest material prevented it from being decomposed and, since there were no plants to take up N, inorganic N accumulated. However, based on our results we hypothesise that ant nests do not produce large amounts of inorganic N as long as the ants bring fresh litter with high C/N ratio to the nests and keep the nests dry. However, the nests can be considered as potential "compost heaps" which probably decompose faster and will be a source of N leaching when the ants no longer maintain the specific dry conditions.     

The topographic thresholds of hillslope incisions in southwestern Rwanda

This article presents new quantitative evidence that land use in Rwanda contributes to the development of hillslope incisions.Two types of hillslope incisions can be distinguished in southern Rwanda. Incisions of the first type drain an area depending on the form and extension on the natural topography and geology. The Runyinya gully (25°) and the Rugabano soil slippage (39°) are two examples. On a logarithmic plot of critical slope inclination at the incision head versus drainage area towards the incision head, both incisions lay sensibly to the right of the Montgomery–Dietrich (M-D) envelope. The latter gives the range of these topographical thresholds for gully and mass-wasting incision in parts of North America. The Runyinya and Rugabano cases obey the linear equation:

S_cr=(±0.6)A^−(±0.6)

where S_cr=critical slope gradient (tangent of slope in °) at the gully head or the scar and A=the area (ha) drained towards the incision head.Hillslope incisions of the second group rely on a run-on area larger than normal because they are localised at the ‘outlet’ of artificially runoff-collecting systems like roads, soil conservational contour trenches, tracks and other linear landscape elements. Such systems often drain a surface much larger in extension than the natural run-on area to the ‘outlet.’ These hillslope incisions, taking into account their artificially big drainage area, concentrate more or less along the line:

S_cr=(±0.3)A^−(±0.6)

This line is about in the center of the Montgomery–Dietrich envelope. If, however, only the natural drainage area of these ‘outlet’ incisions is taken into account, all points fall close to the left border or even to the left of the Montgomery–Dietrich envelope. This indicates a much higher probability for incision in those localities receiving supplementary runoff or interflow from outside the natural drainage area. In the case of a soil slippage at Rwaza Hill, detailed stability calculations show that the slope failure should be due to excessive water infiltration into the bottom of a trench. The digging of the trench provoked an increase in the area drained to the slippage head by a factor of 6.The phenomenon of ‘forward’ erosion is compatible with the existence of threshold combinations of slope and drained area. For slopes steeper than 7–8°, the phase of regressive erosion does often follow the forward incision event with a delay of several years or more.Finally, the scanty data set now available for Rwanda suggests that the drainage area critical to hillslope incision on the red-brown ferrallitic soils in Rwanda might be nearly twice as big as those in North America.     

Analysis of the early stages of lipid oxidation in freeze-stored pork back fat and mechanically recovered poultry meat

An analytical method that can detect low levels of oxidation in food earlier than a sensory panel would be a valuable tool for food manufacturers as well as research institutes. Two model matrixes, pork back fat and mechanically recovered poultry meat (MRPM), were freeze-stored in air at -20 degrees C for 26 weeks. Peroxide value, thiobarbituric acid reactive substances, volatiles analyzed with dynamic headspace gas chromatography-mass spectrometry (GC-MS) and a gas-sensor array technique (electronic nose), chemiluminescence, and front-face fluorescence were evaluated against sensory analysis with regard to detection of early oxidation and correlation with sensory data. Fluorescence and GC-MS could detect oxidative changes in pork back fat earlier than the sensory panel and the electronic nose at the same time. The three methods were highly correlated with sensory attributes (r = 0.8-0.9). GC-MS gave the best results with regard to detection of small oxidative changes in MRPM.     

The effect of acidification,liming and reacidification on macrophyte development,water quality and sediment characteristics of soft-water lakes

Rapid expansion of Juncus bulbosus L. and the concomitant suppression of isoetid plant species has often been observed in acidifying soft water lakes in Western Europe. Experimental studies have shown that this mass development of J.bulbosus was caused by changes in the carbon and nitrogen budgets in these ecosystems. Acidification leads to temporarily strongly increased carbon dioxide (CO₂) levels in the slightly calcareous sediment and to accumulation of ammonium as a result of a reduced nitrification rate in acidifying waters. Many acidifying Scandinavian soft water lakes, however, have a well developed macrophyte vegetation. It is suggested that this is related with the non-calcareous sediments of these lakes. After liming, however, mass development of J. bulbosus and/or Sphagnum spec. has been observed in Swedish and S.W. Norwegian lakes. From field experiments it has become clear that part of the lime is deposited on the sediments leading to an increase of mineralisation rates, CO₂ production, sediment pore water levels of phosphate and ammonium and to a decrease of the nitrate concentrations in the sediment. These changes have been earlier observed in acidifying West European waters. Rooted species like J.bulbosus can only benefit from the higher nutrient levels in the sediment when the CO₂ level of the water layer is relatively high as this species is adapted to leaf carbon uptake. It is demonstrated that gradual reacidification by the acid water from the catchments and the increased flux of carbonic acid from the limed sediments to the overlying water leads to increased CO₂ levels in the water layer of the limed lakes already a few months after liming.     

The effects of water and hydrosol chemistry on the accumulation of beryllium and germanium in selected species of macrohydrophytes

The accumulation of Be and Ge by selected macrohydrophytes in environments polluted by industrial dust and waste products was shown to be higher than the average concentrations in unpolluted water. The Ge content of macrohydrophytes in polluted environments ranges from 7.1 to 220.4 μg g^?1 and the Be content from 0.7 to 136.6 μg g^?1. We have at the same time shown the relationships between Be and Ge in water and plants. The accumulation of Be and Ge in plants is conditioned by the amount of N and K in water, hydrosol and in the plants themselves. Our experiments show growth disturbances in macrohydrophytes containing high concentration of Be and Ge.     

Aluminium and sulphate in acidic soils and groundwaters on the Swedish west coast

Acidic groundwaters and soils in Halland County (Hailands län), southwest Sweden, have been investigated with respect to conditions of soluble aluminium (Al) and sulphate (SO₄ ^2?. Basic Al-sulphate, Fe-oxide, Al-oxide, Al-hydroxide and clay minerals, are discussed and evaluated in their roles for governing Al and SO₄ ^2? in the groundwaters. Based on this investigation, it is suggested that Al³⁺ solubility is controlled by amorphous Al-hydroxide. The SO₄ ^2? in the groundwaters will depend primarily on the H₂SO₄ input. The H₂SO₄ load enhances soil mineral weathering which enhances the production of Fe-oxides, i.e. anion exchange surface sites, to which groundwater SO₄ ^2? attain adsorption equilibra. The factors that control solubility of Al and SO₄ ^2? are both influenced by the acidity in the soil catenas which in the area largely depend on the H₂SO₄ input. Clay minerals such as illite, smectites, halloysite, and variable composition Al-silicates do not exert strong control on Al in the groundwaters investigated.     

Tree species selection for land rehabilitation in Ethiopia: from fragmented knowledge to an integrated multi-criteria decision approach

Dryland regions worldwide are increasingly suffering from losses of soil and biodiversity as a consequence of land degradation. Integrated conservation, rehabilitation and community-based management of natural resources are therefore of vital importance. Local planting efforts should focus on species performing a wide range of functions. Too often however, unsuitable tree species are planted when both ecological suitability for the targeted area or preferences of local stakeholders are not properly taken into account during selection. To develop a decision support tool for multi-purpose species selection, first information needs to be pooled on species-specific ranges, characteristics and functions for a set of potentially valuable species. In this study such database has been developed for the highly degraded northern Ethiopian highlands, using a unique combination of information sources, and with particular attention for local ecological knowledge and preferences. A set of candidate tree species and potentially relevant criteria, a flexible input database with species performance scores upon these criteria, and a ready-to-use multi-criteria decision support tool are presented. Two examples of species selection under different scenarios have been worked out in detail, with highest scores obtained for Cordia africana and Dodonaea angustifolia, as well as Eucalyptus spp., Acacia abyssinica, Acacia saligna, Olea europaea and Faidherbia albida. Sensitivity to criteria weights, and reliability and lack of knowledge on particular species attributes remain constraints towards applicability, particularly when many species are jointly evaluated. Nonetheless, the amount and diversity of the knowledge pooled in the presented database is high, covering 91 species and 45 attributes.