Abstract:X. M. 2015. Temporal effects of food waste compost on soil physical quality and productivity. Can. J. Soil Sci. 95: 251Á268. The benefits of compost additions on soil organic carbon content and crop productivity are extant in the literature, but detailed studies of compost effects on soil physical quality (SPQ) are limited. The objective of this study was therefore to describe how one-time additions of compost impact the immediate, mid-term and long-term SPQ and crop yields of an agricultural soil. Food waste … Show more
“…Soil samples were collected from three long-term field experiments, including: i) an organic amendment study which received one-time applications (fall 1997) of household food waste compost (75 Mg ha −1 , 150 Mg ha −1 , 300 Mg ha −1 ), yard waste compost (75 Mg ha −1 ), and pig manure plus wheat straw compost (75 Mg ha −1 ) (see Yang et al 30. and Reynolds et al 31. for details); ii) a long-term fertilization and rotation experiment (initiated 1959) consisting of three cropping treatments (continuous corn, corn-oat-alfalfa-alfalfa rotation, continuous bluegrass sod) and two fertilizer treatments (fertilized, not fertilized) with each phase of the rotation present every year (see Drury et al 32.…”
Section: Methodsmentioning
confidence: 99%
“… 30 and Reynolds et al . 31 for details); ii) a long-term fertilization and rotation experiment (initiated 1959) consisting of three cropping treatments (continuous corn, corn-oat-alfalfa-alfalfa rotation, continuous bluegrass sod) and two fertilizer treatments (fertilized, not fertilized) with each phase of the rotation present every year (see Drury et al . 32 for details); and iii) a long-term tillage study (initiated in 1983 and modified in 1996) with corn under moldboard plow tillage, ridge tillage and no-tillage, plus continuous Kentucky bluegrass sod (see Yang et al .…”
We test the common assumption that organic carbon (OC) storage occurs on sand-sized soil particles only after the OC storage capacity on silt- and clay-sized particles is saturated. Soil samples from a Brookston clay loam in Southwestern Ontario were analysed for the OC concentrations in bulk soil, and on the clay (<2 μm), silt (2–53 μm) and sand (53–2000 μm) particle size fractions. The OC concentrations in bulk soil ranged from 4.7 to 70.8 g C kg−1 soil. The OC concentrations on all three particle size fractions were significantly related to the OC concentration of bulk soil. However, OC concentration increased slowly toward an apparent maximum on silt and clay, but this maximum was far greater than the maximum predicted by established C sequestration models. In addition, significant increases in OC associated with sand occurred when the bulk soil OC concentration exceeded 30 g C kg−1, but this increase occurred when the OC concentration on silt + clay was still far below the predicted storage capacity for silt and clay fractions. Since the OC concentrations in all fractions of Brookston clay loam soil continued to increase with increasing C (bulk soil OC content) input, we concluded that the concept of OC storage capacity requires further investigation.
“…Soil samples were collected from three long-term field experiments, including: i) an organic amendment study which received one-time applications (fall 1997) of household food waste compost (75 Mg ha −1 , 150 Mg ha −1 , 300 Mg ha −1 ), yard waste compost (75 Mg ha −1 ), and pig manure plus wheat straw compost (75 Mg ha −1 ) (see Yang et al 30. and Reynolds et al 31. for details); ii) a long-term fertilization and rotation experiment (initiated 1959) consisting of three cropping treatments (continuous corn, corn-oat-alfalfa-alfalfa rotation, continuous bluegrass sod) and two fertilizer treatments (fertilized, not fertilized) with each phase of the rotation present every year (see Drury et al 32.…”
Section: Methodsmentioning
confidence: 99%
“… 30 and Reynolds et al . 31 for details); ii) a long-term fertilization and rotation experiment (initiated 1959) consisting of three cropping treatments (continuous corn, corn-oat-alfalfa-alfalfa rotation, continuous bluegrass sod) and two fertilizer treatments (fertilized, not fertilized) with each phase of the rotation present every year (see Drury et al . 32 for details); and iii) a long-term tillage study (initiated in 1983 and modified in 1996) with corn under moldboard plow tillage, ridge tillage and no-tillage, plus continuous Kentucky bluegrass sod (see Yang et al .…”
We test the common assumption that organic carbon (OC) storage occurs on sand-sized soil particles only after the OC storage capacity on silt- and clay-sized particles is saturated. Soil samples from a Brookston clay loam in Southwestern Ontario were analysed for the OC concentrations in bulk soil, and on the clay (<2 μm), silt (2–53 μm) and sand (53–2000 μm) particle size fractions. The OC concentrations in bulk soil ranged from 4.7 to 70.8 g C kg−1 soil. The OC concentrations on all three particle size fractions were significantly related to the OC concentration of bulk soil. However, OC concentration increased slowly toward an apparent maximum on silt and clay, but this maximum was far greater than the maximum predicted by established C sequestration models. In addition, significant increases in OC associated with sand occurred when the bulk soil OC concentration exceeded 30 g C kg−1, but this increase occurred when the OC concentration on silt + clay was still far below the predicted storage capacity for silt and clay fractions. Since the OC concentrations in all fractions of Brookston clay loam soil continued to increase with increasing C (bulk soil OC content) input, we concluded that the concept of OC storage capacity requires further investigation.
“…Many investigations on SPQ were performed on agricultural soils because there is the need to establish what happens with different agronomic practices (e.g., Keller et al, 2007;Moebius et al, 2007;Reynolds et al, 2007;Fernández-Ugalde et al, 2009;Głąb et al, 2009;Chakraborty et al, 2010;Arthur et al, 2011;Bamberg et al, 2011;Li et al, 2011;Stavi and Lal, 2011;Iovino et al, 2016;Reynolds et al, 2014Reynolds et al, , 2015Baiamonte et al, 2015). Moreover, guidelines of practical interest have been developed with specific reference to these soils (e.g., Reynolds et al, 2009), and this circumstance has stimulated SPQ assessment in agricultural environments notwithstanding that optimal/critical values or ranges for SPQ indicators are still approximate (Reynolds et al, 2007) mainly because they are based on empirical observations that cannot cover all the possible situations.…”
Section: S Cullotta V Bagarello* G Baiamontementioning
Soil physical quality (SPQ) can be assessed by different experimental methodologies\ud
and criteria and the optimal/critical values or ranges for SPQ\ud
indicators are still approximate. Sampling soils with minimal anthropic pressures\ud
should allow improvements in SPQ assessment. Different experimental\ud
methodologies and criteria were applied to sample a Mediterranean oak forest\ud
(Quercus ilex L.) and pasture land, in Sicily, with a varying degree of\ud
anthropic disturbance. Soil water retention was determined in the laboratory\ud
and the field, using the BEST (Beerkan Estimation of Soil Transfer parameters)\ud
procedure of soil hydraulic characterization. Capacity-based indicators, the\ud
S index, and location and shape parameters of the pore volume distribution\ud
function were calculated for assessing SPQ. With the laboratory data,\ud
only the criterion using the capacity-based indicators suggested that SPQ\ud
increased as external pressures decreased. Therefore, this criterion appeared\ud
to be more reliable than the other tested criteria in the sampled environment.\ud
The field method was more prone to suggest good conditions and less able\ud
to signal differences between plots as compared with the laboratory method.\ud
A forest soil with a good SPQ has an ability to store and provide water to\ud
plant roots similar to, but it is more aerated than, a good agricultural soil.\ud
Developing BEST for SPQ assessment is advisable since parameters descriptive\ud
of the soil water transport properties can be collected with a single\ud
experiment. Simultaneous characterization of dendrometric and soil parameters\ud
at other sites is recommended to explore the relationships between SPQ\ud
indicators and characteristics of the forest cover
“…Mean annual air temperature and precipitation (45 year average) at the field site were 8.9˚C and 832 mm, respectively (Reynolds et al 2015). Average soil texture in the Ap horizon (0-20 cm) is 28 wt.…”
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