Some effects of urea and of soil moisture on solute translocation

1975 ◽  
Vol 53 (8) ◽  
pp. 756-763 ◽  
Author(s):  
Wm. Harold Minshall
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Soil Moisture Content ◽  
Sandy Loam ◽  
Water Control ◽  
Tomato Plants ◽  
Soil Mixture ◽  
Solute Uptake ◽  
Before And After ◽  
Loam Soil

In detopped plants, stump exudation resulting from root pressure provides a measure of the quantity of solutes and of water being transferred to the xylem. In dry soil the transfer of water to the xylem stops when the force required to remove the water from the soil is equal to the osmotic pull of the solutes in the xylem. In a sandy loam soil mixture, detopped tomato plants (Lycopersicon esculentum Mill.) treated with urea maintained stump exudation to a soil moisture content as low as 12.1% while water-control plants ceased exudation at 15.0% soil moisture. By maintaining the transfer of solutes to the xylem, the application of urea enhanced the ability of the detopped root system to remove water from the dry soil.By watering plants to pot capacity at different times before and after detopping, a series of soil moisture levels were obtained with detopped roots of tomato. In this clay loam soil mixture stump exudation started at 10% soil moisture (about −3.0 bars potential). With increasing moisture the rate of exudation increased rapidly to reach a maximum exceeding 5 ml per hour at soil moisture contents between 20 and 25% (about −0.05 bars potential). The rate then decreased gradually to 2.5 ml per hour as the soil moisture content increased from 25 to 45%. Starting at 10% soil moisture and continuing up to 25%, solute uptake increased proportionately with increasing moisture content, and at these dry and medium soil moisture levels, the supply of water to the root determined the quantity of solutes being translocated to the stump. The depletion of oxygen and accumulation of carbon dioxide in soils containing more than 25% moisture reduced the translocation of solutes in the plants.

EFFECTS OF IRRIGATION AND NITROGEN ON A NATURAL PASTURE SWARD

1978 ◽  
Vol 58 (2) ◽  
pp. 347-356
Author(s):  
W. N. BLACK
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Soil Moisture Content ◽  
Sandy Loam ◽  
Field Capacity ◽  
Early Spring ◽  
Naturally Occurring ◽  
Natural Pasture ◽  
Loam Soil ◽  
Grazing Period

Irrigation and nitrogen (N) requirements of a natural pasture sward were studied on a Charlottetown sandy loam soil over a 5-yr period. The soil moisture content at the 0-to 15- and 15- to 30-cm depths was determined at from 7- to 10-day intervals, while irrometer soil moisture readings at 15-, 30-, and 45-cm depths were recorded more frequently during the grazing seasons. Soil moisture content in irrigated plots averaged 92 and 94% of field capacity, respectively, at 0- to 15- and 15- to 30-cm sampling depths. In non-irrigated plots, corresponding values were 77 and 82%. N treatments resulted in significant dry matter (DM) increases over untreated plots. Yield differences among plots receiving 56, 84, and 112 kg of N/ha in mid-June and again in mid-August were not significant. Early spring and September applications of N at 56 kg/ha, combined with mid-June and early August supplements of N at 84 kg/ha were superior to all other treatments in prolonging the grazing period. Neither irrigation nor N affected the characteristic yield decline of naturally occurring forage species in mid- and late-season. Mean DM production for the 5-yr period, and for years, showed no significant N treatment × moisture level interaction. While irrigation failed to increase yields significantly, livestock preferred to graze the irrigated plots. As a result of less competition from grasses, volunteer white clover became better established, and constituted a larger percentage of the sward than on non-irrigated plots.

scholarly journals Effect of Ploughing Depth, Tractor Forward Speed, and Plough Types on the Fuel Consumption and Tractor Performance

2019 ◽  
Vol 9 (1) ◽  
pp. 43-49
Author(s):  
Kareem Ibrahim kareem ◽  
P. Sven
Keyword(s):  
Soil Moisture ◽  
Fuel Consumption ◽  
Agricultural Production ◽  
Soil Moisture Content ◽  
Sandy Loam ◽  
Forward Speed ◽  
Power Requirement ◽  
Primary Tillage ◽  
Loam Soil ◽  
Ploughing Depth

Cost of fuel has a significant impact on the input costs of agricultural production, especially during primary tillage. It is affected by several parameters including tractor forward speed, depths of ploughing, and plough types. The experiment was performed in a Soil Hall at Harper Adams University, United Kingdom, in April 2015. A Massey Ferguson 8480 4WD tractor was used for investigating objectives of this study. The experiment was performed in a sandy loam soil texture at 11.73% soil moisture content and 1.35 (g/cm3) dry bulk density to study the amount of fuel consumption (l/ha) and the performance of tractor with effect of moldboard and disc ploughs as ploughs type, 15 and 20 cm as ploughing depth and 5 and 7 km/h as tractor forward speeds. The results showed that fuel consumption with a disc plough 5% was higher compared to the moldboard. Fuel consumption decreased approximately 8% when tractor at 7 km/h. Fuel consumption significantly decreased about 34% when ploughing depth increased from 15 to 20 cm. The power requirement to operate moldboard plough was higher by about 14% than a disc. The power requirement at speeds of 7 km/h was higher compared to the speeds of 5 km/h by about 27%. When the depth of ploughing increased from 15 to 20 cm, the power requirement increased by about 1.5%.

scholarly journals Draft Requirement of Two Animal - Drawn Institute for Agricultural Research (IAR) Weeders

2020 ◽  
pp. 14-20
Author(s):  
Y. A. Unguwanrimi ◽  
A. M. Sada ◽  
G. N. Ugama ◽  
H. S. Garuba ◽  
A. Ugoani
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Bulk Density ◽  
Soil Moisture Content ◽  
Agricultural Research ◽  
Soil Samples ◽  
Soil Conditions ◽  
Experimental Plot ◽  
Moisture Contents ◽  
Loam Soil

Draft requirements of two animal – drawn (IAR) weeders operating on loam soil were determined in the study. The implements include a straddle row weeder and an emcot attached rotary weeder evaluated under the same soil conditions, using a pair of white Fulani breed of oxen. The animal draft requirement was first estimated from the animal ergonomics measurements. Using area of 0.054 hectare as experimental plot for each implement the draft requirement of each implement was investigated after taking soil samples for soil moisture content and bulk density determinations. The implements tested showed variation in their average draft requirement. The straddle row weeder had the highest value of 338.15 N respectively while the emcot attached rotary weeder had the lowest value of 188.12 N with 47.03%, respectively. The average soil moisture contents and bulk density were 13.0% and 1.46%/cm3, respectively.

scholarly journals Effects of Rain Intensity and Initial Soil Moisture on Hydrological Responses in Laboratory Conditions

2015 ◽  
Vol 29 (2) ◽  
pp. 165-173 ◽  
Author(s):  
Abdulvahed Khaledi Darvishan ◽  
Kazimierz Banasik ◽  
Seyed Hamidreza Sadeghi ◽  
Leila Gholami ◽  
Leszek Hejduk
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Soil Moisture Content ◽  
Sandy Loam ◽  
Initial Moisture Content ◽  
Hydrological Responses ◽  
Laboratory Conditions ◽  
Initial Soil Moisture ◽  
Erosion Processes ◽  
Initial Soil

Abstract Although the possibility of measuring and analysing all parts of the rainfall, infiltration, runoff, and erosion process as a natural hydrologic cycle in field conditions is still one of the more unattainable goals in the hydrological sciences, it can be accomplished in laboratory conditions as a way to understand the whole process. The initial moisture content is one of the most effective factors on soil infiltration, runoff, and erosion responses. The present research was conducted on a 2 m2 laboratory plot at a slope of 9% on a typical sandy-loam soil. The effects of the initial soil moisture content on the infiltration, runoff, and erosion processes were studied at four levels of initial soil moisture content (12, 25, 33, and 40 volumetric percentage) and two rainfall intensities (60 and 120 mm h-1). The results showed a significant (p ≤ 0.05) correlation between rainfall intensity and downstream splash, with r = 0.87. The results reflected the theory of hydrological responses, showing significant (p ≤ 0.05) correlations with r =-0.93, 0.98, -0.83, 0.88, and 0.73 between the initial soil moisture content and the time-to-runoff, runoff coefficient, drainage as a part of the infiltrated water, downstream splash, and total outflow sediment, respectively.

A LABORATORY STUDY ON THE EFFECTS OF SOIL MOISTURE CONTENT, TEXTURE, AND TIMING OF LEACHING ON N LOSS FROM TWO SOUTHERN ALBERTA SOILS

1982 ◽  
Vol 62 (2) ◽  
pp. 407-413 ◽  
Author(s):  
T. G. SOMMERFELDT ◽  
C. CHANG ◽  
J. M. CAREFOOT
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Soil Moisture Content ◽  
Sandy Loam ◽  
Wetting Front ◽  
N Losses ◽  
Initial Soil Moisture ◽  
N Removal ◽  
Southern Alberta ◽  
Initial Soil

A column study was conducted to determine the effects of soil texture, initial soil moisture content and timing of leaching on N removal from two irrigated soils of southern Alberta. Pelleted NH4NO3 fertilizer (0.639 g N per column = 336 kg∙ha−1) was applied to Lethbridge loam (Leth L) and Cavendish fine sandy loam (CV FSL) at three initial levels of soil moisture: air dry (AD), 0.5 field capacity (0.5 FC), and wet (W, 25 cm suction). Leaching began immediately after the fertilizer application or was delayed 1 wk. Water was applied in 1400-mL (7.6 cm depth) increments every 2nd day for a total of 33 600 mL (175 cm depth). The leachate was collected, measured, and analyzed for NH4-N and NO3-N. The soil was analyzed for N content before and after leaching. More N was leached from CV FSL (0.600 g) than from Leth L (0.521 g). Responses to initial soil moisture were similar for both soils; the NO3-N concentration peak followed the advancing wetting front more closely in the AD than in the W systems and leaching losses were greatest from the 0.5 FC treatment. Delayed leaching did not significantly affect the amount of N leached. N losses, other than from leaching, were greatest in the W and AD treatments, in the AD treatment these losses were attributed to volatilization and, in the W soils, to denitrification.

Atrazine Adsorption on Soil as Influenced by Temperature, Moisture Content and Electrolyte Concentration

Weed Science ◽  
1978 ◽  
Vol 26 (3) ◽  
pp. 303-308 ◽  
Author(s):  
T. H. Dao ◽  
T. L. Lavy
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Soil Solution ◽  
Adsorption Isotherms ◽  
Soil Moisture Content ◽  
Electrolyte Concentration ◽  
Thermodynamic Quantities ◽  
Endothermic Reaction ◽  
Freundlich Equation ◽  
Before And After

The adsorption of atrazine [2-chloro-4-(ethylamino)-6-(isopropylamino)-s-triazine] was measured on soil at water:soil ratio of 5:1 and 0.4:1. The adsorption isotherms for atrazine were described by the Freundlich equation. A decrease in water:soil ratio and in soil moisture content led to an increased adsorption of the herbicide. Increasing the concentration of electrolytes in the soil solution by adding solutions up to 0.1M CaCl2increased atrazine adsorption. Greater amounts of atrazine were adsorbed at 30 than at 5 C on four soils at 0.1 bar moisture content. This indicates an endothermic reaction which was observed both before and after correction for differential atrazine solubility due to temperature. Thermodynamic quantities associated with the adsorption reaction were calculated to characterize the adsorption of atrazine on soil.

REGRESSIONS FOR ESTIMATING STRAW YIELDS AND N AND P CONTENTS OF SPRING WHEAT AND N MINERALIZATION IN A BROWN LOAM SOIL

1988 ◽  
Vol 68 (2) ◽  
pp. 337-344 ◽  
Author(s):  
C. A. CAMPBELL ◽  
R. P. ZENTNER ◽  
F. SELLES
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Spring Wheat ◽  
N Mineralization ◽  
Soil Moisture Content ◽  
N Uptake ◽  
Growing Season ◽  
Net N Mineralization ◽  
Loam Soil ◽  
Growing Season Precipitation

Data from an 18-yr crop rotation study carried out on a Brown loam soil at Swift Current, Saskatchewan, were used to estimate equations that relate spring wheat straw yields, and N and P content of grain and straw to moisture use (MU). Moisture use was defined as soil moisture content in 0- to 120-cm depth at seeding, less soil moisture content at harvest, plus growing season precipitation. Grain yields were also related to straw yields and to N content of the straw. Potential net N mineralization (Nmin) in summerfallow (periods during the growing season with negative Nmin omitted) was related (r = 0.74**) to precipitation received during the spring to fall period. An attempt to relate apparent net Nmin (determined by N balance) in cropped systems to growing season precipitation or to MU was not successful. Highly significant linear regressions were obtained for straw yields, grain N and P contents vs. MU, and for grain yield vs. straw yield (r = 0.66** – 0.83**), but the other relationships were less reliable (r = 0.41** – 0.55**) though still significant. We discussed how these relationships might be used to estimate fertilizer N requirements, for examining N immobilization-mineralization, and for estimating residue sufficiency for erosion control on summerfallowed land. Key words: Straw:grain ratio, N uptake, P uptake, crop residues, N mineralization

Soil moisture content estimation using water absorption bands

GEOMATICA ◽  
2019 ◽  
Vol 73 (3) ◽  
pp. 63-73 ◽  
Author(s):  
Mohammad Reza Mobasheri ◽  
Meisam Amani ◽  
Mahin Beikpour ◽  
Sahel Mahdavi
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Water Absorption ◽  
Soil Moisture Content ◽  
Mean Squared Error ◽  
Sandy Loam ◽  
Soil Types ◽  
Accurate Estimation ◽  
Absorption Bands ◽  
New Models

Soil moisture content (SMC) is a crucial component in various environmental studies. Although many models have been proposed for SMC estimation, developing new models for accurate estimation of SMC is still an interesting subject. This study aimed to develop new models for SMC estimation using the water absorption bands in the spectral signatures of three different soil types: loam, silty loam, and sandy loam. Based on the three absorption bands (i.e., 1400, 1900, and 2200 nm) and regression analyses, six approaches were considered. These scenarios were generally based on the reflectance value and its logarithm, as well as the difference between the wet and dry reflectance values for the absorption bands. Finally, 24 models were developed for SMC estimation from the three different soil types, as well as the entire soil samples. The most accurate SMC, as indicated by the lowest root mean squared error (RMSE) and the highest correlation coefficient (r), was obtained from the model developed using the logarithm of the average values reflectance in the three water absorption bands for sandy loam (RMSE = 0.31 g/kg, r = 0.99). Overall, using the spectrometry data derived in the lab, the results of the proposed models were promising and demonstrate great potential for SMC estimation using spectral data collected by satellites in the future studies.

scholarly journals Soil Compaction Due to Harvest Traffic in Sugarcane Fields on a Lajas Valley Farm of Puerto Rico

1969 ◽  
Vol 58 (3) ◽  
pp. 279-292
Author(s):  
Lal N. Shukla
Keyword(s):  
Puerto Rico ◽  
Soil Moisture ◽  
Moisture Content ◽  
Soil Compaction ◽  
Soil Moisture Content ◽  
Field Capacity ◽  
Before And After

Soil compaction tests were conducted on a farm in the Lajas Valley of Puerto Rico. Experiments were carried out in five fields of sugarcane to determine soil compaction caused in the center of furrows by a J & L harvester and in banks of ridges caused by loaded transport carts. Similar tests also were conducted in three additional fields to determine soil compaction caused by the harvester in the center of furrows at a moisture content close to field capacity. Penetrometer readings were taken at random in the center of furrows and in the banks of ridges before and after the passing of the load. Soil moisture content was determined in these locations by the oven-dry method. Soil compaction caused by the harvester was not severe under the conditions of the test, but the loaded transport carts caused considerable soil compaction in the bank of the ridges.

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