Kandiah Sanmugadas

Subsurface denitrification in a forest riparian zone: Interactions between hydrology and supplies of nitrate and organic carbon

The influence of hydrology andpatterns of supply of electron donors and acceptors onsubsurface denitrification was studied in a forestriparian zone along the Boyne River in southernOntario that received high nitrogen inputs from a sandaquifer. Two hypotheses were tested: (1) subsurfacedenitrification is restricted to localized zones ofhigh activity; (2) denitrification zones occur atsites where groundwater flow paths transportNO3− to supplies of available organiccarbon. A plume of nitrate-rich groundwater withconcentrations of 10–30 mg N L−1 flowed laterallyat depths of 1.5–5 m in sands beneath peat for ahorizontal distance of 100–140 m across the riparianzone to within 30–50 m of the river. In situ acetyleneinjections to piezometers revealed that significantdenitrification was restricted to a narrow zone ofsteep NO3− and N2O decline at theplume margins. The location of these denitrificationsites in areas with steep gradients of groundwater DOCincrease supported hypothesis 2. Many of thesedenitrification “hotspots” occurred near interfacesbetween sands and either peats or buried river channeldeposits. Field experiments involving in situadditions of either glucose or NO3− topiezometers indicated that denitrification wasC-limited in a large subsurface area of the riparianzone, and became N-limited beyond the narrow zone ofNO3− consumption. These data suggest thatdenitrification may not effectively removeNO3− from groundwater transported at depththrough permeable riparian sediments unlessinteraction occurs with localized supplies of organicmatter.

Hyporheic zone hydrology and nitrogen dynamics in relation to the streambed topography of a N-rich stream

The influence of riffle-pool units on hyporheic zone hydrology and nitrogen dynamics was investigated in Brougham Creek, a N-rich agricultural stream in Ontario, Canada. Subsurface hydraulic gradients, differences in background stream and groundwater concentrations of conservative ions, and the movement of a bromide tracer indicated the downwelling of stream water at the head of riffles and upwelling in riffle-pool transitions under base flow conditions. Channel water also flowed laterally into the floodplain at the upstream end of riffles and followed a subsurface concentric flow path for distances of up to 20 m before returning to the stream at the transition from riffles to pools. Differences in observed vs predicted concentrations based on background chloride patterns indicated that the hyporheic zone was a sink for nitrate and a source for ammonium. The removal of nitrate in the streambed was confirmed by the loss of nitrate in relation to co-injected bromide in areas of downwelling stream water in two riffles. Average stream water nitrate-N concentrations of 1.0 mg/L were often depleted to <0.005 mg/L near the sediment-water interface. Consequently, an extensive volume of the hyporheic zone in the streambed and floodplain had a large unused potential for nitrate removal. Conceptual models based mainly on studies of streams with low nutrient concentrations have emphasized the extent of surface-subsurface exchanges and water residence times in the hyporheic zone as important controls on stream nutrient retention. In contrast, we suggest that nitrate retention in N-rich streams is influenced more by the size of surface water storage zones which increase the residence time of channel water in contact with the major sites of rapid nitrate depletion adjacent to the sediment-water interface.

Temporal Variability in Atmospheric Nutrient Influx to a Tropical Ecosystem

The daily input of plant macro-nutrients in bulk precipitation was measured over a 16-month period at Siguatepeque, Honduras. Total annual inputs of all elements were small relative to those recorded elsewhere in the tropics, a difference which is attributed to the low rainfall of the area, its elevation, and its remoteness from the ocean. Input patterns were highly irregular with most of the annual influx of each element taking place on only a few rain days. A major influx of all elements was recorded at the start of each wet season, and one period of exceptionally high cation input during the wet season is tentatively attributed to volcanic activity. Despite the irregularity of nutrient influx, calculation of a daily water balance for the area shows that a large proportion of elements received can normally be retained temporarily in soil-moisture storage. However, effective capture of these by ecosystems probably requires rapid plant uptake. We suggest that plants occupying infertile tropical soils may be strongly selected for the ability to absorb irregular pulses of atmospheric nutrients.

Chemistry, mineralogy and microbiology of termite mound soil eaten by the chimpanzees of the Mahale Mountains, Western Tanzania

Subsamples of termite mound soil used by chimpanzees for geophagy, and topsoil never ingested by them, from the forest floor in the Mahale Mountains National Park, Tanzania, were analysed to determine the possible stimulus or stimuli for geophagy. The ingested samples have a dominant clay texture equivalent to a claystone, whereas the control samples are predominantly sandy clay loam or sandy loam, which indicates that particle size plays a significant role in soil selection for this behaviour. One potential function of the clays is to bind and adsorb toxins. Although both termite mound and control samples have similar alkaloid-binding capacities, they are in every case very high, with the majority of the samples being above 80%. The clay size material (<2 μm) contains metahalloysite and halloysite, the latter a hydrated aluminosilicate (Al 2 Si 2 O 4 -nH 2 O), present in the majority of both the termite mound soil and control soil samples. Metahalloysite, one of the principal ingredients found in the pharmaceutical Kaopectate is used to treat minor gastric ailments in humans. The soils commonly ingested could also function as antacids, as over half had pH values between 7.2 and 8.6. The mean concentrations of the majority of elements measured were greater in the termite mound soils than in the control soils. The termite mound soils had more filamentous bacteria, whereas the control soils contained greater numbers of unicellular bacteria and fungi.

Analysis of geophagy soils in Kibale Forest, Uganda

Four soil samples from the Kibale Forest, Uganda, representative of material regularly ingested by chimpanzees, were studied for their mineral, chemical, and geochemical composition. These geophagy soils have a high content of metahalloysite, a partially hydrated clay mineral that may act much like the pharmaceutical Kaopectate™. Among the elements that may act as a stimulus or stimuli for geophagy behavior, only iron is very high (total iron ranges from 6% to 17%); other possibilities such as calcium, chromium, cobalt, bromine, and iodine are either relatively low or are below their detection limits. Chlorine is below detection limits which eliminates sodium chloride as a possible stimulus. Depending on relative availability in the gut, iron offers the most likely chemical stimulus for geophagy and given the mineral composition of the samples, metahalloysite is the most likely mineral stimulus. Iron may play a role in replenishing hemoglobin which would be important in chimpanzee physiology at high elevations near the flanks of the Ruwenzori Mountains. Metahalloysite, which in this case exists in a relatively pure crystalline form, may well act to quell symptoms of diarrhea and act similarly to Kaopectate™. Organic chemical analyses indicate only traces of organic matter and no humic acids in the K14-E14 sample.

Denitrification rates in relation to stream sediment characteristics

Abstract Potential rates of nitrate removal were studied in sediments from three Ontario rivers that differed in texture, organic carbon contents and other characteristics. Intact 0–5 cm depth sediment cores from 22 sites on each river were overlain with aerated 5 mg 1 −1 NO 3 − -N solution and incubated in the laboratory at 21°C for 48 h. Rates of nitrate-N loss from the overlying solutions varied from 37 to 412 mg m −2 day −1 for a 24 h incubation period. The acetylene blockage technique was used with nitrate amended sediments to evaluate the relative importance of denitrification and nitrate reduction to ammonium. Denitrification accounted for 80–100% of the nitrate loss in the majority of sediment samples tested. Rates of nitrate loss for the 24 h period exhibited a highly significant positive correlation ( r = 0.82–0.89) with the water-soluble carbon content of the sediments in each river. Significant relationships were also observed between nitrate loss and organic carbon, total nitrogen and sediment ammonium. A decline in nitrate loss via denitrification and increased nitrate reduction to ammonium was correlated with the organic carbon and water-soluble carbon content of the stream sediments.

Geophagy amongst rhesus macaques on Cayo Santiago, Puerto Rico

Soil mining and eating (geophagy) behavior of rhesus macaques (Macaca mulatta) on Cayo Santiago, Puerto Rico, is described and assessed with respect to the chemical, geochemical, and mineralogical composition of the ingested materials. The samples forming the uneaten (control) and eaten (matrix and blocky) groups of soils come from the top and flanks of a marine terrace underlain with volcanic tuff on Cayo Santiago, off the east shore of Puerto Rico. Both the uneaten and geophagy samples were analyzed to determine particle size distributions, clay and primary mineralogy, and soil chemical and geochemical compositions. Primary minerals such as orthoclase and plagioclase feldspar in the clay fraction is higher in the control group than in the ingested samples. Both the control and matrix plus blocky samples have moderate to abundant amounts of kaolinite and halloysite (both silicon:aluminum = 1:1 type clay minerals) that may be important as a stimulus to geophagy behavior. The pH, total salts, and phosphorus levels in both the control and geophagy samples show considerable overlap with little clear indication of causal factors. Analysis of the geochemical data showed no clear cut elemental differences to suggest elemental supplementation as a possible explanation for mining and eating of tropical soil. It is possible that rhesus macaques ingest clay to obtain kaolinite/halloysite minerals which may alter the taste of their provided food, and may act as pharmaceutical agents to alleviate intestinal ailments such as diarrhea.

Middle-Holocene timberline fuctuation: influence on the genesis of Podzols (Spodosols), Norra Storfjället Massif, northern Sweden

Fluctuations of the altitudinal position and composition of the timberline in northern Sweden have occurred in response to climatic changes following deglaciation (c. 8800 yrs BP). In this study a soil sequence of predominantly Podzols (Spodosols) was analysed to determine if the soil profiles located above the present timberline were actively forming in the low-alpine environment, or whether they represent relict features of a once stronger pedogenic regime. The results of the soil analysis indicate a relatively uniform parent material with increasing fines near the surface reflecting aeolian influxed sediment. The soil profiles located above the timberline are generally characterized by darker colours, although with a lower accumulation of organic carbon and either similar or higher iron and aluminium in the spodic horizon than are found in the profiles located below the timberline. The alpine Podzols, generally located in protected swales, are quite distinct from Brunisols (Inceptisols) and Regosols (Entisols) found in slopes and swells on the predominantly undulating morainic and glaciofluvial landscape. This appears to indicate that Spodosols located above the present timberline are not actively being modified under the present low-alpine environmental conditions, but rather were initiated during the Atlantic Chronozone when a dwarf or stunted forest extended to approximately 900 m above sea level.

Prescribed burning of Pinus oocarpa in Honduras I. Effects on surface runoff and sediment loss

Abstract The effects of low-intensity prescribed burning on surface runoff and sediment loss were studied in a stand of oocarpa pine ( Pinus oocarpa Schiede) in central Honduras. The effects of burning in two seasons were compared on small paired plots on 10°, 25° and 40° slopes. Over a period of almost 2 years, mean percent runoff was 1.73% on the control plots and 5.03% on the burned plots. Mean sediment loss during the same period was 80 kg ha −1 on the control plots and 1732 kg ha −1 on the burned plots. The relationship between slope and surface runoff and sediment loss was negative; the effect of slope being masked by variation of other site factors. Recovery from burning was rapid and is attributed to the rapid rate of recovery of the ground vegetation of grasses and forbs which are adapted to frequent burning. Surface runoff and sediment loss on control plots were very low and the increases caused by burning are considered an acceptable alternative to the exposure of the overstory and site to the high risk of wildfires in accumulated fuels. Greater runoff and sediment loss were recorded on the plots burned in February than on those burned in June. As the period November to mid-February offers the greatest number of days with weather conditions suitable for low-intensity prescribed burning, it is concluded that burning for hazard reduction should be conducted as early as possible in this period, in November and December, to permit greater recovery of the ground vegetation before the heavy rains of May and early June.

Extractable FeAl and geochemistry of late pleistocene paleosols in the Dalijia Shan, western China

Surface paleosols in two tills and a diamicton were analyzed for extractable Fe and Al and to determine if elemental distributions would assist in the interpretation of past and present soil-forming environments. Extractable Fe and Al distributions indicate that leaching (based on movement of Fep) is pronounced in paleosols dating from the last glaciation. Moreover, analysis of oxalate extractable Fe and dithionite extractable Fe (FeoFed) shows that amorphous Fe increases with depth in all three paleosola with similar rates of conversion to crystalline Fe. Data for extractable forms of Al-oxides show somewhat higher values of pyrophosphate extractable Al with time. Because the climate in the field area is dry (precipitation < 760 mm) the amounts of crystalline Fe (Fed) in paleosols dating from early and late stades of the last glaciation are not high. Using values in the paleosol sola the difference amounts to 0.4%. Pyrophosphate extractable Fe shows a pronounced increase in the two older paleosols that may result from interstadial paleoclimates of the last glaciation. The geochemistry of the glacial and aeolian sediments (paleosols) indicates differences that they are probably related to the source areas of the different parent materials.