scholarly journals Effects of Soil Properties and Illumination Intensities on Matric Suction of Vegetated Soil

2019 ◽  
Vol 11 (22) ◽  
pp. 6475
Author(s):  
Qi Liu ◽  
Lijun Su ◽  
Zhenyao Xia ◽  
Daxiang Liu ◽  
Wennian Xu ◽  
...  
Keyword(s):  
Soil Properties ◽  
Sandy Loam ◽  
Matric Suction ◽  
Practical Significance ◽  
Soil Conditions ◽  
Silty Clay ◽  
Research Attention ◽  
Plant Transpiration ◽  
Fine Sandy Loam ◽  
Sandy Silt

Matric suction induced by evapotranspiration is an important parameter for determining the hydraulic mechanisms of vegetation on slope stability. Despite evapotranspiration closely associated with atmospheric parameters and soil conditions, the influence of soil properties and illumination intensities on matric suction of vegetated soil has so far received the least research attention. In this paper, three kinds of soil, namely, fine sandy loam, sandy silt, and silty clay, were selected as experimental soils, and Indigofera amblyantha was chosen as the test plant. The test conditions were controlled, such as the use of homogeneous soil and uniform plant growth conditions. Each specimen was exposed to identical atmospheric conditions controlled in a laboratory for monitoring matric suction responses over 10 days. The results showed that illumination intensities play an important role in evapotranspiration, and the thermal energy from lighting had a direct impact on plant transpiration, whereas the lighting only affected plant photosynthesis. Plant roots in vegetated soil can effectively improve the air intake value of soil, and matric suction induced by plant transpiration in vegetated soil was 1.5–2.0 times that of un-evapotranspirated soil. There is a correlation between matric suction and the silt and clay contents, and the matric suction of silty clay was sensitive to changes in the soil moisture content. Compared to fine sandy loam, the water retention of sandy silt and silty clay was high, and a high level of matric suction was maintained in the corresponding time. The results for predicting soil water evapotranspiration based on matric suction have theoretical and practical significance for preventing soil erosion and shallow landslides. In addition, these results have great guiding significance for agricultural production, such as irrigation.

Fluometuron in Soil Solution as an Indicator of Its Efficacy in Three Soils

Weed Science ◽  
1982 ◽  
Vol 30 (6) ◽  
pp. 688-691 ◽  
Author(s):  
Michael G. Patterson ◽  
Gale A. Buchanan ◽  
Robert H. Walker ◽  
Richard M. Patterson
Keyword(s):  
Organic Matter ◽  
Field Experiment ◽  
Soil Solution ◽  
Sandy Loam ◽  
Silty Clay ◽  
Clay Loam ◽  
Weed Species ◽  
Silty Clay Loam ◽  
Fine Sandy Loam

Analysis of fluometuron [1,1-dimethyl-3-(α,α,α-trifluoro-m-tolyl)urea] in soil solution after application of 0.5 or 1.0 ppmw revealed up to five-fold differences among three Alabama soils (Lucedale fine sandy loam, Decatur silty clay loam, and Sacul loam). Differences in fluometuron in soil solution were attributed to variable organic matter present and clay fractions. Fluometuron concentration in soil solution for each soil correlated well with control of four broadleaf weed species in a field experiment.

scholarly journals Study on abundance of benthic macroinvertebrates in relation to soil texture types of sediment in three ponds

2018 ◽  
Vol 7 (2) ◽  
pp. 27-35
Author(s):  
BR Irin ◽  
MA Mansur ◽  
MS Rahman
Keyword(s):  
Soil Texture ◽  
Sandy Loam ◽  
Quality Parameters ◽  
Soil Conditions ◽  
Silty Clay ◽  
Clay Loam ◽  
Silty Clay Loam ◽  
Bottom Soil ◽  
Positive Correlations ◽  
Macro Benthos

The present research was conducted to evaluate the monthly variations of macrozoobenthos of three ponds (pond 1, bottom soil is loam; pond 2, bottom soil is sandy loam; pond 3, bottom soil is silty clay loam) in relation to soil texture types of sediment. The major groups of macro-zoobenthos recorded were Chironomidae, Oligochaeta, Mollusca and Ceratopogonidae. The values of all water quality parameters such as temperature, water depth, rainfall, transparency, dissolved oxygen, pH, free CO2, NO3-N and PO4-P were found to have positive correlations in most cases, in some cases negative correlations and in few cases significant correlations. The abundance of Chironomidae was to be dominant in the pond no. 3 during the whole study period. The highest number of Oligochaeta (400 per m2) was found in pond no. 3 at depth of 150 cm and the lowest number of Oligochaeta (0 per m2) was found in pond nos. 1, 2 and 3 at both depths. The highest number of Chironomidae (1332 per m2) was found in pond no. 3 at depth of 150 cm and the lowest number of Chironomidae (444 per m2) was found in pond no. 2 at depth of 100 cm. The highest number of Ceratopogonidae (977 per m2) was found in pond no. 3 at the depth of 150 cm and the lowest number of Ceratopogonidae (178 per m2) was found in pond no. 2 at both depths. The highest number of Mollusca (1288 per m2) was found in pond no. 3 at the depth of 150 cm and the lowest number of Mollusca (222 per m2) was found in pond no. 2 at the depth of 100 cm. Satisfactory quantity of macrobenthos in the pond no. 3 at the depth of 150 cm than those of other two ponds. Between 2 depths (100 and 150 cm), the depth of 150 cm was to have highest quantity of macro-zoobenthos in all the three ponds because this depth was most favourable for macro-zoobenthos production. In pond no. 1, 2 and 3 relation of macro-benthos (no. per m2) with chemical parameters of pond bottom-soil conditions vary pond to pond which influence primary production and also influence macro-zoobenthos production (secondary production). The highest macro-zoobenthos population density was found in pond no. 3 followed by pond no. 1 and the lowest production in pond no. 2 but macro-zoobenthos production in pond no. 2 and pond no. 1 are more or less similar and macro-zoobenthos production in pond no. 3 is different and higher than those of pond nos. 1 and 2 which indicates that silty clay loam of bottom-soil is more suitable for macrozoobenthos than other soil textural classes of bottom-soil loam and sandy loam.Int. J. Agril. Res. Innov. & Tech. 7 (2): 27-35, December, 2017

Soil and alfalfa response after amelioration of subsoil acidity in a fine sandy loam Podzol in Prince Edward Island

2000 ◽  
Vol 80 (4) ◽  
pp. 607-615 ◽  
Author(s):  
M. R. Carter ◽  
J. E. Richards
Keyword(s):  
Soil Properties ◽  
Medicago Sativa ◽  
Prince Edward Island ◽  
Sandy Loam ◽  
Root Penetration ◽  
Deep Placement ◽  
Fine Sandy Loam ◽  
Subsoil Acidity ◽  
Medicago Sativa L ◽  
Over Time

Subsoils in Prince Edward Island have poor chemical and often physical quality for root growth that may present a barrier to development of alfalfa (Medicago sativa L.). This study was conducted to characterise the response or benefit, on soil properties and alfalfa growth, of chemical amelioration and loosening of the subsoil. In 1987, the following three treatments were imposed on an acidic, fine sandy loam, Humo-Ferric Podzol: control (no subsoiling or lime), subsoiling alone, and subsoiling plus lime (5 Mg ha−1 dry CaCO3) mixed into the subsoil. The subsoiler was a Wye Double-Digger, a combined plough and rotary cultivator that facilitated the mixing of lime into the soil over the 230–480 mm depth. Management of the 0–200 mm soil depth was the same for all treatments. Growth of alfalfa and change in soil properties were monitored over time. In 2 of 4 yr (1991–1994), alfalfa yield was significantly (P < 0.05) increased by the subsoil plus lime treatment, compared with subsoiling alone or the control. Yield increases were related to periods of low growing season precipitation. Subsoil amelioration increased alfalfa root penetration (by 90 mm) and reduced leaf Mn concentration. Over an 8-yr period (1987–1994), soil exchangeable Ca was increased over fourfold, while exchangeable Al was decreased threefold in the ameliorated subsoil, compared with the control. Soil pH (in water) was increased from 4.8 to near 6.0. There was some evidence that liming of the topsoil improved the subsoil chemistry over time. Bulk density and penetrometer resistance contours, measured over time, indicated that the soil loosening effect was sustained throughout the soil profile over the duration of the study. Soil biological properties were not changed by the subsoil treatments. Key words: Subsoil acidity, podzol, lime, deep placement, alfalfa (Medicago sativa L.), cool-humid climate

Rice Response to Clomazone as Influenced by Application Rate, Soil Type, and Planting Date

2007 ◽  
Vol 21 (1) ◽  
pp. 199-205 ◽  
Author(s):  
John H. O'Barr ◽  
Garry N. McCauley ◽  
Rodney W. Bovey ◽  
Scott A. Senseman ◽  
James M. Chandler
Keyword(s):  
Field Experiments ◽  
Rice Yield ◽  
Sandy Loam ◽  
Application Rate ◽  
Planting Date ◽  
Silty Clay ◽  
Clay Loam ◽  
Silty Clay Loam ◽  
Planting Dates ◽  
Fine Sandy Loam

Clomazone is an effective herbicide widely used for PRE grass control in rice. However, use of clomazone on sandy textured soils of the western Texas rice belt can cause serious rice injury. Two field experiments at three locations were conducted in 2002 and 2003 to determine the optimum rate range that maximizes barnyardgrass and broadleaf signalgrass control and minimizes rice injury across a wide variety of soil textures and planting dates. At Beaumont (silty clay loam), Eagle Lake (fine sandy loam), and Ganado (fine sandy loam), TX, PRE application of 0.34 kg ai/ha clomazone applied to rice planted in March, April, or May optimized barnyardgrass and broadleaf signalgrass control and rice yield while minimizing rice injury. Data suggest that, although injury might occur, clomazone is safe to use in rice on sandy textured soils.

The Effect of Thinning Methods on Soil Physical Properties in North-Central Mississippi

1987 ◽  
Vol 11 (2) ◽  
pp. 110-112 ◽  
Author(s):  
B. L. Karr ◽  
J. D. Hodges ◽  
T. E. Nebeker
Keyword(s):  
Sandy Loam ◽  
Soil Disturbance ◽  
Soil Physical Properties ◽  
Soil Conditions ◽  
Silty Clay ◽  
Clay Loam ◽  
Silty Clay Loam ◽  
North Central ◽  
Soil Disturbances ◽  
Dry Soil

Abstract Soil disturbances created by thinning systems on a fine sandy loam and silty clay loam during wet and dry soil conditions were examined. The extent of areal disturbance, rutting, and bulk density increased and macroporosity decreased as soil moisture and trafficking increased. Schedulingthinning during dry weather and minimizing the crossing of planting beds with equipment reduced soil disturbance. South. J. Appl. For. 11(2):110-112.

Dissipation and Leaching of Pyroxasulfone andS-Metolachlor

2014 ◽  
Vol 28 (1) ◽  
pp. 72-81 ◽  
Author(s):  
Eric P. Westra ◽  
Dale L. Shaner ◽  
Philip H. Westra ◽  
Phillip L. Chapman
Keyword(s):  
Sandy Loam ◽  
Sandy Loam Soil ◽  
Soil Conditions ◽  
Clay Loam ◽  
Clay Loam Soil ◽  
Fine Sandy Loam ◽  
Northern Colorado ◽  
Fine Clay ◽  
Loam Soil ◽  
Dry Soil

Pyroxasulfone dissipation and mobility in the soil was evaluated and compared toS-metolachlor in 2009 and 2010 at two field sites in northern Colorado, on a Nunn fine clay loam, and Olney fine sandy loam soil. Pyroxasulfone dissipation half-life (DT50) values varied from 47 to 134 d, and those ofS-metolachlor ranged from 39 to 63 d. Between years, herbicide DT50values were similar under the Nunn fine clay loam soil. Under the Olney fine sandy loam soil, dissipation in 2009 was minimal under dry soil conditions. In 2010, under the Olney fine sandy loam soil,S-metolachlor and pyroxasulfone had half-lives of 39 and 47 d, respectively, but dissipation rates appeared to be influenced by movement of herbicides below 30 cm. Herbicide mobility was dependent on site-year conditions, in all site-years pyroxasulfone moved further downward in the soil profile compared toS-metolachlor.

Influence of tillage and liquid swine manure on productivity of a soybean-barley rotation and some properties of a fine sandy loam in Prince Edward Island

2006 ◽  
Vol 86 (4) ◽  
pp. 741-748 ◽  
Author(s):  
M R Carter ◽  
A J Campbell
Keyword(s):  
Soil Properties ◽  
Prince Edward Island ◽  
Sandy Loam ◽  
Soil Depth ◽  
Swine Manure ◽  
Residual Effect ◽  
Crop Response ◽  
Fine Sandy Loam ◽  
Liquid Swine Manure ◽  
Second Year

Interactions between tillage management for manure incorporation and rate of manure application may influence crop productivity and soil properties. This study was conducted to evaluate the effect of liquid swine (Sus scrofa L.) manure (LSM) applied at three N rates (40, 80, 160 kg ha-1), compared with mineral N fertilizer, in a 2-yr barley (Hordeum vulgare L.)-soybean (Glycine max L. Merr.) rotation, incorporated by two tillage methods (chisel plough and disc), on crop yield and quality and some soil properties, especially C parameters. The LSM was applied every second year in the spring, prior to barley seeding. The study was conducted over a 5-yr period on a Charlottetown fine sandy loam (Orthic Humo-Ferric Podzol) in Prince Edward Island. The experimental design was a split-plot with four replicates. Soil samples (0–60 cm) were obtained at the termination of the study to determine residual effects of the LSM on soil properties. The two methods of LSM incorporation had no differential effect on crop response. Generally, increasing the application rate of LSM increased the barley yield, but had no effect on grain N concentration. A residual effect on crop grain yield for the high rate of LSM was evident in the soybean year. Crop response to LSM was similar to that of mineral fertilizer. Application operations for LSM had no adverse effect on soil strength or soil bulk density. Soil properties (microbial biomass C, carbohydrates, water-stable aggregates) were not greatly influenced by LSM application, however, increases in particulate C (POM-C) were evident for the high LSM rate at the 10- to 30-cm soil depth. The study showed that for fine sandy loams in Prince Edward Island low to medium rates of LSM applied every second year could serve as a source of N for barley in barley-soybean rotations. Key words: Barley, soybean, liquid swine manure, fine sandy loam, soil properties, tillage incorporation, eastern Canada

Johnsongrass Control in Soybeans by Trifluralin and Nitralin

Weed Science ◽  
1974 ◽  
Vol 22 (2) ◽  
pp. 111-115 ◽  
Author(s):  
C. G. McWhorter
Keyword(s):  
Glycine Max ◽  
Field Experiments ◽  
Sandy Loam ◽  
Continuous Treatment ◽  
Sorghum Halepense ◽  
Silty Clay ◽  
Clay Loam ◽  
Silty Clay Loam ◽  
Fine Sandy Loam ◽  
Immediate Incorporation

Field experiments were conducted to study the feasibility of using trifluralin (α,α,α-trifluoro-2,6-dinitro-N,N-dipropyl-p-toluidine) and nitralin [4-(methylsulfonyl)-2,6-dinitro-N,N-dipropylaniline] for the selective control of johnsongrass [Sorghum halepense(L.) Pers.] from rhizomes and seed in soybeans[Glycine max(L.) Merr. ‘Lee’]. Both herbicides were incorporated into the soil at 0.56 to 3.36 kg/ha with two disk cultivations immediately after application. Most effective johnsongrass control on Dundee silty clay loam (sicl) followed treatments of nitralin or trifluralin at 1.68 to 3.36 kg/ha, but 2 years or more of continuous treatment were required for acceptable control. Trifluralin at 1.12 and 2.24 kg/ha on Sharkey clay and at 0.56 to 2.24 kg/ha on Bosket fine sandy loam (fsl) provided better average johnsongrass control over a 2-year period than nitralin at the same rates, but soybean yields after both herbicides at the same rates were equal. Immediate incorporation of trifluralin or nitralin in all three soils at 1.12 to 2.24 kg/ha for 2 successive years effectively controlled johnsongrass from rhizomes without soybean injury and with greatly increased soybean yields.

Impact of natural or industrial liming materials on soil properties and microbial activity

2009 ◽  
Vol 89 (2) ◽  
pp. 209-222 ◽  
Author(s):  
Roger Lalande ◽  
Bernard Gagnon ◽  
Isabelle Royer
Keyword(s):  
Alkaline Phosphatase ◽  
Soil Properties ◽  
Microbial Activity ◽  
Soil Ph ◽  
Clay Soil ◽  
Sandy Loam ◽  
Soil Layer ◽  
Cement Kiln ◽  
Silty Clay ◽  
Silty Clay Soil

Soil acidity is a major problem in agriculture because it limits plant growth and reduces crop productivity. The neutralizing potential of industrial by-products and their impact on soil properties were evaluated in two acidic soils characterized by contrasting textures, and submitted to intensive agriculture practices. Soil pH, microbial (dehydrogenase and alkaline phosphatase) activity, and Mehlich-3 extractable P, K, Ca and Mg were monitored in the year of soil incorporation of eight liming products and in the following 2 yr. In the sandy loam, liming products did not result in significant increases in soil pH in the 0- to 7.5-cm soil layer. Lime mud (LM) significantly increased soil pH by 0.4 units in the 7.5- to 20-cm layer compared with cement kiln dust (CKD). In the silty clay, calcium-phosphate-magnesium (CalPoMag) significantly raised pH by 0.65 units over both natural calcitic lime (NCa) and the magnesium dissolution product (MgD) in the first soil layer, and by 0.5 units over carbide lime (CL) treatment in the second soil layer. Activities of dehydrogenase and alkaline phosphatase were increased to various degrees by all liming materials, especially on the silty clay; LM and CalPoMag were the most beneficial materials. The exception was MgD, which did not result in any impact on microbial activity relative to the control. Both enzymatic activities were related to the increase in soil pH, particularly the alkaline phosphatase. Ion leaching was more pronounced in the sandy loam than in the silty clay soil, where large differences in the Ca and Mg ion levels were still detected in the 20- to 40-cm layer of the sandy loam. In this study, LM and CalPoMag are interesting liming products, particularly in the silty clay soil. Key words: Enzymatic activity, soil pH, lime, soil cations

The effect of tillage and KCl addition on pH, conductance, NO3-N, P, K and Cl distribution in the soil profile

1994 ◽  
Vol 74 (3) ◽  
pp. 307-314 ◽  
Author(s):  
C. A. Grant ◽  
L. D. Bailey
Keyword(s):  
Soil Profile ◽  
Clay Soil ◽  
Sandy Loam ◽  
Sandy Loam Soil ◽  
Silty Clay ◽  
Zero Tillage ◽  
Tillage Systems ◽  
Fine Sandy Loam ◽  
Loam Soil ◽  
Silty Clay Soil

Distribution of NO3, P, K, Cl, pH and conductance through the soil profile were measured on two soil types after 4 yr of crop production using zero tillage (ZT) or conventional tillage (CT), with or without addition of KCl. All plots received N and P fertilizer each year as banded applications. Surface concentrations of NO3-N were higher under ZT than CT, particularly on the fine sandy loam soil. Accumulation of NO3-N also occurred in the 60- to 120-cm zone, under both tillage systems in both soils. Carryover of NO3-N was substantially greater on the silty clay than the fine sandy loam soil. Phosphate accumulated at the depth of band application in both soils under both tillage systems. Potassium concentration was generally higher under ZT than CT in the surface 15 cm of both soils, presumably due to surface retention of K from fertilizer applications and crop residues. Chloride was higher under ZT than CT in the surface 5 cm of both soils, but was higher under CT than ZT in the 30- to 60-cm and 60- to 120-cm depths in the silty clay soil, if KCl had been applied. The pH on both soils under both tillage systems was reduced in the 10- to 12.5-cm soil depth, corresponding to the zone of fertilizer application. On the silty clay soil, pH was higher under ZT than CT in the 10- to 15-cm depth and tended to be higher under ZT than CT at all depths below 15 cm. Conductance was not influenced by tillage in either soil. Application of KCl increased K and Cl concentrations in the surface 15 cm on both soils. Concentration of Cl was increased to 120 cm in both soils, indicating the mobility and leaching potential of this anion. Conductance and pH were increased in the 2.5- to 5.0-cm and 10- to 12.5-cm depths by KCl application in the fine sandy loam soil, but on the silty clay soil, only conductance was increased. Key words: Zero tillage, nutrient stratification, pH stratification

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