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Sand Soil (sand + soil)

Distribution by Scientific Domains
Life Sciences25%
Engineering25%
Earth and Environmental Science25%

Kinds of Sand Soil

  • loamy sand soil
    		•

    Selected Abstracts

    Evaluation of laboratory assays for the assessment of leaching of copper and chromium from ground-contact wood

    ENVIRONMENTAL TOXICOLOGY & CHEMISTRY, Issue 10 2007
    Ana I. García-Valcárcel
    Abstract Laboratory studies were conducted to assess the leaching of Cu and Cr from wood, treated with a Cu-Cr-B preservative, when placed in contact with soil. Two laboratory assays were performed: Wood in contact with soil solutions over 30 d, and wood in direct contact with soil over 30 weeks. The influence of several factors, such as soil type and fertilizer use, was studied in both assays. In addition, the effect of soil moisture content and temperature was evaluated when wood was in contact with soil. A discrepancy in the results of the laboratory assays was observed. Leaching of Cu and Cr increased when soil in contact with wood was fertilized, but only an increase of Cu leaching was observed when soil solutions from fertilized soils were used. Moreover, soil solutions from a sandy clay loam soil produced a higher Cu leaching than those from a loamy sand soil, whereas the contrary occurred when treated wood was in direct contact with these soils. In the assay of treated wood in ground contact, the highest metal losses were produced in fertilized soils maintained at constant temperature and high soil moisture content, the latter being the most important factor. These losses were in the range of 5.34 to 15.6% for Cu and 1.85 to 2.35% for Cr in the soils studied. The proposed laboratory assay, using treated wood in direct contact with soil at a moisture content near field capacity during a period of 30 weeks, produced total metal losses that were in accordance with those reported by other authors under field conditions, expressed on a per-year basis. [source]

    Vapor Intrusion in Homes over Gasoline-Contaminated Ground Water in Stafford, New Jersey

    GROUND WATER MONITORING & REMEDIATION, Issue 1 2006
    Paul F. Sanders
    The potential for chemical vapor intrusion from contaminated ground water to the interior of homes was investigated at a site with a leaking underground gasoline storage tank in Stafford Township, New Jersey. This location exhibited conditions favorable to vapor intrusion, with sand soil and a water table depth of 3.3 m. Concentrations of volatile organic chemicals in the ground water were as high as 82 mg/L for total benzene, toluene, ethylbenzene, and xylene (BTEX) and up to 590 mg/L for methyl- t -butyl ether (MTBE). Soil vapor samples at multiple depths were taken adjacent to several homes. Inside the homes, air samples were taken on the main floor, in the basement, and under the foundation slab. Despite high ground water concentrations, only one home had measurable impacts to indoor air quality attributable to some of the ground water contaminants. In this house, the BTEX chemicals were not detected in the basement, indicating a lack of indoor air impacts from the ground water for these chemicals. Oxygen measurements suggested that degradation attenuated these chemicals as they diffused through the vadose zone. However, MTBE, 2,2,4-trimethylpentane (isooctane), and cyclohexane were found in the indoor air. The first two of these chemicals served as gasoline-specific tracers and indicated that vapor intrusion was occurring. Attenuation factors (the ratio of the indoor air concentration to a source soil vapor concentration) for the BTEX chemicals between the ground water and the indoor air were <1 × 10,5, and for MTBE was 1.2 × 10,5. Attenuation factors between the deep-soil vapor and the basement air were as follows: BTEX compounds, <1 × 10,5; MTBE, 2.2 × 10,5; 2,2,4-trimethylpentane, 3.6 × 10,4; and cyclohexane, 1.2 × 10,4. Attenuation factors between the subslab vapor and the basement air were 7 to 8 × 10,3. [source]

    The effects of log erosion barriers on post-fire hydrologic response and sediment yield in small forested watersheds, southern California,

    HYDROLOGICAL PROCESSES, Issue 15 2001
    Peter M. Wohlgemuth
    Abstract Wildfire usually promotes flooding and accelerated erosion in upland watersheds. In the summer of 1999, a high-severity wildfire burned a series of mixed pine/oak headwater catchments in the San Jacinto Mountains of southern California. Log erosion barriers (LEBs) were constructed across much of the burned area as an erosion control measure. We built debris basins in two watersheds, each about 1 ha in area, one with LEBs, the other without, to measure post-fire hydrologic response and sediment yield and to evaluate the effectiveness of the LEBs. The watersheds are underlain by granitic bedrock, producing a loamy sand soil above large extents of weathered bedrock and exposed core stones (tors) on the surface. Measured soil water-repellency was similar over the two catchments. Rain gauges measured 348 mm of precipitation in the first post-fire year. The ephemeral stream channels experienced surface flow after major rainstorms, and the source of the water was throughflow exfiltration at the slope/channel interface. Post-fire overland flow produced some rilling, but hillslope erosion measured in silt fences away from any LEBs was minor, as was sediment accumulation behind the LEBs. Stream channels in the catchments exhibited minor net scour. Water yield was much greater in the LEB-treated watershed. This resulted in 14 times more sediment yield by weight than the untreated watershed. Average soil depths determined by augering were nearly double in the catchment without the LEBs compared with the treated watershed. This suggests that differences in water and sediment yield between the two catchments are due to the twofold difference in the estimated soil water-holding capacity in the untreated watershed. It appears that the deeper soils in the untreated watershed were able to retain most of the precipitation, releasing less water to the channels and thereby reducing erosion and sediment yield. Thus, the test of LEB effectiveness was inconclusive in this study, because soil depth and soil water-holding capacity may have masked their performance. Published in 2001 John Wiley & Sons, Ltd. [source]

    Effects of soil bulk density on seminal and lateral roots of young maize plants (Zea mays L.)

    JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 2 2004
    Rolf O. Kuchenbuch
    Abstract It is well established that increasing soil bulk density (SBD) above some threshold value reduces plant root growth and thus may reduce water and nutrient acquisition. However, formation and elongation of maize seminal roots and first order lateral (FOL) roots in various soil layers under the influence of SBD has not been documented. Two studies were conducted on a loamy sand soil at SBD ranging from 1.25 g,cm,3 to 1.66 g,cm,3. Rhizotrons with a soil layer 7 mm thick were used and pre-germinated plants were grown for 15 days. Over the range of SBD tested, the shoot growth was not influenced whereas total root length was reduced by 30,% with increasing SBD. Absolute growth rate of seminal roots was highest in the top soil layer and decreased with increasing distance from the surface. Increasing SBD amplified this effect by 20,% and 50,% for the top soil layer and lower soil layers, respectively. At the end of the experiment, total seminal roots attributed to approximately 15,% of the total plant root length. Increasing SBD reduced seminal root growth in the lowest soil layer only, whereas FOL root length decreased with SBD in all but the uppermost soil layer. For FOL, there was a positive interaction of SBD with distance from the soil surface. Both, increasing SBD and soil depth reduced root length by a reduction of number of FOL roots formed while the length of individual FOL roots was not influenced. Hence, increasing SBD may reduce spatial access to nutrients and water by (i) reducing seminal root development in deeper soil layers, aggravated by (ii) the reduction of the number of FOL roots that originate from these seminal roots. Einfluss der Bodendichte auf Seminal- und Lateralwurzeln von jungen Maispflanzen (Zea mays L.) Es ist bekannt, dass zunehmende Bodendichte (SBD) oberhalb eines Grenzwertes das Wurzelwachstum von Pflanzen und die Wasser- und Nährstoffaufnahme reduziert. Bildung und Wachstum der Seminal- und der Lateralwurzeln erster Ordnung (FOL) von Mais in Bodenschichten verschiedenen Abstands von der Bodenoberfläche unter dem Einfluss verschiedener Bodendichten wurde bisher nicht beschrieben. Zwei unabhängige Versuche wurden mit einem lehmigen Sandboden durchgeführt. Vorgekeimte Maiskörner wurden in Rhizotrone mit einer etwa 7,mm dicken Bodenschicht eingesetzt, die Bodendichten lagen im Mittel der Rhizotrone zwischen 1,25 g,cm,3 und 1,66 g,cm,3. Die Versuchsdauer betrug 15 Tage. Über den Bereich der geprüften SBD wurde das Sprosswachstum nicht beeinflusst, während die Gesamtwurzellänge mit zunehmender SBD um bis zu 30,% abnahm. Die absolute Wachstumsrate der Seminalwurzeln war in der obersten Bodenschicht am höchsten und nahm mit zunehmendem Abstand von der Bodenoberfläche ab. Seminalwurzeln trugen zu ca. 15,% zur Gesamtwurzellänge bei. Zunehmende SBD reduzierte das Wachstum der Seminalwurzeln nur in der untersten Bodenschicht. Demgegenüber wurden die Längen der FOL in allen außer der obersten Schicht bei zunehmender SBD verringert. Bei den FOL wurde eine positive Interaktion zwischen SBD und Abstand von der Bodenoberfläche festgestellt. Sowohl zunehmende SBD als auch zunehmende Tiefe reduzierte die Wurzellänge durch eine Verringerung der Anzahl an FOL, während deren Länge nicht beeinflusst wurde. Folglich kann zunehmende SBD die räumliche Zugänglichkeit zu Wasser und Nährstoffen für die Pflanzen dadurch beeinflussen, dass (i) die Entwicklung von Seminalwurzeln in tieferen Bodenschichten reduziert wird und dass dieser Effekt verstärkt wird durch (ii) die verringerte Bildung von FOL an Seminalwurzeln. [source]

    Preparation, swelling behaviors and application of polyacrylamide/attapulgite superabsorbent composites

    POLYMERS FOR ADVANCED TECHNOLOGIES, Issue 1 2006
    Junping Zhang
    Abstract A series of superabsorbent composites, polyacrylamide/attapulgite (PAMA), were prepared from acrylamide (AM) and attapulgite micropowder in aqueous solution, using N,N,-methylenebisacrylamide (MBA) as a crosslinker and ammonium persulfate (APS) as an initiator and then saponified with sodium hydroxide solution. This paper focuses on swelling behaviors of the PAMA superabsorbent composites in various saline solutions. The results indicate that saline solutions can weaken the swelling abilities of the PAMA compsites greatly. Water absorbency of the PAMA composites with 20 and 40,wt% attapulgite in aqueous chloride salt solutions has the following order: Li+,=,Na+,=,K+, Mg2+,>,Ca2+,=,Ba2+ all through the range of concentration investigated. However, swelling properties of the composites are complicated in CuCl2(aq), AlCl3(aq) and FeCl3(aq) solutions and are related to saline solutions concentration. The deswelling behavior of PAMA composites is more obvious in univalent chloride salt solutions than in divalent and trivalent ones. The influence of kind and valence of anions on swelling ability of the composites is limited and almost the same. Moreover, reswelling capability, practical water retention ability in sand soil of the composites and the effect of pH on water absorbency of the PAMA composites were investigated. The PAMA composite shows good water retention and reswelling ability in sand soil, and may be used as a recyclable water-managing material for the renewal of arid and desert environment. Copyright © 2006 John Wiley & Sons, Ltd. [source]

    An epidemiological study of risk factors associated with the recurrence of equine grass sickness (dysautonomia) on previously affected premises

    EQUINE VETERINARY JOURNAL, Issue 2 2004
    J. R. Newton
    Summary Reasons for performing study: The reasons why equine grass sickness (EGS) recurs on premises are unknown and, consequently, practical methods for reducing the risk of recurrence are not available. Objectives: To identify risk factors associated with recurrence of EGS on premises and to gain possible insights into the pathogenesis of the disease. Methods: Data on disease history and risk factors were collected by postal questionnaire from premises with EGS cases between 1st January 1997 and 31st December 2001. Data on variation in rates of recurrence of EGS for different risk factors were analysed using Poisson regression analysis. Results: Of 509 premises contacted, 305 (60%) returned useable questionnaires and 100 of these (33%) were classified as ,recurrent' premises. An overall median incidence rate for EGS of 2.1 EGS incidents/100 horses/premises/year was recorded. There was an increased rate of recurrence with higher numbers of horses, presence of younger animals, stud farms and livery/riding establishments, loam and sand soils, rearing of domestic birds and mechanical droppings removal. The rate of recurrence decreased with chalk soil, cograzing ruminants, grass cutting on pastures and removal of droppings by hand. Several statistically significant interactions were identified. Conclusions: Many of the findings are consistent with the theory that EGS is a toxico-infectious form of botulism. Several of the significant factors identified may directly or indirectly relate to soil disturbance and consequent soil contamination of grass, thereby increasing the rate of exposure of grazing horses to Clostridium botulinum, which resides in soil. Potential relevance: Identification of potentially modifiable risk factors may, ideally following validation in appropriately designed, controlled and randomised intervention studies, lead to practical measures to reduce the incidence of EGS on previously affected premises. [source]

    Comparing the Feasibilities of Pearlmillet-Based Intercropping Systems Supplied with Varying Levels of Nitrogen and Phosphorus

    JOURNAL OF AGRONOMY AND CROP SCIENCE, Issue 2 2001
    O. P. Sharma
    To compare the feasibilities of pearlmillet-based intercropping systems, field experiments were carried out for 2 years on loamy sand soils in the semi-arid plain zone of Rajasthan, India. Results showed that the pooled yields of pearlmillet from the single crop (1525 kg ha,1) and from the crop intercropped with legumes (1528, 1498 or 1540 kg ha,1) were statistically the same. The yields from intercrop legumes were obtained as a bonus. The highest value of land equivalent ratio (1.21) was recorded for the pearlmillet + clusterbean system, which gave significantly better results than the pearlmillet + cowpea system. It was also found that the dose of nitrogen can be reduced by up to 25 % when pearlmillet is grown with legumes. However, intercrop legumes required the recommended dose of fertilizer to produce their optimal yields. The practice of intercropping without fertilizer proved disadvantageous. Ein Vergleich der Eignung eines auf Perlhirse basierenden Mischanbausystems mit unter- schiedlichen Stickstoff- und Phosphorsäuremengen Um die Eignung der Perlhirse auf der Basis eines Mischanbausystems zu überprüfen, wurden Feldexperimente für zwei Jahre auf einem lehmigen Sandboden in der semiariden Ebene von Rajastan, Indien durchgeführt. Die Ergebnisse zeigten, dass der Gesamtertrag von Perlhirse in einem Reinanbau (1525 kg ha,1) und in einem Mischanbau mit Leguminosen (1528, 1498 bzw. 1540 kg ha,1) statistisch gleich war. Die Erträge der Leguminosen im Mischanbau waren ein zusätzlicher Gewinn. Die höchsten Werte von LER (1,21) wurden im Mischanbau von Perlhirse + Klusterbohnenanbau nachgewiesen, wobei eine signifikante Überlegenheit gegenüber Perlhirse + Kuhbohnenanbausystemen nachzuweisen war. Die Ergebnisse weisen ferner darauf hin, dass bei der Stickstoffanwendung bis zu 25 % eingespart werden können, wenn Perlhirsen zusammen mit Leguminosen angebaut werden. Allerdings, der Mischanbau mit Leguminosen erfordert eine zu empfehlende Anwendungsmenge von Dünger, um optimale Erträge zu produzieren. Die Praxis des Mischanbaus ohne zusätzliche Düngung erwies sich als ungünstig. [source]

    Tree Community Change across 700 km of Lowland Amazonian Forest from the Andean Foothills to Brazil

    BIOTROPICA, Issue 5 2008
    Nigel C. A. Pitman
    ABSTRACT We describe patterns of tree community change along a 700-km transect through terra firme forests of western Amazonia, running from the base of the Andes in Ecuador to the Peru,Brazil border. Our primary question is whether floristic variation at large scales arises from many gradual changes or a few abrupt ones. Data from 54 1-ha tree plots along the transect support the latter model, showing two sharp discontinuities in community structure at the genus level. One is located near the Ecuador,Peru border, where the suite of species that dominates large areas of Ecuadorean forest declines abruptly in importance to the east. This discontinuity is underlain by a subterranean paleoarch and congruent with a change in soil texture. A second discontinuity is associated with the shift from clay to white sand soils near Iquitos. We hypothesize that the first discontinuity is part of an edaphic boundary that runs along the Andean piedmont and causes a transition from tree communities preferring richer, younger soils near the base of the Andes to those preferring poorer, older soils farther east. Because the floristic changes observed at this discontinuity are conserved for large distances to the east and west of it, the discontinuity is potentially key for understanding floristic variation in western Amazonia. The significant floristic turnover at the Ecuador,Peru border suggests that the only large protected area in the region,Ecuador's Yasuní National Park,is not adequate protection for the very diverse tree communities that cover vast areas of northern Peru. RESUMEN Describimos cambios en la comunidad de árboles a lo largo de un transecto de 700 km que atraviesa los bosques de tierra firme de la Amazonía occidental, desde la base de los Andes en Ecuador hasta la frontera Perú-Brasil. Nuestra pregunta principal es si la variación florística a grandes escalas es generada a base de muchos cambios graduales o en unos pocos cambios abruptos. Datos de 54 parcelas de árboles de 1 ha a lo largo del transecto apoyan el segundo modelo, mostrando dos discontinuidades bien definidas en la estructura de la comunidad a nivel de género. Una discontinuidad está localizada cerca de la frontera Ecuador-Perú, donde el grupo de especies que domina grandes áreas de la Amazonía ecuatoriana declina abruptamente en importancia hacia el este. Esta discontinuidad está asociada con un paleoarco subterráneo y es congruente con cambios en la textura del suelo. Una segunda discontinuidad está asociada con un cambio de suelos arcillosos a suelos de arena blanca cerca de Iquitos. Sugerimos que la primera discontinuidad es parte de un limite edáfico que corre a lo largo del piedemonte andino y causa una transición de comunidades de árboles que prefieren suelos más fértiles y jóvenes cerca de los Andes, a aquellos que prefieren suelos más pobres y antiguos hacia el este. Ya que los cambios florísticos observados en esta discontinuidad se conservan por grandes distancias hacia el este y oeste, la discontinuidad es potencialmente clave para entender la variación florística en la Amazonía occidental. El importante recambio florístico en la frontera Ecuador-Perú sugiere que la única gran área protegida en la región,el Parque Nacional Yasuní en Ecuador,no presta protección adecuada a las muy diversas comunidades de árboles en el norte del Perú. [source]