scholarly journals Effect of molybdenum treatment on the element uptake of food crops in a long-term field experiment

2011 ◽  
pp. 75-79
Author(s):  
Anita Puskás-Preszner ◽  
Béla Kovács ◽  
Dávid Andrási ◽  
Zita Kata Burján
Keyword(s):  
Field Experiment ◽  
Environmental Pollution ◽  
Field Experiments ◽  
Cadmium Accumulation ◽  
Anthropogenic Sources ◽  
Food Crops ◽  
Different Levels ◽  
Term Field

Molybdenum, as a constituent of several important enzymes, is an essential microelement. It can be found in all kind of food naturally at lowlevels. However, environmental pollution, from natural or anthropogenic sources, can lead to high levels of the metal in plants. Our study is based on long-term field experiments at Nagyhörcsök, where different levels of soil contamination conditions are simulated. Plant samples were collected from the experiment station to study the behavior of elements: uptake by and transport within the plants, accumulation in different organs, phytotoxicity and effects on the quantity and quality of the crop. In this study, we present the effect of molybdenum treatment on the uptake of other elements. Molybdenum is proved to be in an antagonist relationship with copper and sulphur, while molybdenum-phosphorus is a synergist interaction. However, in most of the plants we studied, increasing molybdenum-treatment enhanced cadmium uptake. We found the most significant cadmium accumulation in the case of pea, spinach and red beet. 

scholarly journals Effect of molybdenum treatment on the element uptake of plants in a long-term experiment

2012 ◽  
pp. 121-125
Author(s):  
Anita Puskás-Preszner ◽  
Béla Kovács ◽  
Dávid Andrási ◽  
Zita Kata Burján
Keyword(s):  
Field Experiments ◽  
Cadmium Accumulation ◽  
Anthropogenic Sources ◽  
Term Experiment ◽  
Long Term Experiment ◽  
High Level ◽  
Different Levels ◽  
Term Field

Molybdenum as a constituent of several inmportant enzymes is an essential micorelement. It can be found in all kind of food naturally at low level, however, environmental pollution, from natural or anthropogenic sources, can lead to high level of the metal in plants. Our study is based on the long-term field experiments of Nagyhörcsök, where different levels of soil contamination conditions are simulated. Plant samples were collected from the experiment station to study the behaviour of elements: uptake by and transport within the plants, accumulation in different organs, phytotoxicity and effects on the quantity and quality of the crop.In this work we present the effect of molybdenum treatment on the uptake of other elements. Molybdenum is proved to be in an antagonist relationship with copper and sulphur, while molybdenum-phosphorus is a synergist interaction.However, in most of the plants we studied increasing molybdenum-treatment enhanced cadmium-uptake. We have found the most significant cadmium-accumulation in the case of pea, spinach and red beet.

scholarly journals Phosphorus fertilisation under nitrogen limitation can deplete soil carbon stocks – evidence from Swedish meta-replicated long-term field experiments

2015 ◽  
Vol 12 (19) ◽  
pp. 16527-16551 ◽  
Author(s):  
C. Poeplau ◽  
M. A. Bolinder ◽  
H. Kirchmann ◽  
T. Kätterer
Keyword(s):  
Mycorrhizal Fungi ◽  
Field Experiments ◽  
Net Primary Productivity ◽  
Crop Yields ◽  
Agricultural Soils ◽  
Heterotrophic Respiration ◽  
Different Levels ◽  
Soc Stocks ◽  
Term Field

Abstract. Increasing soil organic carbon (SOC) in agricultural soils can mitigate atmospheric CO2 concentration and also contribute to increase soil fertility and ecosystem resilience. The role of major nutrients on SOC dynamics is complex, due to simultaneous effects on net primary productivity (NPP) that influence crop residue carbon inputs and on the rate of heterotrophic respiration (carbon outputs). This study investigated the effect on SOC stocks of three different levels of phosphorus and potassium (PK) fertilisation rates in the absence of nitrogen fertilisation and of three different levels of nitrogen in the absence of PK. This was done by analysing data from 10 meta-replicated Swedish long-term field experiments (> 45 years). With N fertilisation, SOC stocks followed yield increases. However, for all PK levels, we found average SOC losses ranging from −0.04 ± 0.09 Mg ha−1 yr−1 (ns) for the lowest to −0.09 ± 0.07 Mg ha−1 yr−1 (p = 0.008) for the highest application rate, while crop yields as a proxy for carbon input increased significantly with PK fertilization by 1, 10 and 15 %. We conclude that SOC dynamics are mainly output-driven in the PK fertilised regime but mostly input-driven in the N fertilised regime, due to the much more pronounced response of NPP to N than to PK fertilisation. It has been established that P rather than K is the element affecting ecosystem carbon fluxes, where P fertilisation has been shown to: (i) stimulate heterotrophic respiration, (ii) reduce the abundance of arbuscular mycorrhizal fungi and (iii) decrease crop root : shoot ratio, leading to lower root-derived carbon input. The higher export of N in the PK fertilised plots in this study could (iv) have led to increased N mining and thus mineralisation of organic matter. More integrated experiments are needed to gain a better understanding of the relative importance of each of the above-mentioned mechanisms leading to SOC losses after P addition.

KMnO4 determination of active carbon for laboratory routines: three long-term field experiments in Austria

Soil Research ◽  
2015 ◽  
Vol 53 (2) ◽  
pp. 190 ◽  
Author(s):  
M. Tatzber ◽  
N. Schlatter ◽  
A. Baumgarten ◽  
G. Dersch ◽  
R. Körner ◽  
...  
Keyword(s):  
Field Experiment ◽  
Field Experiments ◽  
Cropping Systems ◽  
Organic Amendments ◽  
Sodium Oxalate ◽  
Tillage Systems ◽  
Organic C ◽  
Significant Difference ◽  
Term Field

Recent studies show that a labile soil carbon (C) fraction determined with potassium permanganate (KMnO4) reflects the type of soil management. The present study combines the method for determining the active C (AC) pool with an alternative titration of the 0.02 m KMnO4 solution with sodium oxalate (Na2C2O4) for routine laboratory analyses. Three long-term field experiments investigated: (i) different cropping systems and 14C-labelled organic amendments, (ii) three different tillage systems, and (iii) the application of four different kinds of compost. The results showed the depletion of AC in the permanent bare-fallow system of the 14C-labelled field experiment. When calculating the ratio AC/total organic C (TOC), the depletion of the AC/TOC curve reflected a priming effect, in accord with previous work. We obtained significant positive correlations of AC with TOC, total nitrogen (Nt), humic acid-C and remaining 14C-labelled material. The AC in the tillage systems experiment was significantly (P < 0.05) different between all three tillage treatments at 0–10 cm depth, and the ratio AC/TOC also revealed a significant difference between minimum and conventional tillage treatments at 10–20 cm. For the compost field experiment, significant differences occurred between plots fertilised solely with N and plots receiving organic amendments. The AC/TOC ratio of the sewage sludge amendment was significantly lower than in all other systems. Correlations of AC with TOC for all samples of the different long-term field experiments revealed different behaviours in different soil types. The correlations of AC with Nt showed higher coefficients than with TOC. The applied methodology has a potential for sensitive and reliable detections of differences in soil organic matter characteristics.

scholarly journals Evaluating of soil sulphur forms changes in long-term field experiments of Látókép

2019 ◽  
pp. 71-76
Author(s):  
Evelin Kármen Juhász ◽  
Andrea Balláné Kovács
Keyword(s):  
Winter Wheat ◽  
Field Experiment ◽  
Field Experiments ◽  
Stem Elongation ◽  
Water Soluble ◽  
Research Station ◽  
Npk Fertilizers ◽  
Sulphate Content ◽  
Term Field

The aim of this work was to evaluate the changes of different sulphur forms (soluble, adsorbed) in chernozem soil in a long-term field experiment supplied with increasing doses of NPK fertilizers for a long time. In addition, other objective of this study included the examination of the applicability of recommended extractants of the different sulphate fraction in Hungarian soils. A long-term field experiment was established at the Research Station of Látókép of the University of Debrecen in 1984. In addition to control, two levels of NPK fertilizer doses have been used with irrigated and non-irrigated variants. Winter wheat and corn were cropped in a crop rotation on plots. Soil samples were collected in three different development stages of winter wheat, at the stage of stem elongation (April), flowering (May) and ripening (June of 2018) from the topsoil (0–20 cm) of experiment plots. Water-soluble inorganic sulphate was extracted with 0.01M CaCl2 solutions. The soluble plus adsorbed sulphate was extracted with 0.016M KH2PO4 solution. Sulphate was measured by turbidimetric method. 0.01M CaCl2-SO42— ranged between 0.293–1.896 mg kg-1 and the 0.016 M KH2PO4-SO42- varied between 5.087–10.261 mg kg-1. The values of KH2PO4 SO42- was higher than that of CaCl2-SO42-, because KH2PO4 extracted the adsorbed and soluble fractions of sulphate, while CaCl2 extracted the soluble sulphate fraction. The amount of absorbed sulphate was calculated by the differences of KH2PO4- SO4 and CaCl2-SO4. The KH2PO4 characterizes mainly the adsorbed sulphate fraction much more than the water-soluble fraction. KCl is the most widely used extractant for the determination of plant available sulphate content of soil in Hungary; therefore, KCl-SO42- fraction also was determined. The KCl-SO42- ranged between 0.328–2.152 mg kg-1. The CaCl2-SO42- and KCl-SO42- fractions were compared and based on Pearson's linear correlation, moderate correlation was established (r=0.511) between them. In all three extractant (0.01M CaCl2, 1M KCl, 0.016 M KH2PO4) higher sulphate fractions were measured in the fertilized plots where superphosphate had been supplied for ages until 2010. The arylsulphatase activity of soil also was determined and ranged between 9.284 and 26.860 µg p-nitrophenol g-1 h-1. The lowest value was observed in the treatment with highest NPK2 dose, both in irrigated and non-irrigated areas.

scholarly journals Phosphorus fertilisation under nitrogen limitation can deplete soil carbon stocks: evidence from Swedish meta-replicated long-term field experiments

2016 ◽  
Vol 13 (4) ◽  
pp. 1119-1127 ◽  
Author(s):  
Christopher Poeplau ◽  
Martin A. Bolinder ◽  
Holger Kirchmann ◽  
Thomas Kätterer
Keyword(s):  
Mycorrhizal Fungi ◽  
Field Experiments ◽  
Net Primary Productivity ◽  
Crop Yields ◽  
Agricultural Soils ◽  
Heterotrophic Respiration ◽  
Different Levels ◽  
Soc Stocks ◽  
Term Field

Abstract. Increasing soil organic carbon (SOC) in agricultural soils can mitigate atmospheric CO2 concentration and also contribute to increased soil fertility and ecosystem resilience. The role of major nutrients in SOC dynamics is complex, due to simultaneous effects on net primary productivity (NPP) that influence crop residue carbon inputs and in the rate of heterotrophic respiration (carbon outputs). This study investigated the effect on SOC stocks of three different levels of phosphorus and potassium (PK) fertilisation rates in the absence of nitrogen fertilisation and of three different levels of nitrogen fertiliser in the absence of PK fertiliser. This was done by analysing data from 10 meta-replicated Swedish long-term field experiments (> 45 years). With N fertilisation, SOC stocks followed yield increases. However, for all PK levels, we found average SOC losses ranging from −0.04 ± 0.09 Mg ha−1 yr−1 (ns) for the lowest to −0.09 ± 0.07 Mg ha−1 yr−1 (p =  0.008) for the highest application rate, while crop yields as a proxy for carbon input increased significantly with PK fertilisation by 1, 10 and 15 %. We conclude that SOC dynamics are mainly output-driven in the PK-fertilised regime but mostly input-driven in the N-fertilised regime, due to the much more pronounced response of NPP to N than to PK fertilisation. It has been established that P rather than K is the element affecting ecosystem carbon fluxes, where P fertilisation has been shown to (i) stimulate heterotrophic respiration, (ii) reduce the abundance of arbuscular mycorrhizal fungi and (iii) decrease the crop root : shoot ratio, leading to higher root-derived carbon input. The higher export of N in the PK-fertilised plots in this study could (iv) have led to increased N mining and thus mineralisation of organic matter. More integrated experiments are needed to gain a better understanding of the relative importance of each of the above-mentioned mechanisms leading to SOC losses after P addition.

scholarly journals Effect of seed dressing treatment of Streptomyces griseoviridis on barley and spring wheat in field experiments

1995 ◽  
Vol 4 (4) ◽  
pp. 419-427 ◽  
Author(s):  
Risto Tahvonen ◽  
Asko Hannukkala ◽  
Hanna Avikainen
Keyword(s):  
Seed Treatment ◽  
Field Experiments ◽  
Yield Losses ◽  
Fusarium Spp ◽  
Root Rots ◽  
Seed Dressing ◽  
Streptomyces Griseoviridis ◽  
Different Levels ◽  
Term Field

The effect of seed dressing with the antagonist Streptomyces griseoviridis on root rots and yields of wheat and barley was studied in field experiments. In long-term field experiments, where different levels of soil-borne inoculum of root rots were maintained with different crop sequences, seed treatment with the antagonist increased yields slightly on average over all experimental years. However, variations between years, crops and crop sequences were considerable. The highest yield increases were in excess of 600 kg/ha, whilst treatment occasionally resulted in slight yield losses. In experiments in which seed naturally infested with Fusarium spp. was used, seed treatment with S. griseoviridis increased yields of wheat but not those of barley. Seed dressing with an organomercurial fungicide resulted in higher yield increases than the biopreparate.

Introduction

2000 ◽  
Vol 14 (6) ◽  
pp. 719 ◽  
Author(s):  
Ebbe Nielsen ◽  
Rolf Oberprieler
Keyword(s):  
Habitat Fragmentation ◽  
Field Experiment ◽  
International Level ◽  
Data Set ◽  
Eucalyptus Forest ◽  
Great Insight ◽  
Term Field

In this brief review we outline the contribution of Dr J. F. Lawrence to a major long-term field experiment in the southeast forests of NSW that examines the effect of habitat fragmentation on beetles. Dr J. F. Lawrence identified and curated the beetle fauna, which proved to be a significant and long-term commitment. The beetle data set has since provided great insight to the complex effects of habitat fragmentation. In addition, the size and quality of the data set mean that, on an international level, it is a major inventory of beetle diversity in a temperate Eucalyptus forest, in its own right. Here we outline Dr J. F. Lawrence’s contribution and summarise the main features of the beetle data set and our findings about the impacts of fragmentation on the beetle fauna.

scholarly journals <sup>14</sup>C in cropland soil of a long-term field trial – experimental variability and implications for estimating carbon turnover

SOIL ◽  
2015 ◽  
Vol 1 (2) ◽  
pp. 537-542 ◽  
Author(s):  
J. Leifeld ◽  
J. Mayer
Keyword(s):  
Field Experiment ◽  
Soil Carbon ◽  
Field Experiments ◽  
Soil Depth ◽  
Carbon Turnover ◽  
Independent Field ◽  
Experimental Variability ◽  
Soil Carbon Turnover ◽  
Term Field

Abstract. Because of their controlled nature, the presence of independent replicates, and their known management history, long-term field experiments are key to the understanding of factors controlling soil carbon. Together with isotope measurements, they provide profound insight into soil carbon dynamics. For soil radiocarbon, an important tracer for understanding these dynamics, experimental variability across replicates is usually not accounted for; hence, a relevant source of uncertainty for quantifying turnover rates is missing. Here, for the first time, radiocarbon measurements of five independent field replicates, and for different layers, of soil from the 66-year-old controlled field experiment ZOFE in Zurich, Switzerland, are used to address this issue. 14C variability was the same across three different treatments and for three different soil layers between the surface and 90 cm depths. On average, experimental variability in 14C content was 12 times the analytical error but still, on a relative basis, smaller than variability in soil carbon concentration. Despite a relative homogeneous variability across the field and along the soil profile, the curved nature of the relationship between radiocarbon content and modelled carbon mean residence time implies that the absolute error of calculated soil carbon turnover time increases with soil depth. In our field experiment findings on topsoil carbon turnover variability would, if applied to subsoil, tend to underweight turnover variability even if experimental variability in the subsoil isotope concentration is the same. Together, experimental variability in radiocarbon is an important component in an overall uncertainty assessment of soil carbon turnover.

scholarly journals Effect of molybdenum treatment on uptake of plant and soil molybdenum content in a field experiment

2009 ◽  
pp. 117-122 ◽  
Author(s):  
Anita Puskás-Preszner ◽  
Béla Kovács
Keyword(s):  
Field Experiments ◽  
Total Concentration ◽  
Anthropogenic Sources ◽  
Extrinsic Factors ◽  
Vegetative Organs ◽  
Plant Samples ◽  
Low Levels ◽  
High Level

Molybdenum is not a well-known microelement, but being a constituent of several important cellular enzymes it is an essential microelement. Molybdenum occurs in all foods, but at very low levels. There does not appear to be any particular foods or types of foods, which in the absence of extrinsic factors, naturally have high levels of molybdenum. However, environmental pollution, from natural or anthropogenic sources, can lead to high level of the metal in plants.Our study is based on the long-term field experiments of Nagyhörcsök, where different levels of soil contamination conditions are simulated. Soil and plant samples were collected from the experiment station to study the behaviour of molybdenum: total concentration, available  concentration, leaching, transformation, uptake by and transport within the plants, accumulation in different organs, phytotoxicity and effects on the quantity and quality of the crop. In this work we present the results of maize and peas and the soil samples related to them.According to our data molybdenum is leaching from the topsoil at a medium rate and it appears in the deeper layers. In the case of plant samples we found that molybdenum level in the straw is many times higher than that is in the grain, so molybdenum accumulates in the vegetative organs of the plant. The data also show differences in the molybdenum-uptake of cereals and Fabaceae (or Leguminosae).

Sign in / Sign up

Export Citation Format

Share Document