YIELD OF SOYBEANS AND OIL QUALITY IN RELATION TO SOIL TEMPERATURE AND MOISTURE IN A FIELD ENVIRONMENT

1972 ◽  
Vol 52 (2) ◽  
pp. 225-235 ◽  
Author(s):  
A. R. MACK ◽  
K. C. IVARSON
Keyword(s):  
Soil Temperature ◽  
Oil Quality ◽  
Seasonal Temperature ◽  
High Concentration ◽  
Field Environment ◽  
Soil Temperatures ◽  
Oil Concentration ◽  
High Yields ◽  
High Soil Temperature ◽  
Soil Temperature And Moisture

Under comparable field conditions of air temperature and solar radiation, yield of soybeans increased 43.4% when the day-degrees units of the soil were raised from a seasonal value of 859 to 1822 (> 5 C) and yield decreased 82.4% when the day-degrees for the same period were lowered to 408 for the 20-cm depth. These heat values from July 10 to September 21 correspond to mean daily soil temperatures of 11.2, 17.7, and 31.2 C. The change in yield represents a reduction on the cold soils of 208 kg/ha (3.1 bu/acre) per 1 degree C below the seasonal temperature, and an increase on the warm plots of 54 kg/ha per 1 degree C (unfertilized) above the seasonal temperature. In general, yield was related linearly to the reciprocal of the temperature and of the day-degrees. Oil concentration varied little among the three soil temperatures, although the iodine number decreased and the percentage protein increased with higher soil temperature. Coinciding with the high yields on the warm soils was a high concentration of P in the foliage, e.g., 0.15% P at 11.2 C and 0.42% at 31.9 C. During early growth, concentration of K in the plant material increased and that of Mn and Cu was reduced with high soil temperature. This resulted in a greater removal of P and K from the warm soil than from the cool soil, and little difference in removal of Mn and Cu between the low and high temperatures.

ROOT-SURFACE MYCOFLORA OF SOYBEAN IN RELATION TO SOIL TEMPERATURE AND MOISTURE IN A FIELD ENVIRONMENT

1972 ◽  
Vol 52 (2) ◽  
pp. 199-208 ◽  
Author(s):  
K. C. IVARSON ◽  
A. R. MACK
Keyword(s):  
Soil Temperature ◽  
Relative Frequency ◽  
Incubation Temperature ◽  
Growing Season ◽  
Root Surface ◽  
Growing Seasons ◽  
Field Environment ◽  
Abundant Genus ◽  
Field Plots ◽  
Soil Temperature And Moisture

Studies were made on the root-surface fungi of soybean grown in field plots where various soil temperature and moisture environments had been maintained for five previous growing seasons. Washed-root segments were incubated on agar plates at temperatures corresponding to those of the field plots. Fusarium was the most abundant genus appearing on the plates. Species of Mucor, Trichoderma, Alternaria, Mortierella, Aspergillus, Corynespora, Rhizoctonia, Penicillium, Gliocladium, and sterile forms appeared fairly frequently. Statistical analysis of the data revealed that changes in soil and incubation temperature markedly affected the relative frequency of 12 genera, and age of plant significantly affected nine genera. Soil moisture influenced the frequency of only one genus. High soil and incubation temperature (28 C) encouraged greater root populations of Rhizoctonia early in the season, Trichoderma and Aspergillus throughout the growing season, and Fusarium late in the season. Low soil temperature conditions (12 C) favored growth of Pythium, Mortierella, Mucor, Alternaria, Cladosporium, throughout the growing season, and Corynespora and Cylindrocarpon, primarily during mid-season. Late in the season Gliocladium preferred the intermediate temperature of 20 C.

scholarly journals A Musty “Off” Flavor in Nova Scotia Potatoes Is Associated with 2,4,6-Trichloroanisole Released from Pesticide-treated Soils and High Soil Temperature

2007 ◽  
Vol 132 (1) ◽  
pp. 112-119 ◽  
Author(s):  
Barbara J. Daniels-Lake ◽  
Robert K. Prange ◽  
Sonia O. Gaul ◽  
Kenneth B. McRae ◽  
Roberto de Antueno ◽  
...  
Keyword(s):  
Soil Temperature ◽  
Solid Phase ◽  
The Other ◽  
Spectrometric Analysis ◽  
Potato Tubers ◽  
High Soil ◽  
Two Factors ◽  
Soil Temperatures ◽  
Annapolis Valley ◽  
High Soil Temperature

In Fall 2001 in Nova Scotia's Annapolis Valley (Canada), several million kilograms of processing and table-stock potatoes (Solanum tuberosum L.) were affected by a severe “musty” “off” flavor and “off” odor that persisted after cooking. 2,4,6-Trichloroanisole (TCA), a potent musty flavor/odor compound that is not known to be a potato metabolite was detected in samples of three potato lots rejected by consumers. To determine the role and source of TCA in the affected crop, samples of tubers from 30 fields were evaluated, including examination of production inputs and industry estimation of the “off” flavor, expert organoleptic assessment of flavor–odor intensity, and analytical quantitation of the TCA content of affected tubers, followed by a soil challenge to provoke TCA production. Production of “musty” potatoes was associated with unusually hot (>30 °C) soil temperatures during the 2001 growing season, and in some cases with γ-cyclohexane hexachloride (CHC) applied to control soil wireworm (putatively Limonius agonus Say). TCA quantitation and organoleptic assessment were in general agreement. Samples of soils from “idle” fields (no agricultural inputs for at least 8 years) and “production” fields (produced “off”-flavor potatoes in 2001) were subjected to several factors: 1) presence or absence of potato tubers; 2) preheating at 30 °C for 3 days, or no preheating; and followed by 3) no pesticides, or γ-CHC, chlorothalonil, chlorpyrifos, fludioxonil, imidacloprid, or linuron applied singly, or all six pesticides applied together. After incubation for 2 weeks at 22 °C day/14 °C night with a 14-hour photoperiod, solid-phase microextraction/gas chromatographic–mass spectrometric analysis revealed that untreated soils released small quantities of TCA (2.8 mol·kg−1) whereas higher quantities of TCA were present in soils treated with pesticides (3.8–6.6 mol·kg−1). The quantity of TCA released was not significantly affected by the presence or absence of potato tubers, but it was increased by preheating the soil sample, regardless of the other two factors, and by an interaction between pesticides and soil source. The quantity of TCA from both “idle” and “production” soils was highest when γ-CHC was added alone (214% and 284% of checks respectively). TCA production increased in the presence of the other five pesticides applied singly in “production” soils, but not in “idle” soils. Application of the six pesticides together increased TCA in both soils. Such an association of TCA-based “musty” “off” flavor with field soils containing γ-CHC and other pesticides combined with high soil temperature had not been reported previously.

STUDIES ON RHIZOCTONIA SOLANI KÜHN.: IV. EFFECT OF SOIL TEMPERATURE AND MOISTURE ON VIRULENCE

1938 ◽  
Vol 16c (5) ◽  
pp. 203-213 ◽  
Author(s):  
G. B. Sanford
Keyword(s):  
Growth Rate ◽  
Soil Moisture ◽  
Moisture Content ◽  
Soil Temperature ◽  
Growth Rates ◽  
Nutrient Medium ◽  
Soil Moisture Content ◽  
Soil Temperatures ◽  
Dry Soil ◽  
Soil Temperature And Moisture

The effects of soil temperatures between 16° and 25 °C., and of soil moisture content between 19 and 40% of the moisture-holding capacity, on the virulence and type of attack of Rhizodonia Solani on young potato sprouts, were studied under controlled conditions and the results from 13 separate tests are discussed. The comparative growth rates of the pathogen on nutrient agar and in soil are outlined.At 25 °C. the disease diminished very abruptly. Between 23° and 16 °C., the pathogen appeared equally virulent throughout the range of soil moisture mentioned. The fluctuations which occurred in separate tests were not definite or consistent enough to warrant a conclusion that the virulence is greater at 16° than at 23°, or that a dry soil is more or less favorable to it than a wet one.In a fertile, steam sterilized loam, at medium moisture content, it required about ten days for the pathogen to grow as far as it did on the surface of a nutrient medium in four days. The growth rate at either 23° or 16 °C. was slightly higher in a wet soil than in one of medium moisture content, but in a dry soil the rate was somewhat less at 23° than at 16° in a medium or wet soil. Even in a fairly dry soil (19% moisture-holding capacity) at 16° the growth of the pathogen covered a distance of 5 cm. in ten days, which would appear adequate for infection of young sprouts from a set bearing viable sclerotia.The effort of the host to recover, by means of secondary and tertiary sprouts from the attacked primary sprout, was better in a wet soil than in a dry one at both 16° and 23 °C. The best effort was in a wet soil at 23°. A distinction is made between the effects of soil moisture and temperature in stimulating growth of the host, and their effect on parasitism itself.The remarkable tendency of the secondary sprouts to escape infection, regardless of soil temperature and soil moisture, is indicated. There was evidence that certain factors other than soil temperature and moisture may play an important role in the parasitism of R. Solani.

Effect of Soil Temperature and Moisture on Glyphosate and Photoassimilate Distribution in Quackgrass (Agropyron repens)

Weed Science ◽  
1984 ◽  
Vol 32 (3) ◽  
pp. 402-407 ◽  
Author(s):  
Thomas B. Klevorn ◽  
Donald L. Wyse
Keyword(s):  
Soil Moisture ◽  
Water Stress ◽  
Soil Temperature ◽  
Soil Temperatures ◽  
Growth Chambers ◽  
Rhizome Buds ◽  
Rhizome System ◽  
Soil Temperature And Moisture ◽  
Agropyron Repens

Experiments were conducted in growth chambers to evaluate the effect of soil temperature and soil moisture on the distribution of14C-photoassimilates and14C-glyphosate [N-(phosphonomethyl) glycine] in quackgrass [Agropyron repens(L.) Beauv. ♯3AGRRE]. When14C-glyphosate was applied to leaves, the radioactivity was less in the rhizome buds of plants exposed to 7-C soil temperature than in plants exposed to 12- and 18-C soil temperatures after 2 days. In plants with leaves exposed to14CO2, the radioactivity from14C-photoassimilates was greatest in rhizomes and rhizome buds of plants at the 12-C soil temperature. As soil moisture levels were decreased, uptake of C-glyphosate into leaves declined, and transport to the daughter shoots, rhizomes, and rhizome buds was reduced. The concentration of14C-photoassimilates in the rhizome system of water-stressed quackgrass plants was similar to that in nonstressed plants. This study shows that the patterns of glyphosate distribution differ from those of photoassimilate distribution in quackgrass plants exposed to water stress.

Influence of Soil Temperature and Moisture on Terbutryn Activity and Persistence

Weed Science ◽  
1974 ◽  
Vol 22 (6) ◽  
pp. 571-574 ◽  
Author(s):  
Chu-Huang Wu ◽  
P. W. Santelmann ◽  
J. M. Davidson
Keyword(s):  
Soil Moisture ◽  
Soil Temperature ◽  
Incubation Temperature ◽  
Sandy Loam ◽  
Distribution Coefficients ◽  
Measured Parameter ◽  
Soil Conditions ◽  
Soil Temperatures ◽  
Dry Soil ◽  
Soil Temperature And Moisture

The phytotoxicity of soil-applied terbutryn [2-(tert-butylamino)-4-(ethylamino)-6-(methylthio)-s-triazine] to wheat (Triticum aestivumVill.) was significantly affected by soil moisture and soil temperature. Distribution coefficients (Kd) provided a better indication of the phytotoxicity of terbutryn to wheat than any single measured parameter contributing to herbicide adsorption by the soil. Soil temperatures and soil moisture levels suitable for good plant growth tended to enhance the phytotoxicity of terbutryn. No phytotoxic levels of terbutryn to wheat were detected in Teller sandy loam after 20 weeks of incubation at above 10C and 14% soil moisture by weight. However, phytotoxicity to wheat was observed in air-dry terbutryntreated soil after an incubation period of 20 weeks, regardless of incubation temperature. Significant quantities of terbutryn may remain in the field under dry soil conditions.

Effects of soil temperature and moisture on the pathogenicity of fungi associated with root rot of subterranean clover

1984 ◽  
Vol 35 (5) ◽  
pp. 675 ◽  
Author(s):  
DH Wong ◽  
MJ Barbetti ◽  
K Sivasithamparam
Keyword(s):  
Soil Temperature ◽  
Root Rot ◽  
Marked Effect ◽  
Subterranean Clover ◽  
Pythium Irregulare ◽  
Highly Pathogenic ◽  
Soil Temperatures ◽  
Moisture Conditions ◽  
Water Holding ◽  
Soil Temperature And Moisture

The effects of soil temperature (10, 15, 20 and 25�C) and moisture (45% water holding capacity (WHC), 65% WHC, and flooding) on the pathogenicity of five fungi, both alone and in combinations, were investigated to determine the involvement of these fungi in a severe root rot disorder of subterranean clover in Western Australia. Fusarium avenaceum, Pythium irregulare, and Rhizoctonia solani were highly pathogenic while Fusarium oxysporum and Phoma medicaginis, particularly when used singly, were only weakly pathogenic. Compared with individual fungi, fungal combinations increased the severity of root disease and decreased plant survival and plant fresh weight. While the fungi investigated caused root rot over the range of soil temperatures and moisture conditions of this investigation, the most severe root rot occurred at 10�C, with less at 15 and 25�C, and least at 20�C. Temperature had a marked effect on the disease severity and its effect varied with individual fungi and their combinations, in particular, combinations involving P. irregulare (severest root rot at 10 and 15�C). The most severe root rotting, compared with the control, occurred at 65% WHC, with less at 45% WHC, and least under flooding conditions. There was often a significant interaction between temperature and moisture for the various fungi and fungal combinations tested.

Seasonal comparison of soil temperature and moisture in pits and mounds under vine maple gaps and conifer canopy in a coastal western hemlock forest

1998 ◽  
Vol 78 (2) ◽  
pp. 291-300 ◽  
Author(s):  
Margaret G. Schmidt ◽  
Aynslie E. Ogden ◽  
Kenneth P. Lertzman
Keyword(s):  
Soil Temperature ◽  
Groundwater Table ◽  
Conifer Forest ◽  
Moisture Contents ◽  
Treefall Gaps ◽  
Air Temperatures ◽  
Soil Temperatures ◽  
Soil Climate ◽  
Made In ◽  
Soil Temperature And Moisture

In this study we attempted to determine if vine maple priority gaps show similar trends in temperature and moisture status to those reported in the literature for treefall gaps and whether temperature and moisture status differed between microtopographic positions (pits and mounds). Biweekly measurements of mid-day soil and air temperature, moisture contents at 30-, 50- and 80-cm depths, and depths to the groundwater table were made in pit and mound locations within six vine maple priority gaps paired with six conifer canopy sites. Trends did not follow those found in treefall gaps: vine maple gaps had similar mid-day temperature and moisture status to the surrounding conifer forest. Larger gaps had higher mid-day air temperatures in the summer, higher mid-day soil temperatures in the spring and summer, and greater amounts of throughfall in the spring and summer than smaller gaps. Trends in mid-day soil temperature and moisture status for pit and mound microtopography followed those reported in the literature. Pits were significantly cooler in summer and warmer in winter than mounds and pits were wetter than mounds in all seasons. This study suggests that soil microtopography has an effect on soil climate that overwhelms the influence of vine maple gaps. Key words: Vine maple, canopy gap, soil moisture, soil temperature, microtopography, pits and mounds

YIELD OF BROMEGRASS AND REMOVAL OF NITROGEN, PHOSPHORUS AND POTASSIUM UNDER MODIFIED SOIL-TEMPERATURE FIELD CONDITIONS

1971 ◽  
Vol 51 (2) ◽  
pp. 195-209 ◽  
Author(s):  
A. R. MACK
Keyword(s):  
Soil Temperature ◽  
Moisture Stress ◽  
Seasonal Temperature ◽  
Yield Increase ◽  
Herbage Yield ◽  
Soil Temperatures ◽  
Phosphorus And Potassium ◽  
Major Nutrients ◽  
Warm Soil ◽  
Modified Soil

In a 3-year field experiment with bromegrass grown under low moisture stress (< 2 atm), total herbage yield from unfertilized plots was reduced by 39% when the average seasonal soil temperature (14.1 C at a 50-cm depth) was lowered and maintained at 9.2 C; the yield was increased by 71% when the seasonal temperature was raised and maintained at 25.4 C. This represents a change in yield of 6.8% per 1 C change in the seasonal soil temperature, or a Q10 of 1.3 at 9.2 C. Herbage grown on the warm soils continued throughout the season until fall, but growth on the cool soils was negligible after the first harvest in June. Addition of N, P and K to the soil in the spring reduced the effect of a change in soil temperature on herbage yield (3.7% per 1 C). The amount of the yield increase, however, was similar at all three soil temperatures. In contrast to the effect on herbage yield, root accumulation was much greater in the cool soil (30.7 metric tons per ha, 0 to 30 cm depth) than in the seasonal soil (22.7 MT/ha) or in the warm soil (12.1 MT/ha). An increase in concentration of the major nutrients (N, P, K) in the plants coincided with the greater herbage growth on the warm soil. The changes in uptake for N, P and K per 1 C change of the seasonal temperature were 8.7, 10.4 and 7.1%, respectively, and the associated Q10 values were 1.5, 1.6 and 1.4 at 9.2 C. After growing bromegrass for three years, the amount of NO3-N mineralized for subsequent crops was low in soil from the cool plots but much higher in soil from the warm plots. The relative amounts mineralized varied with incubation conditions.

The temperature and moisture regime of charcoal-enriched land use legacy soils

2020 ◽  
Author(s):  
Anna Schneider ◽  
Florian Hirsch ◽  
Alexander Bonhage ◽  
Alexandra Raab ◽  
Thomas Raab
Keyword(s):  
Thermal Conductivity ◽  
Land Use ◽  
Soil Moisture ◽  
Soil Temperature ◽  
Bulk Density ◽  
Forest Soils ◽  
Moisture Regime ◽  
Seasonal Temperature ◽  
Water Contents ◽  
Soil Temperature And Moisture

&lt;p&gt;The stratigraphy and properties of soils can be significantly altered by past land use, even in areas that have been continuously used for forestry. Soils on relict charcoal hearths (RCHs) are a widespread example of such a pedological legacy of past forest use. RCH soils occur in many forest areas and receive increasing attention as model sites to study long-term effects of soil amendment with biochars, however, their physical properties have hardly been studied. The objective of our study was to characterize the soil temperature and moisture regime of RCH soils through comparison to reference forest soils on sandy substrates in woodlands in Brandenburg, Germany. We combined laboratory analyses of bulk density, pore size distribution, thermal conductivity and saturated hydraulic conductivity with sensor-based monitoring of soil temperature, moisture contents and matric potentials.&amp;#160;&lt;/p&gt;&lt;p&gt;The results of laboratory analysis reveal high soil organic matter (SOM) contents, a low bulk density and high porosity of the RCH substrates. Associated with this RCH specific soil structure, RCHs exhibit clearly lower thermal conductivity. However, the higher total porosity of RCH substrates does not necessarily imply higher water retention and plant-available water contents in the RCH soils than in the topsoil horizons of undisturbed forest soils.&amp;#160; The monitoring results reveal distinct differences between the temperature regimes of the RCH and reference profiles, with the RCH soil exhibiting higher daily and seasonal temperature variations within the topmost horizon, but lower variations in deeper parts of the profiles. Soil moisture monitoring shows higher water contents in RCH soils under relatively wet conditions and lower water contents under dry conditions, and increased spatial variation in soil moisture in RCH soils. Overall, the results show increased spatial and temporal variability of soil temperature and moisture on RCHs, which implies an increased variability in ecological site conditions in historic charcoal production areas.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;

scholarly journals Influence of Soil Temperature and Moisture on Eruptive Germination and Viability of Sclerotia of Sclerotinia minor and S. sclerotiorum

Plant Disease ◽  
2005 ◽  
Vol 89 (1) ◽  
pp. 50-54 ◽  
Author(s):  
M. E. Matheron ◽  
M. Porchas
Keyword(s):  
Soil Temperature ◽  
Germination Rate ◽  
Field Trials ◽  
Sclerotinia Minor ◽  
Production Region ◽  
Mean Temperature ◽  
Soil Temperatures ◽  
History Of ◽  
Dry Soil ◽  
Soil Temperature And Moisture

The effect of soil temperature and moisture on eruptive germination and viability of sclerotia of Sclerotinia minor and S. sclerotiorum in field soil was examined. In two trials at constant temperatures, the proportion of sclerotia of both pathogens that germinated in wet soil ( ≥-0.02 MPa) tended to decrease as soil temperature increased from 15 to 40°C, with no germination of sclerotia of S. minor and S. sclerotiorum detected after 1 and 2 weeks, respectively, at 40°C. In contrast, after 1 to 4 weeks in dry soil ( ≤-100 MPa) at 40°C, germination of sclerotia of S. minor and S. sclerotiorum ranged from 28 to 55% and 42 to 77%, respectively. In field trials, the germination rate of sclerotia of S. minor and S. sclerotiorum after 2 to 8 weeks in irrigated soil on the surface or buried at a depth of 5 cm was significantly lower than that for sclerotia maintained in dry soil at the same depths. On the other hand, after burial at a depth of 10 cm, germination of sclerotia in irrigated and dry soil did not differ significantly after 2 to 8 weeks for S. minor and after 2, 4, and 8 weeks for S. sclerotiorum. For both pathogens, germination of sclerotia from 2 to 8 weeks in irrigated soil with a mean temperature of 32°C was significantly lower than that for sclerotia in irrigated soil with a mean temperature of 26°C. In microplot trials conducted in July and August, no sclerotia of S. minor and S. sclerotiorum germinated after 2 and 3 weeks, respectively, after recovery from flooded soil with mean soil temperatures ranging from 30 to 33°C. A flood irrigation is often applied to fields for salt management during July or August in the Yuma lettuce production region. Results from these studies suggest that maintaining this flooding event for 2 to 3 weeks in fields with a history of lettuce drop caused by S. minor and S. sclerotiorum could significantly reduce the population of viable sclerotia.

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