scholarly journals Risk of phosphorus losses in surface runoff from agricultural land in the Baltic Commune of Puck in the light of assessment performed on the basis of DPS indicator

PeerJ ◽  
2020 ◽  
Vol 8 ◽  
pp. e8396 ◽  
Author(s):  
Stefan Pietrzak ◽  
Grażyna Pazikowska-Sapota ◽  
Grażyna Dembska ◽  
Lidia Anita Dzierzbicka-Glowacka ◽  
Dominika Juszkowska ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Agricultural Land ◽  
Organic Matter Content ◽  
Water Soluble ◽  
Risk Level ◽  
Organic Soils ◽  
P Concentration ◽  
Ammonium Lactate ◽  
Mineral Soils ◽  
The Baltic

Background In order to counteract the eutrophication of waterways and reservoirs, a basic risk assessment of phosphorus (P) losses in the surface runoff from agricultural land should be included in water management plans. A new method has been developed to assess the risk of P losses by estimating the degree of P saturation (DPS) based on the P concentration of the water extract water-soluble P. Methods The risk of P losses in surface runoff from agricultural land in the Puck Commune on the Baltic Sea Coast was assessed with the DPS method. The results were compared to an agronomic interpretation of the soil test P concentration (STP). Research was conducted on mineral and organic soils from 50 and 11 separate agricultural plots with a total area of 133.82 and 37.23 ha, respectively. Phosphorus was extracted from the collected samples using distilled water on all soil samples, acid ammonium lactate on mineral soils, and an extract of 0.5 mol HCl·dm−3 on organic soils. The organic matter content and pH values were also determined. The results of the P content in the water extracted from the soils were converted into DPS values, which were then classified by appropriate limit intervals. Results and discussion There was a high risk of P losses from the soil via surface runoff in 96.7% of the agricultural parcels tested (96% of plots with mineral soils and 100% of plots with organic soils). Simultaneously, a large deficiency of plant-available P was found in soils from 62% of agricultural plots. These data indicate that the assessment of P concentration in soils made on the basis of an environmental soil P test conflicts with the assessment made based on STP and create a cognitive dissonance. The risk level of P losses through surface runoff from the analyzed plots as determined by the DPS indicator is uncertain. This uncertainty is increased as the DPS index is not correlated with other significant factors in P runoff losses, such as the type of crop and area inclination.

scholarly journals Risk of phosphorus loss in surface runoff from agricultural land in the Baltic Commune of Puck

2019 ◽  
Author(s):  
Stefan Pietrzak ◽  
Grażyna Pazikowska-Sapota ◽  
Grażyna Dembska ◽  
Lidia Anita Dzierzbicka-Glowacka ◽  
Dominika Juszkowska ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Agricultural Land ◽  
Water Extract ◽  
Soil Samples ◽  
Water Soluble ◽  
Organic Soils ◽  
Distilled Water ◽  
Degree Of P Saturation ◽  
P Content ◽  
Mineral Soils

Background. Risk assessment of Phosphorus (P) losses in surface runoff from agricultural land is the basic measure that should be used as a part of actions taken to counteract the water eutrophication in watercourses and water reservoirs. To assess this risk, a new method has been recently developed based on the determination of degree of P saturation (DPS) which depends on P content in soil determined with the use of distilled water (water-soluble P – WSP). Methods. Based on DPS method, the risk of P losses in surface runoff from agricultural land in Puck Commune (Baltic Sea Coast) was assessed and a critical analysis of assessment results was carried out. The research was conducted on mineral and organic soils from 50 and 11 separate agricultural plots with a total area of 133.82 and 37.23 ha, respectively. In collected soil samples, P content was determined using distilled water (all soil samples), Egner-Riehm method (mineral soils) and extract of 0.5 mol HCl ∙ dm-3 (organic soils). The results of determinations P content in water extract from soils were converted to DPS values, which were classified by appropriate limit intervals. Results & Discussion. It was found that on 96.7% of tested agricultural parcels (96% plots with mineral soils and 100% plots with organic soils) there was a potentially high risk of P losses from soil by surface runoff. At the same time, it was ascertained that in soils from 62% of agricultural plots, there was a large deficiency of plant available P. Due to the above, as well as due to the lack of connection with other factors affecting the P losses in surface runoff such as type of crop and area inclination, it was considered that the assessment based on the DPS index may be unreliable.

scholarly journals Risk of phosphorus loss in surface runoff from agricultural land in the Baltic Commune of Puck

2019 ◽  
Author(s):  
Stefan Pietrzak ◽  
Grażyna Pazikowska-Sapota ◽  
Grażyna Dembska ◽  
Lidia Anita Dzierzbicka-Glowacka ◽  
Dominika Juszkowska ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Agricultural Land ◽  
Water Extract ◽  
Soil Samples ◽  
Water Soluble ◽  
Organic Soils ◽  
Distilled Water ◽  
Degree Of P Saturation ◽  
P Content ◽  
Mineral Soils

Background. Risk assessment of Phosphorus (P) losses in surface runoff from agricultural land is the basic measure that should be used as a part of actions taken to counteract the water eutrophication in watercourses and water reservoirs. To assess this risk, a new method has been recently developed based on the determination of degree of P saturation (DPS) which depends on P content in soil determined with the use of distilled water (water-soluble P – WSP). Methods. Based on DPS method, the risk of P losses in surface runoff from agricultural land in Puck Commune (Baltic Sea Coast) was assessed and a critical analysis of assessment results was carried out. The research was conducted on mineral and organic soils from 50 and 11 separate agricultural plots with a total area of 133.82 and 37.23 ha, respectively. In collected soil samples, P content was determined using distilled water (all soil samples), Egner-Riehm method (mineral soils) and extract of 0.5 mol HCl ∙ dm-3 (organic soils). The results of determinations P content in water extract from soils were converted to DPS values, which were classified by appropriate limit intervals. Results & Discussion. It was found that on 96.7% of tested agricultural parcels (96% plots with mineral soils and 100% plots with organic soils) there was a potentially high risk of P losses from soil by surface runoff. At the same time, it was ascertained that in soils from 62% of agricultural plots, there was a large deficiency of plant available P. Due to the above, as well as due to the lack of connection with other factors affecting the P losses in surface runoff such as type of crop and area inclination, it was considered that the assessment based on the DPS index may be unreliable.

Field dissipation of S-metolachlor in organic and mineral soils used for sugarcane production in Florida

2019 ◽  
Vol 34 (3) ◽  
pp. 362-370
Author(s):  
Jose V. Fernandez ◽  
D. Calvin Odero ◽  
Gregory E. MacDonald ◽  
Jason A. Ferrell ◽  
Brent A. Sellers ◽  
...  
Keyword(s):  
Organic Matter ◽  
Soil Moisture ◽  
Linear Trend ◽  
Organic Matter Content ◽  
Field Studies ◽  
Matter Content ◽  
Organic Soils ◽  
Sugarcane Production ◽  
Mineral Soils ◽  
Moisture Conditions

AbstractDissipation of S-metolachlor, a soil-applied herbicide, on organic and mineral soils used for sugarcane production in Florida was evaluated using field studies in 2013 to 2016. S-metolachlor was applied PRE at 2,270 g ha−1 on organic and mineral soils with 75% and 1.6% organic matter, respectively. The rate of dissipation of S-metolachlor was rapid on mineral soils compared with organic soils. Dissipation of S-metolachlor on organic soils followed a negative linear trend resulting in half-lives (DT50) ranging from 50 to 126 d. S-metolachlor loss on organic soils was more rapid under high soil-moisture conditions than in corresponding low soil-moisture conditions. On mineral soils, dissipation of S-metolachlor followed an exponential decline. The DT50 of S-metolachlor on mineral soils ranged from 12 to 24 d. The short persistence of S-metolachlor on mineral soils was likely attributed to low organic matter content with limited adsorptive capability. The results indicate that organic matter content and soil moisture are important for persistence of S-metolachlor on organic and mineral soils used for sugarcane production in Florida.

The nature of interference potential of Kalmiaangustifolia

1996 ◽  
Vol 26 (11) ◽  
pp. 1899-1904 ◽  
Author(s):  
Inderjit Inderjit ◽  
A.U. Mallik
Keyword(s):  
Leaf Litter ◽  
Black Spruce ◽  
Organic Soil ◽  
Water Soluble ◽  
Total Phenolic ◽  
Organic Soils ◽  
Soluble Phenolics ◽  
Phenolic Contents ◽  
Mineral Soils ◽  
Rule Out

The nature of interference potential of Kalmiaangustifolia L., a boreal forest understorey shrub, was investigated in laboratory experiments. Organic and mineral soils, not previously associated with Kalmia, were amended with different quantities of its leaf litter and leaf litter leachates. The objectives of the study were (i) to determine changes in soil chemistry after amending with Kalmia and (ii) to determine the effect of amendment on growth of black spruce (Piceamariana (Mill.) BSP) seedlings. All soils were analyzed for pH, organic matter, PO4−, N, Ba, Cu, Zn, Fe, Mn, Ca, Na, K, Mg, Al, and total phenolics. Chemical characteristics of both organic and mineral soils were significantly changed. Water-soluble phenolics in one of the amended organic soils were significantly higher than in unamended organic soil. However, all of the amended mineral soils had significantly higher total phenolic contents than unamended control soils. A linear decrease in N content was observed in amended organic and mineral soils with increasing quantities of Kalmia leaf litter. Amended mineral soils had higher concentrations of Fe, Mn, Al, and PO4− than the control. We relate higher accumulations of PO4−, Fe, Mn, and Al in amended mineral soils to higher soil phenolic contents. Amendment of organic and mineral soils significantly reduced the root and shoot growth of black spruce. This study demonstrates that Kalmia has potential for nutrient interference and does not rule out allelopathic effects of Kalmia to black spruce seedling growth.

COBALT STATUS IN QUEBEC SOILS

1967 ◽  
Vol 47 (2) ◽  
pp. 83-88 ◽  
Author(s):  
S. K. Rana ◽  
G. J. Ouellette
Keyword(s):  
Mineral Soil ◽  
Organic Matter Content ◽  
Clay Content ◽  
Cobalt Content ◽  
Matter Content ◽  
Organic Soils ◽  
Soil Series ◽  
Acid Digestion ◽  
Cobalt Deficiency ◽  
Mineral Soils

Studies on thirty mineral soil series and five organic soils from the broad cultivated areas of Quebec indicated that total cobalt, extracted with 70% perchloric acid digestion, ranged from 1.1 to 21.6 ppm and 2.5% acetic acid-extractable cobalt from 0.3 to 0.83 ppm. Extractable cobalt in the surface soils was significantly correlated with total cobalt, which in turn was highly dependent on the clay content of the soil. The soil pH or the organic matter content did not seem to have any influence on the cobalt content in the cultivated soils. Light-textured and podzolized soils are likely to be low m cobalt, while soils with richer clay content are higher. Organic soils, in general, were found to be lower in cobalt content than mineral soils. Nineteen out of the thirty mineral soils studied and all the organic soils contained less than 0.25 ppm of extractable cobalt and may be considered as critical or deficient because forage grown on such soils is likely to cause cobalt deficiency in livestock.

Physico-Chemical Properties of Soil Collected from Chandrabhaga River in Kalmeshwar, Nagpur, Maharashtra

2020 ◽  
Vol 07 (02) ◽  
pp. 1-3
Author(s):  
Amita M Watkar ◽  
Keyword(s):  
Organic Matter ◽  
Soil Quality ◽  
Agricultural Land ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Matter Content ◽  
Soil Attributes ◽  
Essential Components ◽  
Agricultural Land Management ◽  
Physical And Chemical

Soil, itself means Soul of Infinite Life. Soil is the naturally occurring unconsolidated or loose covering on the earth’s surface. Physical properties depend upon the amount, size, shape, arrangement, and mineral composition of soil particles. It also depends on the organic matter content and pore spaces. Chemical properties depend on the Inorganic and organic matter present in the soil. Soils are the essential components of the environment and foundation resources for nearly all types of land use, besides being the most important component of sustainable agriculture. Therefore, assessment of soil quality and its direction of change with time is an ideal and primary indicator of sustainable agricultural land management. Soil quality indicators refer to measurable soil attributes that influence the capacity of a soil to function, within the limits imposed by the ecosystem, to preserve biological productivity and environmental quality and promote plant, animal and human health. The present study is to assess these soil attributes such as physical and chemical properties season-wise.

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