scholarly journals Pedotransfer functions to estimate retention and availability of water in soils of the state of Santa Catarina, Brazil

2013 ◽  
Vol 37 (4) ◽  
pp. 889-910 ◽  
Author(s):  
André da Costa ◽  
Jackson Adriano Albuquerque ◽  
Jaime Antônio de Almeida ◽  
Adriano da Costa ◽  
Rodrigo Vieira Luciano
Keyword(s):  
Organic Matter ◽  
Regression Analysis ◽  
Path Analysis ◽  
Water Retention ◽  
Organic Matter Content ◽  
Soil Surface ◽  
Matter Content ◽  
The State ◽  
Pedotransfer Functions ◽  
Santa Catarina

Studies on water retention and availability are scarce for subtropical or humid temperate climate regions of the southern hemisphere. The aims of this study were to evaluate the relations of the soil physical, chemical, and mineralogical properties with water retention and availability for the generation and validation of continuous point pedotransfer functions (PTFs) for soils of the State of Santa Catarina (SC) in the South of Brazil. Horizons of 44 profiles were sampled in areas under different cover crops and regions of SC, to determine: field capacity (FC, 10 kPa), permanent wilting point (PWP, 1,500 kPa), available water content (AW, by difference), saturated hydraulic conductivity, bulk density, aggregate stability, particle size distribution (seven classes), organic matter content, and particle density. Chemical and mineralogical properties were obtained from the literature. Spearman's rank correlation analysis and path analysis were used in the statistical analyses. The point PTFs for estimation of FC, PWP and AW were generated for the soil surface and subsurface through multiple regression analysis, followed by robust regression analysis, using two sets of predictive variables. Soils with finer texture and/or greater organic matter content retain more moisture, and organic matter is the property that mainly controls the water availability to plants in soil surface horizons. Path analysis was useful in understanding the relationships between soil properties for FC, PWP and AW. The predictive power of the generated PTFs to estimate FC and PWP was good for all horizons, while AW was best estimated by more complex models with better prediction for the surface horizons of soils in Santa Catarina.

scholarly journals Water retention and availability in soils of the State of Santa Catarina-Brazil: effect of textural classes, soil classes and lithology

2013 ◽  
Vol 37 (6) ◽  
pp. 1535-1548 ◽  
Author(s):  
André da Costa ◽  
Jackson Adriano Albuquerque ◽  
Adriano da Costa ◽  
Patricia Pértile ◽  
Franciani Rodrigues da Silva
Keyword(s):  
Organic Matter ◽  
Cover Crops ◽  
Water Availability ◽  
Water Retention ◽  
Mixed Model ◽  
Organic Matter Content ◽  
Matter Content ◽  
The State ◽  
Santa Catarina ◽  
Alluvial Deposits

The retention and availability of water in the soil vary according to the soil characteristics and determine plant growth. Thus, the aim of this study was to evaluate water retention and availability in the soils of the State of Santa Catarina, Brazil, according to the textural class, soil class and lithology. The surface and subsurface horizons of 44 profiles were sampled in different regions of the State and different cover crops to determine field capacity, permanent wilting point, available water content, particle size, and organic matter content. Water retention and availability between the horizons were compared in a mixed model, considering the textural classes, the soil classes and lithology as fixed factors and profiles as random factors. It may be concluded that water retention is greater in silty or clayey soils and that the organic matter content is higher, especially in Humic Cambisols, Nitisols and Ferralsol developed from igneous or sedimentary rocks. Water availability is greater in loam-textured soils, with high organic matter content, especially in soils of humic character. It is lower in the sandy texture class, especially in Arenosols formed from recent alluvial deposits or in gravelly soils derived from granite. The greater water availability in the surface horizons, with more organic matter than in the subsurface layers, illustrates the importance of organic matter for water retention and availability.

scholarly journals Relationship of soil properties to fractionation, bioavailability and mobility of lead and zinc in soil

2008 ◽  
Vol 53 (No. 5) ◽  
pp. 225-238 ◽  
Author(s):  
N. Finžgar ◽  
P. Tlustoš ◽  
D. Leštan
Keyword(s):  
Organic Matter ◽  
Regression Analysis ◽  
Soil Organic Matter ◽  
Soil Properties ◽  
Multiple Regression ◽  
Contaminated Soils ◽  
Organic Matter Content ◽  
Clay Content ◽  
Exchange Capacity ◽  
Matter Content

Sequential extractions, metal uptake by <i>Taraxacum officinale</i>, Ruby&rsquo;s physiologically based extraction test (PBET) and toxicity characteristic leaching procedure (TCLP), were used to assess the risk of Pb and Zn in contaminated soils, and to determine relationships among soil characteristics, heavy metals soil fractionation, bioavailability and leachability. Regression analysis using linear and 2nd order polynomial models indicated relationships between Pb and Zn contamination and soil properties, although of small significance (<i>P</i> < 0.05). Statistically highly significant correlations (<i>P</i> < 0.001) were obtained using multiple regression analysis. A correlation between soil cation exchange capacity (CEC) and soil organic matter and clay content was expected. The proportion of Pb in the PBET intestinal phase correlated with total soil Pb and Pb bound to soil oxides and the organic matter fraction. The leachable Pb, extracted with TCLP, correlated with the Pb bound to carbonates and soil organic matter content (<i>R</i><sup>2</sup> = 69%). No highly significant correlations (<i>P</i> < 0.001) for Zn with soil properties or Zn fractionation were obtained using multiple regression.

Adsorption and Efficacy of Trifluralin and Butralin as Influenced by Soil Properties

Weed Science ◽  
1985 ◽  
Vol 33 (6) ◽  
pp. 861-867 ◽  
Author(s):  
C. John Peter ◽  
Jerome B. Weber
Keyword(s):  
Organic Matter ◽  
Weed Control ◽  
Organic Matter Content ◽  
Soil Surface ◽  
Matter Content ◽  
Soil Adsorption ◽  
Glycol Monoethyl Ether ◽  
Chamber Studies ◽  
Highly Correlated ◽  
Growth Chamber Studies

Significantly higher rates of butralin [4-(1,1-dimethylethyl)-N-(1-methylpropyl)-2,6-dinitrobenzenamine] were required to produce the same level of weed control as trifluralin [2,6-dinitro -N,N-dipropyl-4-(trifluoromethyl) benzenamine] when applied to soybeans [Glycine max(L.) Merr.] on seven different soils in the field. Higher rates of butralin were also required to control barnyardgrass [Echinochloa crus-galli(L.) Beauv. ♯ ECHCG] in growth chamber studies. No differences in the extent of soil adsorption of trifluralin and butralin were apparent; therefore, differences in efficacy could not be attributed to differences in soil adsorption. Herbicide rates required for 80% weed control and Freundlich K-values (adsorption capacity indices) were mostly highly correlated with soil organic-matter content and soil surface area as measured by benzyl ethyl ether (BEE) and ethylene glycol monoethyl ether (EGME) on nine soils. Analysis of the organic-matter content of the nine soils by 10 soil testing laboratories resulted in highly significant differences among laboratories.

Use of Adsorption Coefficients and Soil Properties to Predict Fluridone Herbicidal Activity

Weed Science ◽  
1979 ◽  
Vol 27 (4) ◽  
pp. 456-459 ◽  
Author(s):  
A. Loh ◽  
S. J. Parka ◽  
R. Albritton ◽  
C. C. Lin
Keyword(s):  
Organic Matter ◽  
Regression Analysis ◽  
Stepwise Regression ◽  
Organic Matter Content ◽  
Grain Sorghum ◽  
Matter Content ◽  
Herbicidal Activity ◽  
Sorghum Vulgare ◽  
Soil Adsorption ◽  
Linear Correlation Analysis

The rate of herbicide required to reduce growth of grain sorghum (Sorghum vulgare, Per. ‘Pioneer 8417′) by 50% (GR50) and soil adsorption coefficients (Ka) were determined for the experimental herbicide, fluridone {1-methyl-3-phenyl-5-[3-(trifluoromethyl)phenyl]-4(1H)-pyridinone}, in 14 soils. A linear correlation analysis was conducted between GR50values and the chemical and physical properties and fluridone absorption coefficient (Ka) for 14 soils. The GR50values were significantly correlated to soil organic matter and Ka. A stepwise regression analysis suggests that Kaor organic matter content can be used to predict the rate of fluridone application required for herbicidal activity.

COMPACTION AND SETTLING OF QUEBEC SOILS IN RELATION TO THEIR SOIL-WATER PROPERTIES

1982 ◽  
Vol 62 (1) ◽  
pp. 165-175 ◽  
Author(s):  
C. R. DE KIMPE ◽  
M. BERNIER-CARDOU ◽  
P. JOLICOEUR
Keyword(s):  
Organic Matter ◽  
Water Retention ◽  
Sandy Loam ◽  
Organic Matter Content ◽  
Matter Content ◽  
Soil Behavior ◽  
Matric Potential ◽  
Moisture Contents ◽  
Water Retention Properties ◽  
Soil Water Properties

Twenty-one topsoils, with texture varying from sandy loam to clay and organic matter content ranging from 1.6 to 11.9%, were submitted to compaction and settling at different moisture contents where dry bulk density was determined. Under compaction, the density curve went through a maximum while a minimum was observed in the case of settling. Optimum moisture contents corresponding to these two characteristic densities were almost the same. The most important physical properties affecting soil behavior under compaction and settling were found to be water retention properties at low matric potential which themselves depended primarily on organic matter content. Samples submitted to compaction had saturated hydraulic conductivities less than 1 cm/h, while after settling, Ksat measurements ranged from 0.8 to 234 cm/h. Organic matter played an important role in reducing the effects of compaction, and moisture content alone was not sufficient to predict the best conditions for workability in the fields.

Plastic limits of agricultural soils as functions of soil texture and organic matter content

Soil Research ◽  
2012 ◽  
Vol 50 (1) ◽  
pp. 7 ◽  
Author(s):  
Thomas Keller ◽  
Anthony R. Dexter
Keyword(s):  
Organic Matter ◽  
Soil Texture ◽  
Agricultural Soils ◽  
Organic Matter Content ◽  
Clay Content ◽  
Liquid Limit ◽  
Matter Content ◽  
Pedotransfer Functions ◽  
Strongly Correlated ◽  
Yield Information

The plastic limits (lower plastic limit, PL; and liquid limit, LL) are important soil properties that can yield information on soil mechanical behaviour. The objective of this paper is to study the plastic limits of agricultural soils as functions of soil texture and organic matter (OM) content. The plastic limits were highly related to the clay content. The LL was more strongly correlated with clay than was PL, but the reasons are unclear. Interestingly, PL was virtually unaffected by clay content for soils with clay contents below ~35%. The OM had a strong effect on the plastic limits. This effect was clearly demonstrated when analysing soils of similar texture with a range of OM. We present equations (pedotransfer functions) for estimation of PL, LL, and plasticity index (PI) from soil texture and OM. Finally, we predict that the clay content must be ≥10% for soils without OM to be plastic; however, soils with <10% clay can be plastic if OM is present. More research is needed to investigate OM effects on soil consistency.

EFFET DU MODELAGE DES CHAMPS SUR L’HETEROGENEITE DES SOLS ET LES RENDEMENTS EN MAIS-GRAIN

1981 ◽  
Vol 61 (2) ◽  
pp. 225-236 ◽  
Author(s):  
C. R. DE KIMPE ◽  
M. R. LAVERDIERE ◽  
J. ZIZKA
Keyword(s):  
Organic Matter ◽  
Physical Properties ◽  
Bulk Density ◽  
Water Retention ◽  
Organic Matter Content ◽  
Matter Content ◽  
The Real ◽  
Standard Deviations ◽  
Similar Texture ◽  
Real Density

Rounding of the lands in a field involves changes in the surface horizons. The thickness of Ap horizons at various sites in corn fields varied from 15 to 41 cm. In these horizons, the organic matter content that ranged between 10 and 250 t/ha influenced the real density of the particles, the bulk density of soils with similar texture, and also the shape of the water retention curves at tensions from 0 to 1.5 MPa. Maximum available water in the Ap horizons between 33.3 kPa and 1.5 MPa varied from 0.5 to 4 cm H2O. Yield differences reached 74% while the standard deviations were generally lower than 15%. Higher yields were observed at higher, intermediate and lower sites of the fields. The differences in the yield were not entirely accounted for by the variations in the chemical and physical properties of the soils.

scholarly journals EFFECT OF DITHIOPYR, SEED PLACEMENT. AND SOIL ORGANIC MATTER CONTENT ON GROWTH OF TOLERANT AND SUSCEPTIBLE WEEDS

HortScience ◽  
1992 ◽  
Vol 27 (6) ◽  
pp. 587f-587
Author(s):  
Nanik Setyowati ◽  
Leslie A. Weston
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Soil Surface ◽  
Matter Content ◽  
Peat Moss ◽  
Silt Loam ◽  
Soil Organic Matter Content ◽  
Silt Loam Soil ◽  
Seed Placement ◽  
Loam Soil

Dithiopyr (Dimension, Monsanto) is a turfgrass herbicide currently under evaluation for use in ornamentals. Granular herbicide depth and seed placement were evaluated in greenhouse studies with tolerant or susceptible weeds. Dithiopyr was applied preemergence to weeds at the rate of 2.24 kg/ha to Maury silt loam soil. Weed seeds were planted routinely at 0.64 cm depth. Dithiopyr placed at the soil surface or 0.64 cm in depth caused the greatest injury to seedlings, followed by dithiopyr at 1.28 cm depth. Dithiopyr at 2.54 and 3.81 cm below the surface had no effect upon seedling growth. When seeding depth was investigated, seed placed at 0.64, 1.28 or 1.91 cm below the surface showed greatest seedling injury when dithiopyr was routinely applied at 0.64 cm depth. Seed placement on the soil surface resulted in the least injury to weeds. Peat moss was added to Maury silt loam soil and to sand to investigate the influence of organic matter upon activity. Soil with 2% peat resulted in the least injury to selected weed seedlings while sand, and sand plus up to 3% peat showed greatest injury. Sand amended with 5 and 6% peat also resulted in less injury to weed seedlings. Ivy leaf morningglory and KY 31 fescue were most tolerant of dithiopyr while barnyardgrass and large crabgrass were most sensitive. Dithiopyr uptake, translocation and metabolism studies will be conducted with susceptible and tolerant weed and woody ornamental species.

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