EFFECT OF SOIL TEMPERATURE ON SEEDLING EMERGENCE

1962 ◽  
Vol 42 (3) ◽  
pp. 481-487 ◽  
Author(s):  
S. Dubetz ◽  
G. C. Russell ◽  
D. T. Anderson
Keyword(s):  
Soil Temperature ◽  
Seedling Emergence ◽  
Herbaceous Species ◽  
Sweet Clover ◽  
Sugar Beets ◽  
Red Fescue ◽  
Wild Oats ◽  
Soil Temperatures ◽  
Rate Of Emergence ◽  
Rough Fescue

Rate and percentage of emergence of 19 native and cultivated herbaceous species were studied at the following soil temperature: 6°, 13°, 18°, and 24 °C. The soil temperatures were held uniformly constant, and emergence data at the end of 5 weeks from four replications in time were obtained. The rate of emergence of all species was greater at 18 °C. than at 6 °C., and of all but five species was greater at 24 °C. than at 18 °C.The percentage of emergence of barley, bromegrass, crested wheatgrass, mustard, oats, peas, spring wheat, and wild oats was not significantly affected by soil temperature. Beans, corn, sugar beets, and sunflowers showed significantly lower emergence percentages at 6 °C. than at the three higher soil temperatures. Alfalfa, creeping red fescue, winter wheat, orchardgrass, rough fescue, sweet clover, and flax emerged best at moderate soil temperatures.

Effects of some crop management practices on reproduction of Meloidogyne javanica on Brassica napus

Nematology ◽  
2002 ◽  
Vol 4 (3) ◽  
pp. 381-386
Author(s):  
Christopher Steel ◽  
John Kirkegaard ◽  
Rod McLeod
Keyword(s):  
Brassica Napus ◽  
Soil Temperature ◽  
Egg Production ◽  
Management Practices ◽  
Seedling Emergence ◽  
Meloidogyne Javanica ◽  
Egg Laying ◽  
Infested Soil ◽  
Young Females ◽  
Soil Temperatures

AbstractThe effects of seed treatments with pesticides, soil temperature at sowing, cutting of plants with and without glyphosate herbicide, root disruption and age of crop at inoculation on reproduction of Meloidogyne javanica on Brassica napus were investigated. When inoculated at sowing, plants grown from fodder rape cv. Rangi seed treated with fenamiphos (0.35 g a.i. per 100 g) and from fodder swede cv. Highlander seed with a coating including imidacloprid had fewer galls than plants from seed untreated or treated with omethoate (0.7 g a.i. per 100 g). When nematode inoculation was delayed until 4 weeks after sowing, omethoate and the imadacloprid treatments had no effect while fenamiphos (0.7 g a.i. per 100 g seed) suppressed galling but also impaired seedling emergence and induced chlorosis. Green manure rape plants cvs Rangi and Humus transplanted into infested soil in the field in mid-autumn (soil temperature 17°C) remained nematode and gall-free, but tomato cv. Grosse Lisse plants were heavily galled. All three cultivars were gall-free when transplanted and grown in early winter (soil temperatures 8-14°C). Cutting off the tops of cv. Rangi plants at from 6 to 11 weeks after sowing and inoculation had no effect on egg production compared to that on intact plants. Predominant nematode stages in cut plants ranged from developing juveniles to egg-laying females. Application of glyphosate to freshly cut stems had no effect on egg production at any stage. Infesting soil with roots of cv. Rangi, finely chopped while nematodes in them were still juveniles, resulted in a low incidence of infection of bioassay tomato plants compared with infesting soil with rape roots chopped later, when females and females with eggs predominated. Young females in tomato roots laid eggs despite fine chopping of the roots. When cv. Rangi plants were inoculated at 3, 5 and 7 weeks after sowing, the 7-week-old plants were the least invaded and fewer eggs were produced on the 5 and 7-week-old plants than on the 3-week-old ones.

EFFECTS OF SOIL TEMPERATURE ON THE PHYTOTOXICITY OF TRIFLURALIN TO WILD OATS

1980 ◽  
Vol 60 (3) ◽  
pp. 929-938 ◽  
Author(s):  
A. L. DARWENT
Keyword(s):  
Soil Temperature ◽  
Shoot Growth ◽  
Avena Fatua ◽  
Controlled Environment ◽  
Wild Oat ◽  
Wild Oats ◽  
Soil Temperatures

Experiments were conducted in the field and in controlled environment chambers at Beaverlodge, Alberta to determine the influence of soil temperature on the phytotoxicity of trifluralin (α,α,α-trifluoro-2,6-dinitro-N, N-dipropyl-p-toluidine) to wild oats (Avena fatua L.). In the field trifluralin reduced wild oat emergence the most in early May when soil temperatures were lowest. As soil temperatures increased in May, the effectiveness of trifluralin in reducing wild oat emergence declined. In controlled environment studies, the effectiveness of trifluralin in reducing wild oat shoot growth was greatest at 4 °C. At 7.5 °C, the effectiveness of trifluralin in reducing wild oat shoot growth declined. However, at both 10 and 20 °C, small increases in trifluralin phytotoxicity occurred. Exposure of wild oat shoots to trifluralin vapors at 7.5 and 20 °C indicated decreased shoot growth of wild oats at 7.5 °C but increased volatilization of trifluralin at 20 °C. Thus, the lack of any major differences in the effectiveness of trifluralin in reducing wild oat shoot growth at temperatures from 7.5 to 20 °C may be due to the counteraction of these two phenomena.

The effects of early season soil temperatures on emergence of summer crops on the north-western plains of NSW

1971 ◽  
Vol 11 (48) ◽  
pp. 39 ◽  
Author(s):  
TE Launders
Keyword(s):  
Soil Temperature ◽  
Pearl Millet ◽  
Early Season ◽  
Related Data ◽  
The North ◽  
Temperature Requirement ◽  
Soil Temperatures ◽  
Emergence Percentage ◽  
Rate Of Emergence ◽  
Lower Temperature

The influence of early season soil temperatures on the extent and rate of emergence of five summer crops was examined using four sowings at weekly intervals between late September and late October. The crops were maize, grain sorghum, pearl millet, and two forage sorghums. Increasing soil temperature reduced the interval between sowing and first emergence, and gave variable results for the interval between first and final emergence. Percentage emergence of maize was high at all sowings, whereas that of all three sorghums was low at sowings with soil temperatures at 4 inches of below 65�F, but did not differ significantly between sowings at temperatures above 65�F. Emergence of pearl millet improved with each later sowing, but differences were not significant. Rate of emergence was accelerated by rising soil temperatures in the four days after first emergence, but subsequent effects after four days were generally minimal. Maize appeared to have a lower temperature requirement for emergence than grain and forage sorghums, which, in turn, showed a lower temperature requirement than pearl millet. From the results and other related data, it seems that maize can be sown with reasonable safety when four inch depth soil temperatures are 59� to 64�F (expected in late September), sorghums (both grain and forage) when this temperature is 65� to 69�F (expected in early- to mid-October), and pearl millet when it is 68� to 72�F (expected in early- to mid-November). The results support the concept of soil temperature being the best criterion to determine a safe time for early season sowing of summer crops.

scholarly journals Emergence of Sugar Beet Seedlings at Low Soil Temperature following Seed Soaking and Priming

HortScience ◽  
1993 ◽  
Vol 28 (1) ◽  
pp. 31-32 ◽  
Author(s):  
Glen Murray ◽  
Jerry B. Swensen ◽  
John J. Gallian
Keyword(s):  
Polyethylene Glycol ◽  
Sugar Beet ◽  
Soil Temperature ◽  
Beta Vulgaris ◽  
Seed Treatment ◽  
Laboratory Experiments ◽  
Seedling Emergence ◽  
Field Soil ◽  
Low Field ◽  
Soil Temperatures

Seedling emergence from primed and nonprimed sugar beet seed (Beta vulgaris L.) was studied for 3 years under field conditions near Kimberly, Idaho, and compared with germination or emergence under controlled laboratory conditions. Maximum seedling emergence did not vary with seed treatment in spite of low field soil temperatures. Time to 50% of maximum emergence was significantly less for seed primed with polyethylene glycol 8000 than for nonprimed seed in only 1 of 3 years. Seed soaked in 30C water for 24 h performed similarly to nontreated seed in the field, but their maximum emergence was significantly improved compared with primed seed in one of two laboratory experiments. Time to 50% of maximum germination was improved by priming with or without a warm water soak in one of the two laboratory experiments.

Effects of laboratory germination, soil temperature and moisture content on the emergence of spring wheat

1986 ◽  
Vol 107 (2) ◽  
pp. 431-438 ◽  
Author(s):  
E. M. Khah ◽  
R. H. Ellis ◽  
E. H. Roberts
Keyword(s):  
Soil Moisture ◽  
Moisture Content ◽  
Soil Temperature ◽  
Linear Function ◽  
Spring Wheat ◽  
Sandy Loam ◽  
Seedling Emergence ◽  
Triticum Aestivum L ◽  
Obvious Effect ◽  
Soil Temperatures

SummaryIn field investigations in a sandy-loam soil, probit percentage seedling emergence of commercial and aged seed lots of spring wheat (Triticum aestivum L., cv. Timmo) was a positive linear function of probit percentage laboratory germination and mean soil temperature and a negative linear function of percentage soil moisture content over the ranges 12·1–15·5% moisture content and 7·0–11·0 °C. In a laboratory investigation using the same soil a similar form of relationship was observed in six lots over a range of constant soil moisture contents between 10 and 18% and at constant soil temperatures of 8 and 20 °C. In all cases there was no interaction between any of these determinants of seedling emergence.Linear relationships between the mean rate of seedling emergence in the field (i.e. reciprocal of mean emergence time) and probit percentage laboratory germination and mean soil temperature were shown, but there was no obvious effect of mean scil moisture content between 12·1 and 15·5% on rate of field emergence. Seed lots of different percentage laboratory germination had the same base tsmperature for emergence (1·9 °C): differences between seed lots in mean emergence rate were due to different thermal time (day-degree) requirements for emergence; the thermal times required were a function of probit percentage germination in a standard laboratory test. The implications of these results in providing better advice on sowing rates are discussed.

Effect of tillage and corn on pigweed (Amaranthusspp.) seedling emergence and density

Weed Science ◽  
1997 ◽  
Vol 45 (1) ◽  
pp. 120-126 ◽  
Author(s):  
Joseph O. E. Oryokot ◽  
Stephen D. Murphy ◽  
Clarence J. Swanton
Keyword(s):  
Soil Temperature ◽  
Seedling Emergence ◽  
Soil Surface ◽  
Seedling Density ◽  
Weed Species ◽  
No Till ◽  
Prior Constraint ◽  
Soil Temperatures ◽  
Management Recommendations ◽  
Moldboard Plow

We studied the effect of no-till, chisel, and moldboard plow and the presence or absence of corn on soil temperature, moisture and, subsequently, the emergence phenology and density of pigweed seedlings at 2 sites from 1993 to 1995 inclusively. Tillage significantly affected the phenology of pigweed seedling emergence only during a June drought at one site in 1994. Soil temperature and moisture, measured at 2.5-cm depths, also were unaffected by tillage. Weed phenology is usually earlier in no-till because more seeds are located closer to the surface (< 5 cm deep) in no-till, thereby reducing the delay in penetrating through the soil, and because soil temperatures and moisture are nearer the germination and emergence optima. However, pigweed seedlings are already physiologically restricted to germination depths of less than 2.5 cm regardless of tillage; therefore, this prior constraint eliminated any potential differences in emergence phenologies caused by tillage. The presence or absence of corn also did not affect soil temperatures, soil moisture, or pigweed seedling emergence phenologies. Pigweed seedling density was significantly higher in no-till; this may have been caused by increased numbers of seeds near the soil surface in no-till. The presence or absence of corn did not affect pigweed seedling density; the lack of a significant effect probably reflects high variances in density. Although necessary for most weed species, tillage may be a less important factor to consider in predicting pigweed population dynamics and subsequent management recommendations.

scholarly journals Soil Temperature Mediated Seedling Emergence and Field Establishment in Bentgrass Species and Cultivars during Spring in the Northeastern United States

2020 ◽  
pp. 1-11
Author(s):  
J. Scott Ebdon ◽  
Michelle DaCosta
Keyword(s):  
Soil Temperature ◽  
Perennial Ryegrass ◽  
Unit Area ◽  
Seedling Emergence ◽  
Creeping Bentgrass ◽  
Experimental Period ◽  
Early Spring ◽  
Golf Greens ◽  
Soil Temperatures ◽  
Mature Stands

Reestablishment of damaged golf greens and fairways planted to creeping bentgrass (Agrostis stolonifera), colonial bentgrass (A. capillaris), and velvet bentgrass (A. canina) is a common practice following winter injuries. Identifying bentgrass species (Agrostis sp.) and cultivars with the potential to establish under low soil temperatures would be beneficial to achieving more mature stands earlier in the spring. Twelve bentgrass cultivars, including seven cultivars of creeping bentgrass (007, 13-M, Declaration, L-93, Memorial, Penncross, and T-1), two colonial bentgrass cultivars (Capri and Tiger II), and three velvet bentgrass cultivars (Greenwich, SR-7200, and Villa), along with ‘Barbeta’ perennial ryegrass (Lolium perenne) were evaluated for grass cover in the field during early spring. Bentgrass species and cultivars were seeded in the field at the same seed count per unit area. Soil temperatures were monitored in unseeded check plots from initial planting date on 8 Apr. to termination on 29 May 2013. Soil temperatures increased linearly during the 52-day experimental period from 4.7 to 23.5 °C. All species and cultivars emerged at ≈10 °C soil temperature. Bentgrass species and cultivars varied only 2 to 3 days in their initial seedling emergence, while days varied among bentgrasses from 5.5 days (to 10% cover) to 8.6 days (to 90% cover). All velvet bentgrass cultivars required higher soil temperatures (13.6 °C) and more time (26 days) following initial seedling emergence to establish to 90% cover in the early spring. Creeping bentgrass cultivars 007, 13-M, and Memorial, along with colonial bentgrass cultivars Capri and Tiger II, were statistically equal to ‘Barbeta’ perennial ryegrass in their capacity after seedling emergence to achieve faster cover at lower soil temperatures. Heavier (larger) bentgrass seed was associated with faster cover during the early stages of establishment, but seed size was uncorrelated with establishment during later stages from 50% to 90% cover.

scholarly journals Simulation of Daily Mean Soil Temperatures for Agricultural Land Use Considering Limited Input Data

Atmosphere ◽  
2021 ◽  
Vol 12 (4) ◽  
pp. 441
Author(s):  
Philipp Grabenweger ◽  
Branislava Lalic ◽  
Miroslav Trnka ◽  
Jan Balek ◽  
Erwin Murer ◽  
...  
Keyword(s):  
Soil Temperature ◽  
Input Data ◽  
Agricultural Land ◽  
Soil Column ◽  
Soil Conditions ◽  
Snow Layer ◽  
Time Step ◽  
Soil Temperatures ◽  
Dimensional Simulation ◽  
Limited Input Data

A one-dimensional simulation model that simulates daily mean soil temperature on a daily time-step basis, named AGRISOTES (AGRIcultural SOil TEmperature Simulation), is described. It considers ground coverage by biomass or a snow layer and accounts for the freeze/thaw effect of soil water. The model is designed for use on agricultural land with limited (and mostly easily available) input data, for estimating soil temperature spatial patterns, for single sites (as a stand-alone version), or in context with agrometeorological and agronomic models. The calibration and validation of the model are carried out on measured soil temperatures in experimental fields and other measurement sites with various climates, agricultural land uses and soil conditions in Europe. The model validation shows good results, but they are determined strongly by the quality and representativeness of the measured or estimated input parameters to which the model is most sensitive, particularly soil cover dynamics (biomass and snow cover), soil pore volume, soil texture and water content over the soil column.

scholarly journals A simple model for predicting soil temperature in snow-covered and seasonally frozen soil: model description and testing

2004 ◽  
Vol 8 (4) ◽  
pp. 706-716 ◽  
Author(s):  
K. Rankinen ◽  
T. Karvonen ◽  
D. Butterfield
Keyword(s):  
Heat Capacity ◽  
Simple Model ◽  
Soil Temperature ◽  
Specific Heat ◽  
Specific Heat Capacity ◽  
Frozen Soil ◽  
Model Description ◽  
Freezing And Thawing ◽  
Catchment Scale ◽  
Soil Temperatures

Abstract. Microbial processes in soil are moisture, nutrient and temperature dependent and, consequently, accurate calculation of soil temperature is important for modelling nitrogen processes. Microbial activity in soil occurs even at sub-zero temperatures so that, in northern latitudes, a method to calculate soil temperature under snow cover and in frozen soils is required. This paper describes a new and simple model to calculate daily values for soil temperature at various depths in both frozen and unfrozen soils. The model requires four parameters: average soil thermal conductivity, specific heat capacity of soil, specific heat capacity due to freezing and thawing and an empirical snow parameter. Precipitation, air temperature and snow depth (measured or calculated) are needed as input variables. The proposed model was applied to five sites in different parts of Finland representing different climates and soil types. Observed soil temperatures at depths of 20 and 50 cm (September 1981–August 1990) were used for model calibration. The calibrated model was then tested using observed soil temperatures from September 1990 to August 2001. R2-values of the calibration period varied between 0.87 and 0.96 at a depth of 20 cm and between 0.78 and 0.97 at 50 cm. R2-values of the testing period were between 0.87 and 0.94 at a depth of 20cm, and between 0.80 and 0.98 at 50cm. Thus, despite the simplifications made, the model was able to simulate soil temperature at these study sites. This simple model simulates soil temperature well in the uppermost soil layers where most of the nitrogen processes occur. The small number of parameters required means that the model is suitable for addition to catchment scale models. Keywords: soil temperature, snow model

scholarly journals Quality control of 10-min soil temperatures data at RMI

2015 ◽  
Vol 12 (1) ◽  
pp. 23-30 ◽  
Author(s):  
C. Bertrand ◽  
L. González Sotelino ◽  
M. Journée
Keyword(s):  
Quality Control ◽  
Soil Temperature ◽  
Bare Soil ◽  
Climate Conditions ◽  
Air Temperatures ◽  
Temperature Observation ◽  
Soil Temperatures ◽  
Different Depths ◽  
Temperature Records ◽  
Energy Processes

Abstract. Soil temperatures at various depths are unique parameters useful to describe both the surface energy processes and regional environmental and climate conditions. To provide soil temperature observation in different regions across Belgium for agricultural management as well as for climate research, soil temperatures are recorded in 13 of the 20 automated weather stations operated by the Royal Meteorological Institute (RMI) of Belgium. At each station, soil temperature can be measured at up to 5 different depths (from 5 to 100 cm) in addition to the bare soil and grass temperature records. Although many methods have been developed to identify erroneous air temperatures, little attention has been paid to quality control of soil temperature data. This contribution describes the newly developed semi-automatic quality control of 10-min soil temperatures data at RMI.

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