Soil Water Table Level Research Articles

Effects of soil water table regime on tree community species richness and structure of alluvial forest fragments in Southeast Brazil

In order to determine the influence of soil water table fluctuation on tree species richness and structure of alluvial forest fragments, 24 plots were allocated in a point bar forest and 30 plots in five forest fragments located in a floodplain, in the municipality of São Sebastião da Bela Vista, Southeast Brazil, totalizing 54, 10 X 20 m, plots. The information recorded in each plot were the soil water table level, diameter at breast height (dbh), total height and botanical identity off all trees with dbh > 5 cm. The water table fluctuation was assessed through 1 m deep observation wells in each plot. Correlations analysis indicated that sites with shallower water table in the flooding plains had a low number of tree species and high tree density. Although the water table in the point bar remained below the wells during the study period, low tree species richness was observed. There are other events taking place within the point bar forest that assume a high ecological importance, such as the intensive water velocity during flooding and sedimentation processes.

Florística e estrutura da comunidade arbórea em fragmentos de floresta aluvial em São Sebastião da Bela Vista, Minas Gerais, Brasil

Fragments of alluvial forest in the South of Minas Gerais, Brazil, were studied in order to assess the vegetation structure, tree diversity and the most influential environmental variables on vegetation variations. The environment and vegetation data (dbh ³ 5 cm) were collected in 54, 20 × 10 m, permanents plots allocated in a riverine forest and in five fragments of alluvial forests. In the plots, the survey totalled 2,064 tree individuals, distributed in 51 species. The canonical correspondence analysis detected a tree composition gradient in the first axis, related to Mg, organic matter and H + Al soil content, sand and clay percentage and soil water table level. The CCA second axis was associated with canopy coverage and soil silte percentage. Theses variables caused a plot group formation related to species distribution.

Relações entre a distribuição das espécies de diferentes estratos e as características do solo de uma floresta aluvial no Estado do Paraná, Brasil

Entre os fatores que influenciam a distribuição de espécies nas comunidades vegetais localizadas em regiões ribeirinhas, as características do solo são consideradas os mais importantes. No presente estudo, foram avaliadas a composição florística, a diversidade e a estrutura de três estratos da vegetação e suas relações com as características do solo em um fragmento de floresta aluvial na bacia do rio Iguaçu, no estado do Paraná. Buscou-se verificar se a estrutura e a diversidade da floresta nos diferentes estratos podem ser explicadas por fatores edáficos e hídricos. Caracterizaram-se os parâmetros estruturais e a composição florística de três estratos da vegetação % de regeneração (20 cm < altura < 1,30 m; 80 sub-parcelas de 1 m×1 m), intermediário (perímetro à altura do peito - PAP < 15 cm, altura > 1,30 m; 20 sub-parcelas de 5 m×5 m) e superior (PAP > 15 cm, 20 parcelas de 10 m×10 m) - e correlacionaram-se as abundâncias das espécies com os parâmetros do solo e do lençol freático de cada parcela. A floresta caracterizou-se por baixa diversidade (H' = 2,36 no estrato de regeneração, 2,49 no estrato no estrato intermediário e 1,59 no estrato superior) e alta similaridade florística entre estratos (índices de similaridade de Sørensen > 0,65). As relações entre a distribuição espacial das espécies e as características do solo foram distintas entre estratos: no estrato superior correlacionou-se com a profundidade do lençol freático e o teor de matéria orgânica; no intermediário, com profundidade do lençol e teor de alumínio, porém no estrato inferior nenhum dos fatores ambientais analisados explicou a distribuição das espécies. Os resultados sugerem que a estrutura e a composição florística destas comunidades aluviais refletem os diferentes níveis de interação ao longo do ciclo de vida dos indivíduos.

CARBON DIOXIDE AND METHANE FLUXES IN DRAINED TROPICAL PEAT BEFORE AND AFTER HYDROLOGICAL RESTORATION

Present tropical peat deposits are the outcome of net carbon removal from the atmosphere and form one of the largest terrestrial organic carbon stores on the Earth. Reclamation of pristine tropical peatland areas in Southeast Asia increased strikingly during the last half of the 20th century. Drainage due to land-use change is one of the main driving factors accelerating carbon loss from the ecosystem. Dams were built in drainage-affected peatland area canals in Central Kalimantan, Indonesia, in order to evaluate major patterns in gaseous carbon dioxide and methane fluxes and in peat hydrology immediately before and after hydrologic restoration. The sites included peat swamp forest and deforested burned area, both affected by drainage for nearly 10 years. Higher annual minimum soil water table levels prevailed on both sites after restoration; the deforested site water table level prevailed considerably longer near the peat surface, and the forest water table level remained for a longer period in the topmost 30 cm peat profile after restoration. Forest soil gas fluxes were clearly higher in comparison to the deforested area. Cumulative forest floor CO2 emissions (7305-7444 g x m(-2) x yr(-1); 166.0-169.2 mol CO2 x m(-2) x yr(-1)) and the deforested site CO2 emissions (2781-2608 g x m(-2) x yr(-1); 63.2-59.3 mol CO2 x m(-2) x yr(-1)) did not markedly reflect the notably differing hydrological conditions the year before and after restoration. The forest floor was a weak CH4 sink (-0.208 to -0.368 g x m(-2) x yr(-1); -13.0 to -22.9 mmol CH4 x m(-2) x yr(-1)) and the deforested site a comparable CH4 source (0.197-0.275 g x m(-2) x yr(-1); 12.3-17.1 mmol CH4 x m(-2) x yr(-1)) in the study period. In general, higher soil water table levels had a relatively small effect on the annual CH4 emission budgets. In the two site types the gas flux response into hydrological conditions in degraded tropical peat can be attributed to differing CO2 and CH4 dynamics, peat physical characteristics, and vegetation.

Regressive modelling of soil water table fluctuations

Environmental and agricultural studies require spatial information on the soil water table level. Data collection based on dip-well measurements requires frequent measurements and a high number of dip-wells as the soil water table depth is varying strongly within short distances and time intervals. This paper presents a model based method, requiring a limited number of dip-wells and related mapped soil information, to describe water table depth fluctuations in time and space. A dip-well specific, regressive model was developed with meteorological data as input. This model described the fluctuations in time at the dip-well locations successfully. Based on the relationship between model parameters and mapped soil data, spatially extended models were created.

Evaluation of soil respiration and soil CO2 concentration in a lowland moist forest in Panama

Soil gas exchange was investigated in a lowland moist forest in Panama. Soil water table level and soil redox potentials indicate that the soils are not waterlogged. Substantial microspatial variation exists for soil respiration and soil CO2 concentration. During the rainy season, soil CO2 at 40 cm below the surface accumulates to 2.3%–4.6% and is correlated with rainfall during the previous two weeks. Temporal changes in soil CO2 are rapid, large and share similar trends between sampling points. Possible effects of soil CO2 changes on plant growth or phenology are discussed.

Inexpensive instrument for measuring soil water table levels. Note : Campbell, J A; Millette, J A; Roy, M Can J Soil Sci, V60, N3, Aug 1980, P575–577

Inexpensive instrument for measuring soil water table levels. Note : Campbell, J A; Millette, J A; Roy, M Can J Soil Sci, V60, N3, Aug 1980, P575–577

AN INEXPENSIVE INSTRUMENT FOR MEASURING SOIL WATER TABLE LEVELS

A simple and inexpensive instrument for measuring soil water table levels that can be used with metal or plastic wells was designed and constructed. The accuracy of the measurements is within ± 1 mm. The instrument has been thoroughly tested both in the field and in the greenhouse and proved to be very reliable.