Effect of boron on clubroot of canola in organic and mineral soils and on residual toxicity to rotational crops

2014 ◽  
Vol 94 (1) ◽  
pp. 109-118 ◽  
Author(s):  
A. Deora ◽  
B. D. Gossen ◽  
S. F. Hwang ◽  
D. Pageau ◽  
R. J. Howard ◽  
...  
Keyword(s):  
Plasmodiophora Brassicae ◽  
Mineral Soil ◽  
Organic Soil ◽  
Field Trials ◽  
Growth And Yield ◽  
Broadcast Application ◽  
Residual Toxicity ◽  
Negative Effect ◽  
Soil Site ◽  
Mineral Soils

Deora, A., Gossen, B. D., Hwang, S. F., Pageau, D., Howard, R. J., Walley, F. and McDonald, M. R. 2014. Effect of boron on clubroot of canola in organic and mineral soils and on residual toxicity to rotational crops. Can. J. Pant Sci. 94: 109–118. Application of boron (B) has been reported to reduce clubroot severity in various Brassica spp., but residual B can have phytotoxic effects on other crops in the rotation. The objective of this study was to test the efficacy of broadcast application of B for clubroot suppression in canola (B. napus) and the effect of residual B on wheat, barley, field pea and canola. Field trials to assess clubroot suppression by B at various rates (1 to 64 kg B ha−1) were conducted in organic (Ontario) and mineral soils (Alberta, Quebec) heavily infested with Plasmodiophora brassicae in 2011 and 2012. Phytotoxicity was not observed in canola until applications rates exceeded 48 kg B ha−1. Boron did not reduce clubroot incidence at any site, irrespective of rate, and only reduced severity at the organic soil site at 6 wk after seeding. There was a small increase in shoot weight and yield of canola with increasing B application rates at the organic soil site. The potential phytotoxicity of residual B (4 to 16 kg B ha−1) was assessed in mineral soils in Ontario and Saskatchewan in 2012. Toxicity symptoms were noted initially in most of the crops, but seedlings recovered quickly and there was no significant reduction in fresh weight at harvest or seed yield of most of the cultivars. The present study indicates that pre-plant broadcast application of B delays clubroot development and increases vegetative growth and yield compared with non-treated plants in organic soil. Also, even high residual rates (16 kg ha−1) of application are unlikely to have a negative effect on crops in rotation in mineral soil. However, the effect of B application on canola yield found in this study was not sufficient to justify application for commercial canola production, even where clubroot is prevalent.

scholarly journals Effect of Host Resistance and Fungicide Application on Clubroot Pathotype 6 in Green Cabbage and Napa Cabbage

2012 ◽  
Vol 22 (3) ◽  
pp. 311-319 ◽  
Author(s):  
Catarina Saude ◽  
Alan McKeown ◽  
Bruce D. Gossen ◽  
Mary Ruth McDonald
Keyword(s):  
Brassica Oleracea ◽  
Brassica Rapa ◽  
Host Resistance ◽  
Plasmodiophora Brassicae ◽  
Field Trials ◽  
Organic Soils ◽  
Southern Ontario ◽  
Clubroot Resistance ◽  
Mineral Soils ◽  
Standard Cultivar

Field trials were conducted to evaluate resistance to clubroot (Plasmodiophora brassicae, pathotype 6) in green cabbage (Brassica oleracea var. capitata) and napa cabbage (Brassica rapa ssp. pekinensis) at sites in southern Ontario in 2009 and 2010. The reaction of green cabbage cultivars Kilaton, Tekila, Kilaxy, and Kilaherb and the commercial standard cultivars, Bronco or Atlantis, were evaluated on organic (two site-years) and mineral soils (two site-years) that were naturally infested with the clubroot pathogen. In addition, fluazinam fungicide was drench applied to one treatment of the commercial standard cultivar immediately after transplanting. The napa cabbage cultivars Yuki, Deneko, Bilko, and Mirako (in 2009) and Emiko, Mirako, Yuki, and China Gold (in 2010) were evaluated only on organic soils (two site-years). At harvest, the roots of each plant were assessed for clubroot incidence and severity. Also, plant and head characteristics of the resistant green cabbage cultivars were evaluated at one site in 2010. The green cabbage cultivars Kilaton, Tekila, Kilaxy, and Kilaherb were resistant to pathotype 6 (0% to 3.8% incidence), but ‘Bronco’ was susceptible (64% to 100% incidence). Application of fluazinam reduced clubroot severity on ‘Bronco’ by 6% at one of three sites. Resistance was more effective in reducing clubroot than application of fluazinam. Plant and head characteristics of the resistant cultivars were similar to those of ‘Bronco’ treated with fluazinam. Napa cabbage cultivars Yuki, Deneko, Bilko, Emiko, and China Gold were resistant to clubroot (0% to 13% incidence), and ‘Mirako’ was highly susceptible (87% to 92% incidence). We conclude that the clubroot resistance available in several cultivars of green and napa cabbage was effective against P. brassicae pathotype 6.

scholarly journals Organic Matter Causes Chemical Pollutant Dissipation Along With Adsorption and Microbial Degradation

2021 ◽  
Vol 9 ◽  
Author(s):  
A. Vilhelmiina Harju ◽  
Ilkka Närhi ◽  
Marja Mattsson ◽  
Kaisa Kerminen ◽  
Merja H. Kontro
Keyword(s):  
Organic Matter ◽  
Microbial Degradation ◽  
Mineral Soil ◽  
Organic Soil ◽  
Organic Soils ◽  
First Response ◽  
Chemical Pollutant ◽  
Mineral Soils ◽  
Soil And Sediment

Views on the entry of organic pollutants into the organic matter (OM) decaying process are divergent, and in part poorly understood. To clarify these interactions, pesticide dissipation was monitored in organic and mineral soils not adapted to contaminants for 241 days; in groundwater sediment slurries adapted to pesticides for 399 days; and in their sterilized counterparts with and without peat (5%) or compost-peat-sand (CPS, 15%) mixture addition. The results showed that simazine, atrazine and terbuthylazine (not sediment slurries) were chemically dissipated in the organic soil, and peat or CPS-amended soils and sediment slurries, but not in the mineral soil or sediment slurries. Hexazinone was chemically dissipated best in the peat amended mineral soil and sediment slurries. In contrast, dichlobenil chemically dissipated in the mineral soil and sediment slurries. The dissipation product 2,6-dichlorobenzamide (BAM) concentrations were lowest in the mineral soil, while dissipation was generally poor regardless of plant-derived OM, only algal agar enhanced its chemical dissipation. Based on sterilized counterparts, only terbutryn appeared to be microbially degraded in the organic soil, i.e., chemical dissipation of pesticides would appear to be utmost important, and could be the first response in the natural cleansing capacity of the environment, during which microbial degradation evolves. Consistent with compound-specific dissipation in the mineral or organic environments, long-term concentrations of pentachloroaniline and hexachlorobenzene were lowest in the mineral-rich soils, while concentrations of dichlorodiphenyltrichloroethane (DTT) and metabolites were lowest in the organic soils of old market gardens. OM amendments changed pesticide dissipation in the mineral soil towards that observed in the organic soil; that is OM accelerated, slowed down or stopped dissipation.

OXYGEN FLUX MEASUREMENTS IN ORGANIC SOIL

1980 ◽  
Vol 60 (4) ◽  
pp. 641-650 ◽  
Author(s):  
JAMES A. CAMPBELL
Keyword(s):  
Applied Voltage ◽  
Mineral Soil ◽  
Organic Soil ◽  
Oxygen Flux ◽  
Organic Soils ◽  
Wide Range ◽  
Effective Voltage ◽  
Flux Measurements ◽  
Mineral Soils ◽  
Almost All

Many measurements of oxygen flux in mineral soils have been reported; however, few such measurements have been made in organic soil. Almost all reported measurements of oxygen flux are at constant applied voltage, despite criticism of this technique, possibly due to the complexity of existing techniques for measuring oxygen flux at effective voltage. Equipment suitable for measuring oxygen flux at applied and effective voltage in organic soil was designed, and simplified techniques were developed and tested. As reported for mineral soils, soil resistance is relatively constant spatially and with depth in individual soils. Limited poisoning of the platinum electrode surface occurred after long periods of time and, contrary to previous assumptions, cannot be detected by erratic readings. Unlike mineral soil, the amperage-voltage slopes are constant over a wide range of organic soils, simplifying the technique for estimating oxygen flux at constant effective volatage. Comparison of simultaneous measurements of oxygen flux at constant and effective voltage indicates that oxygen flux measurements at effective voltage were twice those at applied voltage and strongly correlated (r2 = 0.96, n = 22).

scholarly journals A new approach to simulate peat accumulation, degradation and stability in a global land surface scheme (JULES vn5.8_accumulate_soil)

2021 ◽  
Author(s):  
Sarah E. Chadburn ◽  
Eleanor J. Burke ◽  
Angela V. Gallego-Sala ◽  
Noah D. Smith ◽  
M. Syndonia Bret-Harte ◽  
...  
Keyword(s):  
Soil Carbon ◽  
Land Surface ◽  
Organic Material ◽  
Mineral Soil ◽  
Organic Soil ◽  
Organic Layer ◽  
New Approach ◽  
Land Surface Scheme ◽  
Mineral Soils ◽  
Surface Scheme

Abstract. Peatlands have often been neglected in Earth System Models (ESMs). Where they are included, they are usually represented via a separate, prescribed grid cell fraction that is given the physical characteristics of a peat (highly organic) soil. However, in reality soils vary on a spectrum between purely mineral soil (no organic material), and purely organic soil, typically with an organic layer of variable thickness overlying mineral soil below. They are also dynamic, with organic layer thickness and its properties changing over time. Neither the spectrum of soil types nor their dynamic nature can be captured by current ESMs. Here we present a new version of an ESM land surface scheme (Joint UK Land Environment Simulator, JULES) where soil organic matter accumulation - and thus peatland formation, degradation and stability – is integrated in the vertically-resolved soil carbon scheme. We also introduce the capacity to track soil carbon age as a function of depth in JULES, and compare this to measured peat age-depth profiles. This scheme simulates dynamic feedbacks between the soil organic material and its thermal and hydraulic characteristics. We show that draining the peatlands can lead to significant carbon loss along with soil compaction and changes in peat properties. However, negative feedbacks can lead to the potential for peatlands to rewet themselves following drainage. These ecohydrological feedbacks can also lead to peatlands maintaining themselves in climates where peat formation would not otherwise initiate in the model, i.e. displaying some degree of resilience. The new model produces similar results to the original model for mineral soils, and realistic profiles of soil organic carbon for peatlands. In particular the best performing configurations had root mean squared error (RMSE) in carbon density for peat sites of 7.7–16.7 kgC m−3 depending on climate zone, when compared against typical peat profiles based on 216 sites from a global dataset of peat cores. This error is considerably smaller than the soil carbon itself (around 30–60 kgC m−3) and reduced by 35–80 % compared with standard JULES. The RMSE at mineral soil sites is also smaller in JULES-Peat than JULES itself (reduced by ~30–50 %). Thus JULES-Peat can be used as a complete scheme that simulates both organic and mineral soils. It does not require any additional input data and introduces minimal additional variables to the model. This provides a new approach for improving the simulation of organic and peatland soils, and associated carbon-cycle feedbacks in ESMs, which other land surface models could follow.

scholarly journals The effect of soil type and soil additives on the selected growth parameters and yield of flowerheads of Calendula officinalis L.

2016 ◽  
Vol 62 (2) ◽  
pp. 17-30 ◽  
Author(s):  
Karolina Ratajczak ◽  
Hana Sulewska ◽  
Grażyna Szymańska ◽  
Agnieszka Wolna-Maruwka ◽  
Agnieszka Faligowska
Keyword(s):  
Growth Parameters ◽  
Mineral Soil ◽  
Organic Soil ◽  
Growth And Yield ◽  
Soil Conditions ◽  
Control Group ◽  
Order Factor ◽  
Soil Additives ◽  
Calendula Officinalis L ◽  
Soil Additive

SummaryIntroduction:Soil additives, which usually contain nutrients and microorganism, can improve soil conditions for plants. There are still few papers dedicated to the application of soil additives in herb plants, especially in calendula.Objective:The aim of the study was to determine the effect of selected soil additives on growth and yield of calendula.Methods:In a pot experiment first order factor was a type of soil: mineral soil with straw, mineral soil and organic soil. The second order factor was soil additive: control, UG Max, EM1 and PRP SOL.Results:The application of UG Max and PRP SOL increased the yield of dry matter of flowerheads by respectively 48.1% and 46.3% in comparison with the control group.Conclusions:UG Max and PRP SOL proved to be the most useful soil additive for calendula growing. The effect of UG Max and PRP SOL was particularly good on organic soil.

scholarly journals Abundance of the Sugarcane Borer (Lepidoptera: Crambidae) and Foraging Ants (Hymenoptera: Formicidae) in Sugarcane Grown on Organic and Mineral Soils in Florida

2020 ◽  
Vol 49 (2) ◽  
pp. 473-481
Author(s):  
Erik L Roldán ◽  
Julien M Beuzelin ◽  
Matthew T VanWeelden ◽  
Ronald H Cherry
Keyword(s):  
Soil Type ◽  
Solenopsis Invicta ◽  
Mineral Soil ◽  
Organic Soil ◽  
Organic Soils ◽  
Red Imported Fire Ant ◽  
Sugarcane Borer ◽  
Parasitism Rates ◽  
Solenopsis Invicta Buren ◽  
Mineral Soils

Abstract A study was conducted in Florida to determine sugarcane borer, Diatraea saccharalis (F.), injury and infestation levels in sugarcane (Saccharum spp. hybrids), D. saccharalis parasitism rates, and ant foraging activity in 32 commercial fields as affected by soil type (shallow organic vs deep organic vs mineral). In 2017 and 2018, each field was sampled four times during the summer for D. saccharalis by inspecting 100 sugarcane stalks and for foraging ants using plastic tubes baited with hot dog at 12 locations. One non-parasitized D. saccharalis larva was collected in 2017 and in 2018 out of 12,100 and 12,600 stalks sampled, respectively. Additional sampling of 50 stalks per field in October showed that 0.6% (2017) and 0.1% (2018) of the sugarcane stalks had bored internodes, and one Cotesia flavipes (Cameron) (Hymenoptera: Braconidae) cocoon mass was observed. Seven ant species foraged in sugarcane fields, including the red imported fire ant, Solenopsis invicta Buren, which was the most abundant ant. Solenopsis invicta was not affected by soil type; however, sugarcane fields on shallow organic soils might represent a more suitable environment. The third most abundant foraging ant, Nylanderia bourbonica (Forel), was more abundant in mineral soil fields than in shallow and deep organic soil fields. Results suggest that D. saccharalis population levels in Florida sugarcane are extremely low under current production conditions regardless of soil type. In addition, the observation of C. flavipes, S. invicta, and six other ant species suggest that biological control contributes to these low D. saccharalis population levels.

Adsorption of dissolved nitrogen by forest mineral soils

2009 ◽  
Vol 39 (12) ◽  
pp. 2381-2390 ◽  
Author(s):  
D.N. Kothawala ◽  
T.R. Moore
Keyword(s):  
Soil Properties ◽  
Dissolved Organic Nitrogen ◽  
Organic Nitrogen ◽  
Mineral Soil ◽  
Organic Soil ◽  
Nutrient Sources ◽  
Dissolved Nitrogen ◽  
Soil Solutions ◽  
Mineral Soils ◽  
Similar Soil

Dissolved nitrogen (N) species, including ammonium (NH4+-N), nitrate (NO3–-N), and dissolved organic nitrogen (DON), are important nutrient sources in soils. The mobility of DON and NH4+-N in soil solutions is influenced by abiotic adsorption to mineral soil particle surfaces. We determined relationships between soil properties and their ability to adsorb NH4+-N, NO3–-N, and DON, using batch experiments. A range of 41 mineral horizons was collected from across Canada, including Podzols, Brunisols, Luvisols, Gleysols, and an organic soil. The adsorption of DON and dissolved organic carbon (DOC) were positively correlated (R2 = 0.86), and both were best explained by the amount of iron and aluminum associated with poorly crystalline phases. Adsorption of NH4+-N was strongest in Gleysols and Luvisols, while adsorption of NO3–-N was weak in all soils. A reduction in the DOC:DON ratio was observed for most mineral horizons (89%) after equilibration from an original ratio of 35:1. Mineral horizons with a net desorption of DON had a significantly greater reduction in the final DOC:DON ratios than horizons with a net adsorption of DON. The results from this study found that while similar soil properties could predict DOC and DON adsorption, DON was slightly more mobile than DOC.

scholarly journals Field Infection of Virus-Free Sugarcane by Sugarcane Yellow Leaf Virus and Effect of Yellow Leaf on Sugarcane Grown on Organic and on Mineral Soils in Florida

Plant Disease ◽  
2019 ◽  
Vol 103 (9) ◽  
pp. 2367-2373 ◽  
Author(s):  
Wardatou Boukari ◽  
Claudia Kaye ◽  
Chunyan Wei ◽  
Martha Hincapie ◽  
Chris LaBorde ◽  
...  
Keyword(s):  
Soil Type ◽  
Mineral Soil ◽  
Organic Soil ◽  
Yellow Leaf ◽  
Sugarcane Yellow Leaf Virus ◽  
Infected Seed ◽  
Virus Prevalence ◽  
Mineral Soils ◽  
The Impact ◽  
Leaf Virus

Sugarcane yellow leaf virus (SCYLV), the causal agent of yellow leaf, is widespread in Florida. Two field trials were set up, one on organic soil and one on mineral soil, to investigate the rate and timing of sugarcane infection by SCYLV under field conditions and the effect of the virus on yield. Each trial consisted of plots planted with healthy or SCYLV-infected seed cane of two commercial cultivars. Virus prevalence varied from 83 to 100% in plots planted with infected seed cane regardless of cultivar, location, and crop season. On organic soil, plants of virus-free plots became progressively infected in plant cane and first ratoon crops. On mineral soil, healthy sugarcane became initially infected in the first ratoon crop. After three crop seasons, the highest SCYLV prevalence rates were 33 and 7% on organic and mineral soils, respectively. No significant negative effect of SCYLV on yield was found in plant cane crop regardless of cultivar and soil type. However, yield reductions in ratoon crops varied from nonsignificant to 27% depending on cultivar and soil type. Low virus prevalence observed after three crop seasons suggested that planting virus-free seed cane should limit the impact of SCYLV on sugarcane production in Florida.

INFLUENCE OF SOIL MOISTURE, SOIL pH, AND LIMING SOURCES ON THE INCIDENCE OF CLUBROOT, THE GERMINATION AND GROWTH OF CABBAGE PRODUCED IN MINERAL AND ORGANIC SOILS UNDER CONTROLLED CONDITIONS

1978 ◽  
Vol 58 (1) ◽  
pp. 45-53 ◽  
Author(s):  
HERMAN A. HAMILTON ◽  
RENÉ CRÊTE
Keyword(s):  
Soil Moisture ◽  
Soil Ph ◽  
Soil Acidity ◽  
Plasmodiophora Brassicae ◽  
Mineral Soil ◽  
Organic Soil ◽  
Inhibitory Effect ◽  
Organic Soils ◽  
Plant Nutrient ◽  
Germination And Growth

Under growth chamber conditions, the influence of soil moisture, soil pH, and liming sources on the germination, yield and infection of cabbage by Plasmodiophora brassicae Wor. was studied in artificially infested mineral and organic soils. Clubroot infection occurred at moisture levels as low as 9 and 60% in the mineral and organic soils, respectively. The growth of cabbage and the reduction of the incidence of clubroot were more dependent on liming source than on soil pH. Soil pH adjustment to effect complete clubroot control was invariably deleterious to cabbage growth. It was established for the organic soil that the effect of calcium hydroxide was important in correcting soil acidity as well as supplying calcium as an essential plant nutrient for cabbage. In addition, there was evidence that correction of the soil acidity favored clubroot development, but simultaneously the Ca ion had an inhibitory effect on the disease organism. On the mineral soil, Mg sources producing a soil pH not normally considered deleterious to plants affected the germination and ultimate yield of cabbage.

Combined application of ammonium nitrate and goat manure: Effects on soil nutrients availability, Okra performance and sustainable food security

2021 ◽  
Vol 1 (1) ◽  
pp. 021-028
Author(s):  
Mukhtar Iderawumi ABDULRAHEEM ◽  
Sulaimon Abidemi LAWAL
Keyword(s):  
Block Design ◽  
Chemical Properties ◽  
Soil Nutrient ◽  
Field Trials ◽  
Sub Saharan Africa ◽  
Growth And Yield ◽  
Urea Fertilizer ◽  
Traditional System ◽  
Land Preparation ◽  
Goat Manure

Many see organic agriculture as the most sustainable form of farming and as the paradigm for global food production in the future. One of the solutions to food insecurity and malnutrition in Sub-Saharan Africa is to promote local crops, encourage the use of locally source materials as amendment, improve their traditional system of production, and so diversify subsistence crop. The major reasons are the lack of knowledge and skill in land preparation and agronomic practices, weather uncertainties, pest outbreak and above all the use of fertilizer. Hence, this research will be carried out to investigate the effects of integrated application of Urea fertilizer and Goat Manure on soil Nutrient Availability and Okra performance. Field trials were conducted with four treatments replicated three times in a Randomized Complete Block Design (RCBD). The treatments were Control (no Urea, no goat manure), 8t/ha-1 goat manure + 200kg/ha-1 urea fertilizer; 8t/ha-1 goat manure + 175kg/ha-1 urea fertilizer and 8t/ha-1 goat manure + 150kg/ha-1 urea fertilizer. Treatments were applied three weeks after planting by ring method with Urea and goat manure mixed. Soil physical and chemical properties, growth and yield parameters were evaluated. Data were analyzed using Analysis of Variance (ANOVA) and Duncan Multiple Range. 8t/ha-1 goat manure + 200kg/ha-1 urea fertilizer gave the highest plant height, leaf area as well as number of leaves than other treatment. However, the fruits weight, days of 50% flowering, number of fruit, fruits diameter and fruits length were significantly increased at 8t/ha-1 goat manure + 200kg/ha-1 urea fertilizer.

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