Relationships between soil nitrate desorbed from anion-exchange membranes, canopy reflectance and nitrate leaching losses from cool-season lawn turf.

Nutrient leaching studies are expensive and require expertise in water collection and analyses. Less expensive or easier methods that estimate leaching losses would be desirable. The objective of this study was to determine if anion-exchange membranes (AEMs) and reflectance meters could predict nitrate (NO3-N) leaching losses from a cool-season lawn turf. A two-year field study used an established 90% Kentucky bluegrass (Poa pratensis L.)-10% creeping red fescue (Festuca rubra L.) turf that received 0 to 98 kg N ha-1 month-1, from May through November. Soil monolith lysimeters collected leachate that was analyzed for NO3-N concentration. Soil NO3-N was estimated with AEMs. Spectral reflectance measurements of the turf were obtained with chlorophyll and chroma meters. No significant (p > 0.05) increase in percolate flow-weighted NO3-N concentration (FWC) or mass loss occurred when AEM desorbed soil NO3-N was below 0.84 µg cm-2 d-1. A linear increase in FWC and mass loss (p < 0.0001) occurred, however, when AEM soil NO3-N was above this value. The maximum contaminant level (MCL) for drinking water (10 mg L-1 NO3-N) was reached with an AEM soil NO3-N value of 1.6 µg cm-2 d-1. Maximum meter readings were obtained when AEM soil NO3 N reached or exceeded 2.3 µg cm-2 d-1. As chlorophyll index and hue angle (greenness) increased, there was an increased probability of exceeding the NO3-N MCL. These data suggest that AEMs and reflectance meters can serve as tools to predict NO3-N leaching losses from cool-season lawn turf, and to provide objective guides for N fertilization.

Nitrate leaching from Kentucky bluegrass soil columns predicted with anion exchange membranes

Ideal nitrogen (N) management for turfgrass supplies sufficient N for high-quality turf without increasing N leaching losses. A greenhouse study was conducted during two 27-week periods to determine if in situ anion exchange membranes (AEMs) could predict nitrate (NO3-N) leaching from a Kentucky bluegrass (Poa pratensis) turf grown on intact soil columns. Treatments consisted of 16 rates of N fertilizer application, from 0 to 98 kg N ha-1 mo-1. Percolate water was collected weekly and analysed for NO3-N. Mean flow-weighted NO3-N concentration and cumulative mass in percolate were exponentially related (pseudo-R2=0.995 and 0.994, respectively) to AEM desorbed soil NO3-N, with a percolate concentration below 10 mg NO3-N L-1 corresponding to an AEM soil NO3-N value of 2.9 micro g cm-2 d-1. Apparent N recovery by turf ranged from 28 to 40% of applied N, with a maximum corresponding to 4.7 micro g cm-2 d-1 AEM soil NO3-N. Turf colour, growth, and chlorophyll index increased with increasing AEM soil NO3-N, but these increases occurred at the expense of increases in NO3-N leaching losses. These results suggest that AEMs might serve as a tool for predicting NO3-N leaching losses from turf.

Productores agropecuarios, pampa ondulada y problemáticas edáficas. Un estudio de caso en el noreste bonaerense

El carácter de la heterogeneidad social, económica y productiva de la agriculturización se evidencia en los diversos tipos de productores existentes en la pampa húmeda. La agriculturización se asocia a modificaciones en la calidad de las tierras, en la estructura socio-productiva, en las estrategias productivas aplicadas y en las formas de uso del suelo. Suele plantearse sin embargo que las problemáticas edáficas asociadas a dicha agriculturización, son consecuencia de la aplicación de paquetes tecnológicos relativamente homogéneos, independientemente de los diferentes tipos de productores que los llevan a cabo. Nuestra hipótesis consiste en cambio, en que el deterioro en Argiudoles típicos pampeanos es el resultado, dadas distintas posiciones del relieve, de complejas combinaciones de diversas estrategias productivas adoptadas por diferentes tipos de productores. En el partido de Luján tipificamos los productores tomando en consideración sus niveles de capitalización (capitalizados y no capitalizados) y su organización del trabajo (familiar y no familiar). Definimos cinco estrategias productivas (4 agrícolas -con uno o dos cultivos por año, con siembra directa o labranza convencional- y 1 ganadera) y dos ambientes (loma y bajo). A partir del catastro municipal aplicamos una encuesta a una muestra estratificada estadísticamente representativa, por ubicación y tamaño de lotes. Sobre la misma realizamos el muestreo que nos permitió analizar los siguientes parámetros: profundidad del horizonte, densidad aparente, materia orgánica, acidez, nitrógeno, fósforo, potasio. Calculamos el contenido de materia orgánica y de nitrógeno por hectárea, y el deterioro relativo. Realizamos test de hipótesis de comparación de medias, prueba F y prueba t; y, calculamos finalmente los deterioros relativos. Utilizamos como indicador el contenido de materia orgánica por hectárea, dada su mayor sensibilidad a los cambios en las condiciones del suelo. Dos de nuestros principales hallazgos nos indican, en primer lugar, que al cultivar en lomas y con siembra directa, todos los tipos de productores presentaron los valores más bajos de deterioro relativo, excepto los familiares no capitalizados que obtienen los menores deterioros relativos con labranza convencional, aún en los bajos. Estos productores utilizan la ganadería en rotación con los cultivos como táctica de cuidado del suelo. Los empresarios capitalizados presentan los mayores valores de deterioro relativo en los bajos. Los familiares presentan menores pérdidas, cuando son capitalizados logran las mejores situaciones relativas al aplicar siembra directa en los bajos. En segundo lugar, ninguna dimensión -tipo de productor, estrategias productivas, ambientes- analizada aisladamente determina el deterioro relativo de los suelos. Pero, al mismo tiempo, ninguno puede ser descartado sino que debería ser incluido en una combinación que integre las condiciones de ambiente y las estrategias productivas de los diferentes tipos de productores que manejan los suelos.

Part of the global DOC versus AOU (dissolved organic carbon/apparent oxygen utilization) data compilation, Ross Sea

Dissolved and particulate organic matter was measured during six cruises to the southern Ross Sea. The cruises were conducted during late austral winter to autumn from 1994 to 1997 and included coverage of various stages of the seasonal phytoplankton bloom. The data from the various years are compiled into a representative seasonal cycle in order to assess general patterns of dissolved organic matter (DOM) and particulate organic matter (POM) dynamics in the southern Ross Sea. Dissolved organic carbon (DOC) and particulate organic carbon (POC) were at background concentrations of approximately 42 and 3 µM C, respectively, during the late winter conditions in October. As the spring phytoplankton bloom progressed, organic matter increased, and by January DOC and POC reached as high as 30 and 107 µM C, respectively, in excess of initial wintertime conditions. Stocks and concentrations of DOC and POC returned to near background values by autumn (April). Approximately 90% of the accumulated organic matter was partitioned into POM, with modest net accumulation of DOM stocks despite large net organic matter production and the dominance of Phaeocystis antarctica. Changes in NO3 concentration from wintertime values were used to calculate the equivalent biological drawdown of dissolved inorganic carbon (DICequiv). The fraction of DICequiv drawdown resulting in net DOC production was relatively constant (ca. 11%), despite large temporal and spatial variability in DICequiv drawdown. The C : N (molar ratio) of the seasonally produced DOM had a geometric mean of 6.2 and was nitrogen-rich compared to background DOM. The DOM stocks that accumulate in excess of deep refractory background stocks are often referred to as "semi-labile" DOM. The "semi-labile" pool in the Ross Sea turns over on timescales of about 6 months. As a result of the modest net DOM production and its lability, the role DOM plays in export to the deep sea is small in this region.

Part of the global DOC versus AOU (dissolved organic carbon/apparent oxygen utilization) data compilation, Arabian Sea

Concentrations of total organic carbon (TOC) were determined on samples collected during six cruises in the northern Arabian Sea during the 1995 US JGOFS Arabian Sea Process Study. Total organic carbon concentrations and integrated stocks in the upper ocean varied both spatially and seasonally. Highest mixed-layer TOC concentrations (80-100 µM C) were observed near the coast when upwelling was not active, while upwelling tended to reduce local concentrations. In the open ocean, highest mixed-layer TOC concentrations (80-95 µM C) developed in winter (period of the NE Monsoon) and remained through mid summer (early to mid-SW Monsoon). Lowest open ocean mixed-layer concentrations (65-75 µM C) occurred late in the summer (late SW Monsoon) and during the Fall Intermonsoon period. The changes in TOC concentrations resulted in seasonal variations in mean TOC stocks (upper 150 m) of 1.5-2 mole C/m**2, with the lowest stocks found late in the summer during the SW Monsoon-Fall Intermonsoon transition. The seasonal accumulation of TOC north of 15°N was 31-41 x 10**12 g C, mostly taking place over the period of the NE Monsoon, and equivalent to 6-8% of annual primary production estimated for that region in the mid-1970s. A net TOC production rate of 12 mmole C/m**2/d over the period of the NE Monsoon represented ~80% of net community production. Net TOC production was nil during the SW Monsoon, so vertical export would have dominated the export terms over that period. Total organic carbon concentrations varied in vertical profiles with the vertical layering of the water masses, with the Persian Gulf Water TOC concentrations showing a clear signal. Deep water (>2000 m) TOC concentrations were uniform across the basin and over the period of the cruises, averaging 42.3±1.4 µM C.