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Soil Bulk Density (soil + bulk_density)
Selected AbstractsPredicting Root Density in Streambanks,JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, Issue 2 2008Candice Piercy Abstract:, Roots of riparian vegetation increase streambank erosion resistance and structural stability; therefore, knowledge of root density and distribution in streambanks is useful for stream management and restoration. The objective of this study was to compare streambank root distributions for herbaceous and woody vegetation and to develop empirical models to predict root density. Root length density, root volume ratio, soil physical and chemical properties, and above-ground vegetation densities were measured at 25 sites on six streams in southwestern Virginia. The Mann-Whitney test was used to determine differences in root density along stream segments dominated by either woody or herbaceous vegetation. Multiple linear regression was used to develop relationships between root density and site characteristics. Study results showed that roots were evenly distributed across the bank face with the majority of roots having diameters less than 2 mm. Soil bulk density and above-ground vegetation were key factors influencing root density. While significant relationships were developed to predict root density, the predictive capabilities of the equations was low. Because of the highly variable nature of soil and vegetation properties, it is recommended at this time that soil erodibility and root density be measured in the field for design and modeling purposes, rather than estimated based on empirical relationships. [source] Managing precipitation use in sustainable dryland agroecosystemsANNALS OF APPLIED BIOLOGY, Issue 2 2004GARY A PETERSON Summary In the Great Plains of North America potential evaporation exceeds precipitation during most months of the year. About 75% of the annual precipitation is received from April through September, and is accompanied by high temperatures and low relative humidity. Dryland agriculture in the Great Plains has depended on wheat production in a wheat-fallow agroecosystem (one crop year followed by a fallow year). Historically this system has used mechanical weed control practices during the fallow period, which leaves essentially no crop residue cover for protection against soil erosion and greatly accelerates soil organic carbon oxidation. This paper reviews the progress made in precipitation management in the North American Great Plains and synthesises data from an existing long-term experiment to demonstrate the management principles involved. The long-term experiment was established in 1985 to identify dryland crop and soil management systems that would maximize precipitation use efficiency (maximization of biomass production per unit of precipitation received), improve soil productivity, and increase economic return to the farmers in the West Central portion of the Great Plains. Embedded within the primary objective are sub-objectives that focus on reducing the amount of summer fallow time and reversing the soil degradation that has occurred in the wheat-fallow cropping system. The experiment consists of four variables: 1) Climate regime; 2) Soils; 3) Management systems; and 4) Time. The climate variable is based on three levels of potential evapotranspiration (ET), which are represented by three sites in eastern Colorado. All sites have annual long-term precipitation averages of approximately 400,450 mm, but vary in growing season open pan evaporation from 1600 mm in the north to 1975 mm in the south. The soil variable is represented by a catenary sequence of soils at each site. Management systems, the third variable, differ in the amount of summer fallow time and emphasize increased crop diversity. All systems are managed with no-till techniques. The fourth variable is time, and the results presented in this paper are for the first 12 yr (3 cycles of the 4-yr system). Comparing yields of cropping systems that differ in cycle length and systems that contain fallow periods, when no crop is produced, is done with a technique called "annualisation". Yields are "annualised" by summing yields for all crops in the system and dividing by the total number of years in the system cycle. For example in a wheat-fallow system the wheat yield is divided by two because it takes 2 yr to produce one crop. Cropping system intensification increased annualised grain and crop residue yields by 75 to 100% compared to wheat-fallow. Net return to farmers increased by 25% to 45% compared to wheat-fallow. Intensified cropping systems increased soil organic C content by 875 and 1400 kg ha,1, respectively, after 12 yr compared to the wheat-fallow system. All cropping system effects were independent of climate and soil gradients, meaning that the potential for C sequestration exists in all combinations of climates and soils. Soil C gains were directly correlated to the amount of crop residue C returned to the soil. Improved macroaggregation was also associated with increases in the C content of the aggregates. Soil bulk density was reduced by 0.01g cm,3 for each 1000 kg ha,1 of residue addition over the 12-yr period, and each 1000 kg ha,1 of residue addition increased effective porosity by 0.3%. No-till practices have made it possible to increase cropping intensification beyond the traditional wheat-fallow system and in turn water-use efficiency has increased by 30% in West Central Great Plains agroecosystems. Cropping intensification has also provided positive feedbacks to soil productivity via the increased amounts of crop residue being returned to the soil. [source] Soil organic carbon contents in long-term experimental grassland plots in the UK (Palace Leas and Park Grass) have not changed consistently in recent decadesGLOBAL CHANGE BIOLOGY, Issue 7 2009D. W. HOPKINS Abstract A recent report of widespread declines in soil organic C (SOC) in the UK over the 10,25 years until the early 2000s has focussed attention on the importance of resampling previously characterized sites to assess long-term trends in SOC contents and the importance of soils as a potentially volatile and globally significant reservoir of terrestrial C. We have used two sets of long-term experimental plots which have been under constant and known management for over a century and for which historical data exist that allow comparison over recent decades to determine what, if any, changes in SOC content have occurred. The plots used are the Palace Leas (PL) Meadow Hay Plots in north-east England (UK) established in 1897, and from the Park Grass (PG) Continuous Hay experiment established in 1856 at Rothamsted in south-east England. Collectively, these plots represent the only grassland sites in the UK under long-term management where changes in SOC over several decades can be assessed, and are probably unique in the world. The plots have received different manure and fertilizer treatment and have been under known management for at least 100 years. In 1982, total SOC contents were determined for the 0,27 cm layer of six of the PL plots using measurements of SOC concentrations, bulk density and soil depth. In 2006, the same six PL plots were resampled and SOC contents determined again. Four of the plots showed no net change in SOC content, but two plots showed net loss of SOC of 15% and 17% (amounting to decreases of 18 and 15 t C ha,1) since 1982. However, these differences in total SOC content were in a similar range to the variations in bulk density (6,31%) with changing soil water content. In 1959, the soil masses and SOC concentrations to 23 cm depth were measured on six PG plots with fertilizer and manure treatments corresponding closely with those measured on PL. In 2002, the SOC concentrations on the same plots were measured again. On three of the PG plots, SOC concentrations had declined by 2,10%, but in the other three it had increased by 4,8% between 1959 and 2002. If it is assumed that the soil bulk density had not changed over this period, the losses of SOC from the top soils ranged range from 10 to 3 t C ha,1, while the gains ranged from 4 to 7 t C ha,1. When the differences with time in SOC contents for the six PL and the six PG plots were examined using paired t -tests, that is, regarding the plots as two sets of six replicate permanent grasslands, there were no significant differences between 1982 and 2006 for the PL plots or between 1959 and 2002 for the PG plots. Thus, these independent observations on similar plots at PL and PG indicate there has been no consistent decrease in SOC stocks in surface soils under old, permanent grassland in England in recent decades, even though meteorological records for both sites indicate significant warming of the soil and air between 1980 and 2000. Because the potential influences of changes in management or land use have been definitively excluded, and measured rather than derived bulk densities have been used to convert from SOC concentrations to SOC amounts, our observations question whether for permanent grassland in England, losses in SOC in recent decades reported elsewhere can be attributed to widespread environmental change. [source] Saline Drainage Water, Irrigation Frequency and Crop Species Effects on Some Physical Properties of SoilsJOURNAL OF AGRONOMY AND CROP SCIENCE, Issue 1 2001Y. A. Al-Nabulsi This field study evaluated the effects of water quality, irrigation frequency and crop species on some physical properties of soils. The experiment had a split-split-plot design, with three irrigation water qualities (normal water, drainage water and a 1 : 1 mixture of freshwater and drainage water) as the main treatments, two irrigation frequencies (at 7- and 14-day intervals) as the subtreatments and two crops (barley and alfalfa) as the subsubtreatments. The soil infiltration rate was highest in the barley plot receiving freshwater irrigation at weekly intervals. The lowest soil infiltration rate was found in alfalfa plots receiving saline irrigation water at 14-day intervals. Bulk density and proportions of micropores [pore radius (r) < 1.4 µm] were higher and the proportion of macropores (r > 14.4 µm) was lower in barley than in alfalfa. Saline irrigation caused the greatest decrease in total porosity. The soil infiltration rate was higher with more frequent irrigation, and was highest in alfalfa plots receiving freshwater irrigation. The decrease in soil bulk density and infiltration rate was greater with saline drainage water, irrespective of the crop grown and the irrigation frequency. Salzhaltiges Drainagewasser, Bewässerungshäufig-keit und Kulturpflanzenarten mit Wirkung auf einige physikalische Eigenschaften des Bodens Eine Felduntersuchung wurde vorgenommen, um dem Einfluss der Wasserqualität, der Bewässerungshäufigkeit und Kulturpflanzenarten auf einige physikalische Eigenschaften von Böden zu untersuchen. Die Infiltrationrate mit Frischwasser in wöchentlichen Abständen unter Gerste war hoch. Eine Behandlung mit Salzwasser in 14 tägigen Abständen unter Luzerne zeigte eine geringere Infiltrationsrate des Bodens. Bodendichte und der Anteil der Mikroporen (Poren mit einem Radius von r < 1,4 mm) waren größer und der Anteil der Makroporen (r > 14,4 mm) war unter Gerste geringer. Bewässerung mit Salzwasser verursachte die stärkste Abnahme in der Gesamtporosität. Die Infiltrationsrate des Bodens nahm mit der Häufigkeit der Bewässerung zu und zeigte den höchsten Wert bei Luzerne und einer Frischwasserbewässerung. Die Abnahme in der Bodendichte und der Infiltrationseigenschaften waren bei Salzwasserdrainage unabhängig von der Kulturpflanzenart und der Bewässerungshäufigkeit höher. [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 2004Rolf 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] Estimating water retention curves of forest soils from soil texture and bulk densityJOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 1 2003Robert Teepe Abstract Forest soils differ significantly from the arable land in their distribution of the soil bulk density and humus content, but the water retention parameters are primarily derived from the data of agricultural soils. Thus, there is a need to relate physical parameters of forest soils with their water retention characteristics and compare them with those of agricultural soils. Using 1850 water retention curves from forest soils, we related the following soil physical parameters to soil texture, bulk density, and C content: air capacity (AC), available water capacity (AWC), and the permanent wilting point (PWP). The ACs of forest soils were significantly higher than those of agricultural soils which were related to the low bulk densities of the forest soils, whereas differences in AWCs were small. Therefore, for a proper evaluation of the water retention curves (WRCs) and the parameters derived from them, further subdivisions of the lowest (< 1.45 g cm -3) of the three bulk density classes was undertaken to the wide range of low soil densities in forest soils (giving a total of 5 bulk density classes). In Germany, 31 soil texture classes are used for the estimation of soil physical parameters. Such a detailed classification is not required because of insignificant differences in WRCs for a large number of these classes. Based on cluster analysis of AC, AWC, and PWP parameters, 10 texture collectives were obtained. Using 5 classes of bulk densities, we further calculated the ACs, AWCs, and the PWPs for these 10 classes. Furthermore, "van Genuchten parameters" (, r, , s, ,, and n) were derived which described the average WRC for each designated class. In a second approach using multiple regression analysis, regression functions for AC, AWC, and PWP and for the van Genuchten parameter were calculated. Abschätzung der Wasser-Retentionskurven von Waldböden anhand der Bodenart und Bodendichte Obwohl sich Waldböden in der Verteilung der Bodendichte und Humusgehalte deutlich von Ackerböden unterscheiden, basiert die Ableitung ihrer bodenphysikalischen Kenngrößen in der Kartieranleitung auf Erhebungen landwirtschaftlich genutzter Böden. Die Abschätzung physikalischer Eigenschaften von Waldböden ist daher weiterhin als unzureichend anzusehen. In dieser Arbeit wurde auf Grundlage von 1850 an Waldböden ermittelten Wasser-Retentionskurven die Luftkapazität, die nutzbare Wasserspeicherkapazität und der Wassergehalt am permanenten Welkepunkt aus der Bodenart, der Bodendichte und dem C-Gehalt hergeleitet. Im Vergleich zu Ackerböden lagen die berechneten Luftkapazitäten aufgrund der unterschiedlichen vertikalen Verteilung der Bodendichten und Humusgehalte von Wald- und Ackerböden in Waldböden deutlich höher, Unterschiede in der nutzbaren Wasserspeicherkapazität hingegen waren gering. Die Ergebnisse zeigen, dass für Waldböden eine differenziertere Unterteilung der Dichteklassen notwendig ist, um die große Streuung im Bereich der unteren Bodendichte adäquat zu berücksichtigen. Andererseits basiert in Deutschland die Abschätzung physikalischer Bodeneigenschaften auf einer detaillierten Einteilung von 31 Texturklassen (Kartieranleitung und Forstliche Standortaufnahme). Da die Unterschiede zwischen vielen Texturklassen häufig sehr gering und statistisch nicht zu trennen sind, wurde unser Datensatz mit Hilfe einer Clusteranalyse auf 10 Texturklassen reduziert. Für diese Texturklassen wurden, unterteilt in jeweils 5 Dichteklassen, die Luftkapazitäten, die nutzbaren Wasserspeicherkapazitäten und der permanente Welkepunkt sowie die van Genuchten Parameter , r, , s, ,, und n berechnet. In einem zweiten Ansatz wurde eine Abschätzung dieser Kenngrößen mit Hilfe der multiplen Regression vorgenommen. [source] | |||||||||||||