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Forest roads play a crucial role in commercial forestry. Most of them are unpaved and exposed to increased surface runoff and the occurrence of soil erosion. Therefore, these roads constantly require repairs and maintenance, which are associated with the high cost of earthworks. Soil water repellency causes retardation of water infiltration into soil, which affects the generation of surface runoff, leading to the destruction of the active road layer. This phenomenon is well recognized in forest habitat soils, but poorly investigated in terms of soils constituting roads and communication routes. Therefore, the aims of this research were to determine the severity and persistence of potential water repellency in the case of soil collected from two unpaved roads in coniferous forest and to investigate the dependence between the severity of soil water repellency and its persistence. Soil samples (Dystric Brunic Arenosols) were collected from three points of the roadway, i.e., centre line, rut and roadside, from two different sites located in fresh coniferous and fresh mixed coniferous forest (Poland). The severity of soil water repellency was assessed, based on measured values of the wetting contact angle (Wilhelmy plate method) and the critical and 90° surface tensions. For this purpose, contact angle measurements of the solid phase, wetted by water–ethanol mixtures, were used and data results were analysed using the Zisman approach. The persistence of potential soil water repellency was assessed using the water drop penetration time test. The severity and persistence of soil water repellency depend on the forest habitat type surrounding the road and point locations on the road cross section. The soil samples collected from the roadside were more water repellent than samples taken from the centre line or rut. A strong relationship was found between the water drop penetration time and the advancing contact angle, the critical surface tension and the 90° surface tension.
Ewa Papierowska; Jan Szatyłowicz; Maria Ruta; Andrzej Łachacz; Tomasz Gnatowski; Tomasz Stańczyk. Water repellency of soils on unpaved roads in coniferous forests. CATENA 2020, 195, 104784 .
AMA StyleEwa Papierowska, Jan Szatyłowicz, Maria Ruta, Andrzej Łachacz, Tomasz Gnatowski, Tomasz Stańczyk. Water repellency of soils on unpaved roads in coniferous forests. CATENA. 2020; 195 ():104784.
Chicago/Turabian StyleEwa Papierowska; Jan Szatyłowicz; Maria Ruta; Andrzej Łachacz; Tomasz Gnatowski; Tomasz Stańczyk. 2020. "Water repellency of soils on unpaved roads in coniferous forests." CATENA 195, no. : 104784.
Leaf wettability has an impact on a plant’s ability to retain water on its leaf surface, which in turn has many environmental consequences. In the case of the potato leaf (Solanum tuberosum L.), water on the leaf surface may contribute to the development of a fungal disease. If fungal disease is caused, this may reduce the size of potato harvests, which contribute significantly to meeting global food demand. The aim of this study was to assess the leaf wettability of five potato cultivars (i.e., Bryza, Lady Claire, Rudawa, Russet Burbank, Sweet Caroline) in the context of its direct and indirect impact on potato yield. Leaf wettability was assessed on the basis of contact angle measurements using a sessile drop method with an optical goniometer. For Bryza and Rudawa cultivars, which showed, respectively, the highest and the lowest contact angle values, light microscopy as well as scanning electron microscopy analyses were performed. The results of the contact angle measurements and microscopic image analyses of the potato leaf surfaces indicated that the level of wettability was closely related to the type of trichomes on the leaf and their density. Therefore, higher resistance of the Rudawa cultivar to biotic stress conditions could be the result of the presence of two glandular trichome types (VI and VII), which produce and secrete metabolites containing various sticky and/or toxic chemicals that may poison or repel herbivores.
Ewa Papierowska; Jan Szatyłowicz; Stanisław Samborski; Joanna Szewińska; Elżbieta Różańska. The Leaf Wettability of Various Potato Cultivars. Plants 2020, 9, 504 .
AMA StyleEwa Papierowska, Jan Szatyłowicz, Stanisław Samborski, Joanna Szewińska, Elżbieta Różańska. The Leaf Wettability of Various Potato Cultivars. Plants. 2020; 9 (4):504.
Chicago/Turabian StyleEwa Papierowska; Jan Szatyłowicz; Stanisław Samborski; Joanna Szewińska; Elżbieta Różańska. 2020. "The Leaf Wettability of Various Potato Cultivars." Plants 9, no. 4: 504.
Despite covering only 2–6% of land, wetland ecosystems play an important role at the local and global scale. They provide various ecosystem services (carbon dioxide sequestration, pollution removal, water retention, climate regulation, etc.) as long as they are in good condition. By definition, wetlands are rich in water ecosystems. However, ongoing climate change with an ambiguous balance of rain in a temperate climate zone leads to drought conditions. Such periods interfere with the natural processes occurring on wetlands and restrain the normal functioning of wetland ecosystems. Persisting unfavorable water conditions lead to irreversible changes in wetland habitats. Hence, the monitoring of habitat changes caused by an insufficient amount of water (plant water stress) is necessary. Unfortunately, due to the specific conditions of wetlands, monitoring them by both traditional and remote sensing techniques is challenging, and research on wetland water stress has been insufficient. This paper describes the adaptation of the thermal water stress index, also known as the crop water stress index (CWSI), for wetlands. This index is calculated based on land surface temperature and meteorological parameters (temperature and vapor pressure deficit—VPD). In this study, an unmanned aerial system (UAS) was used to measure land surface temperature. Performance of the CWSI was confirmed by the high correlation with field measurements of a fraction of absorbed photosynthetically active radiation (R = −0.70) and soil moisture (R = −0.62). Comparison of the crop water stress index with meteorological drought indices showed that the first phase of drought (meteorological drought) cannot be detected with this index. This study confirms the potential of using the CWSI as a water stress indicator in wetland ecosystems.
Wojciech Ciężkowski; Sylwia Szporak-Wasilewska; Małgorzata Kleniewska; Jacek Jóźwiak; Tomasz Gnatowski; Piotr Dąbrowski; Maciej Góraj; Jan Szatyłowicz; Stefan Ignar; Jarosław Chormański. Remotely Sensed Land Surface Temperature-Based Water Stress Index for Wetland Habitats. Remote Sensing 2020, 12, 631 .
AMA StyleWojciech Ciężkowski, Sylwia Szporak-Wasilewska, Małgorzata Kleniewska, Jacek Jóźwiak, Tomasz Gnatowski, Piotr Dąbrowski, Maciej Góraj, Jan Szatyłowicz, Stefan Ignar, Jarosław Chormański. Remotely Sensed Land Surface Temperature-Based Water Stress Index for Wetland Habitats. Remote Sensing. 2020; 12 (4):631.
Chicago/Turabian StyleWojciech Ciężkowski; Sylwia Szporak-Wasilewska; Małgorzata Kleniewska; Jacek Jóźwiak; Tomasz Gnatowski; Piotr Dąbrowski; Maciej Góraj; Jan Szatyłowicz; Stefan Ignar; Jarosław Chormański. 2020. "Remotely Sensed Land Surface Temperature-Based Water Stress Index for Wetland Habitats." Remote Sensing 12, no. 4: 631.
Green roofs ought to be perceived as ensuring a wide-ranging contribution to the sustainable urban environment. The aim of the study was; (1) to investigate and analyse the differences in the surface temperature between four models of green roofs of the extensive type and a conventional roof (covered with bitumen) under the conditions of a continental climate; (2) to assess the influence of environmental parameters (climatic water balance, air temperature, relative humidity, moisture content in the profile) on changes in the temperature of the extensive type green roof profile (substrate and vegetation mat). The study (1) was carried out during the period of June–December 2016 using a thermal imaging camera. As a result, the greatest differences in temperature were noted in June and July, with a maximum difference between the temporary surface temperature of a green roof and a conventional roof of up to 24 °C. The (2) study was conducted on a green roof profile with sedum plant vegetation. The measured parameters were: the temperature of the surface, the temperature and humidity at depths of 3 cm and 15 cm, and active radiation in the photosynthesis process (PAR). As the result, the range of daily changes in the surface temperatures and the vegetation mat were higher than the range of changes in the air temperature. Atmospheric precipitation decreased the thermal gradient in the soil, as well as the temperature fluctuations in the course of a day as a result of the increase in humidity following a rainfall. During the summer period, over the course of a day, the surface temperature was 5 °C higher than the air temperature. The largest correlation was obtained between the air temperature and the temperature of the surface as well as the temperature of the structural layers.
Anna Baryła; Tomasz Gnatowski; Agnieszka Karczmarczyk; Jan Szatyłowicz. Changes in Temperature and Moisture Content of an Extensive-Type Green Roof. Sustainability 2019, 11, 2498 .
AMA StyleAnna Baryła, Tomasz Gnatowski, Agnieszka Karczmarczyk, Jan Szatyłowicz. Changes in Temperature and Moisture Content of an Extensive-Type Green Roof. Sustainability. 2019; 11 (9):2498.
Chicago/Turabian StyleAnna Baryła; Tomasz Gnatowski; Agnieszka Karczmarczyk; Jan Szatyłowicz. 2019. "Changes in Temperature and Moisture Content of an Extensive-Type Green Roof." Sustainability 11, no. 9: 2498.
The proper monitoring of soil moisture content is important to understand water-related processes in peatland ecosystems. Time domain reflectometry (TDR) is a popular method used for soil moisture content measurements, the applicability of which is still challenging in field studies due to requirements regarding the calibration curve which converts the dielectric constant into the soil moisture content. The main objective of this study was to develop a general calibration equation for the TDR method based on simultaneous field measurements of the dielectric constant and gravimetric water content in the surface layers of degraded peatlands. Data were collected during field campaigns conducted temporarily between the years 2006 and 2016 at the drained peatland Kuwasy located in the north-east area of Poland. Based on the data analysis, a two-slopes linear calibration equation was developed as a general broken-line model (GBLM). A site-specific calibration model (SSM-D) for the TDR method was obtained in the form of a two-slopes equation describing the relationship between the soil moisture content and the dielectric constant and introducing the bioindices as covariates relating to plant species biodiversity and the state of the habitats. The root mean squared error for the GBLM and SSM-D models were equal, respectively, at 0.04 and 0.035 cm3 cm−3.
Tomasz Gnatowski; Jan Szatyłowicz; Bogumiła Pawluśkiewicz; Ryszard Oleszczuk; Maria Janicka; Ewa Papierowska; Daniel Szejba. Field Calibration of TDR to Assess the Soil Moisture of Drained Peatland Surface Layers. Water 2018, 10, 1842 .
AMA StyleTomasz Gnatowski, Jan Szatyłowicz, Bogumiła Pawluśkiewicz, Ryszard Oleszczuk, Maria Janicka, Ewa Papierowska, Daniel Szejba. Field Calibration of TDR to Assess the Soil Moisture of Drained Peatland Surface Layers. Water. 2018; 10 (12):1842.
Chicago/Turabian StyleTomasz Gnatowski; Jan Szatyłowicz; Bogumiła Pawluśkiewicz; Ryszard Oleszczuk; Maria Janicka; Ewa Papierowska; Daniel Szejba. 2018. "Field Calibration of TDR to Assess the Soil Moisture of Drained Peatland Surface Layers." Water 10, no. 12: 1842.
The research carried out concerned the laboratory assessment of the applicability of the Crop Water Stress Index (CWSI) as a practical tool for assessing the risk of desiccation for selected wetland habitats: transition mires and quaking bogs as well as alkaline fens. The analysis was carried out on 3 soil samples with a vegetation cover (with the dimensions of 40×40×30 cm) collected during the full vegetation season for each mentioned habitat, with a characteristic species composition. Experimental research was carried out between 17th May 2018 and 19th June 2018. Thermal, RGB and multispectral images, chlorophyll content, volumetric soil moisture, air temperature and relative humidity measurements were taken for each sample every two days. The obtained results clearly indicate the dependence between CWSI and plant condition parameters in the first phase of desiccation. At the same time, as a result of the observations taken, thresholds have been set, indicating different desiccation phases.
Maciej Góraj; Wojciech Ciężkowski; Piotr Sikorski; Małgorzata Kleniewska; Sylwia Szporak-Wasilewska; Jacek Jóźwiak; Tomasz Gnatowski; Jan Szatyłowicz; Jarosław Chormański. Characterizing Selected Wetland Habitats’ Desiccation Phenomena Using the Crop Water Stress Index. 2018, 1 .
AMA StyleMaciej Góraj, Wojciech Ciężkowski, Piotr Sikorski, Małgorzata Kleniewska, Sylwia Szporak-Wasilewska, Jacek Jóźwiak, Tomasz Gnatowski, Jan Szatyłowicz, Jarosław Chormański. Characterizing Selected Wetland Habitats’ Desiccation Phenomena Using the Crop Water Stress Index. . 2018; ():1.
Chicago/Turabian StyleMaciej Góraj; Wojciech Ciężkowski; Piotr Sikorski; Małgorzata Kleniewska; Sylwia Szporak-Wasilewska; Jacek Jóźwiak; Tomasz Gnatowski; Jan Szatyłowicz; Jarosław Chormański. 2018. "Characterizing Selected Wetland Habitats’ Desiccation Phenomena Using the Crop Water Stress Index." , no. : 1.
Planet Earth is undergoing significant changes which are driven by natural and anthropogenic factors. However, it is difficult to identify the drivers and their effect on the environment and ecosystems because there are many interdependencies. In this study we present a multi-parameter approach to assess the effect of changes in human-induced and natural drivers on a wetland ecosystem. The study area is one of the most prominent European wetlands: the Biebrza Basin, located in north-eastern Poland. We analysed long-term (ca. 1960–2000) changes in meteorology, hydrology, soil and vegetation, and also conservation history. This approach enabled us to identify interactions between environmental change and management. We found significant trends (1960–2012) indicating climate change: increases in temperature, evapotranspiration and earlier start of spring floods. We identified (1970–2000) a shift towards drier vegetation types after drainage. However, we also found that restoration measures that were implemented have mitigated climate change effects and have led to increases in soil moisture and wetter vegetation types. We conclude that, if carried out sufficiently frequently, the management measures implemented in the Biebrza Basin, which are a combination of different restoration measures (blocking drainage, not clearing aquatic vegetation, bush removal, mowing), can to some extent mitigate the effects of climate change.
Tomasz Berezowski; Martin Wassen; Jan Szatyłowicz; Jarosław Chormański; Stefan Ignar; Okke Batelaan; Tomasz Okruszko. Wetlands in flux: looking for the drivers in a central European case. Wetlands Ecology and Management 2018, 26, 849 -863.
AMA StyleTomasz Berezowski, Martin Wassen, Jan Szatyłowicz, Jarosław Chormański, Stefan Ignar, Okke Batelaan, Tomasz Okruszko. Wetlands in flux: looking for the drivers in a central European case. Wetlands Ecology and Management. 2018; 26 (5):849-863.
Chicago/Turabian StyleTomasz Berezowski; Martin Wassen; Jan Szatyłowicz; Jarosław Chormański; Stefan Ignar; Okke Batelaan; Tomasz Okruszko. 2018. "Wetlands in flux: looking for the drivers in a central European case." Wetlands Ecology and Management 26, no. 5: 849-863.
Leaf CA measurement should take into account angle variation during measurement time. Leaf wettability of common deciduous forest plants is characterized by wetting contact angles ranging from 60° to 140° with a significant variation between species of the same family. Leaf wettability is an important phenomenon that has an influence on several processes such as the hydrological cycle, plant pathogen growth, or pollutant and pesticide absorption/deposition. The main objective of this research was to investigate the leaf wettability differences of 19 species (16 trees and 3 shrubs) of deciduous plants commonly occurring in Polish forests (temperate climate). The measurements were gathered as follows: 20 undamaged leaves were selected for each species and the wettability was determined by contact angle measurements with an optical goniometer CAM 100 using the sessile drop method. The contact angle was measured with 1-s intervals during 2 min from droplet deposition on adaxial and abaxial leaf surface. Laboratory analyses were completed during the summer of 2016 during full vegetation growth. A general CA decrease with time was observed on both leaf sides. The contact angle values ranged from 60° to 140° depending on species and leaf side. Differences between contact angle values at the beginning and the end of measurement reached 23.6° and engendered changes of wetting classes for some species. In many cases, no wettability class change was observed despite a CA lowering of 20°. The abaxial side was found to be the more repellent for 14 out of 19 species. Altogether, the leaves were classified from highly wettable to highly non-wettable, probably depending on the plant-survival strategy.
Ewa Papierowska; Sylwia Szporak-Wasilewska; Joanna Szewińska; Jan Szatyłowicz; Guillaume Debaene; Marta Utratna. Contact angle measurements and water drop behavior on leaf surface for several deciduous shrub and tree species from a temperate zone. Trees 2018, 32, 1253 -1266.
AMA StyleEwa Papierowska, Sylwia Szporak-Wasilewska, Joanna Szewińska, Jan Szatyłowicz, Guillaume Debaene, Marta Utratna. Contact angle measurements and water drop behavior on leaf surface for several deciduous shrub and tree species from a temperate zone. Trees. 2018; 32 (5):1253-1266.
Chicago/Turabian StyleEwa Papierowska; Sylwia Szporak-Wasilewska; Joanna Szewińska; Jan Szatyłowicz; Guillaume Debaene; Marta Utratna. 2018. "Contact angle measurements and water drop behavior on leaf surface for several deciduous shrub and tree species from a temperate zone." Trees 32, no. 5: 1253-1266.
Ewa Papierowska; Wojciech Matysiak; Jan Szatyłowicz; Guillaume Debaene; Emilia Urbanek; Barbara Kalisz; Andrzej Łachacz. Compatibility of methods used for soil water repellency determination for organic and organo-mineral soils. Geoderma 2018, 314, 221 -231.
AMA StyleEwa Papierowska, Wojciech Matysiak, Jan Szatyłowicz, Guillaume Debaene, Emilia Urbanek, Barbara Kalisz, Andrzej Łachacz. Compatibility of methods used for soil water repellency determination for organic and organo-mineral soils. Geoderma. 2018; 314 ():221-231.
Chicago/Turabian StyleEwa Papierowska; Wojciech Matysiak; Jan Szatyłowicz; Guillaume Debaene; Emilia Urbanek; Barbara Kalisz; Andrzej Łachacz. 2018. "Compatibility of methods used for soil water repellency determination for organic and organo-mineral soils." Geoderma 314, no. : 221-231.
The contamination of soil with petroleum products is a major environmental problem. Petroleum products are common soil contaminants as a result of human activities, and they are causing substantial changes in the biological (particularly microbiological) processes, chemical composition, structure and physical properties of soil. The main objective of this study was to assess the impact of soil moisture on CO2 efflux from diesel-contaminated albic podzol soils. Two contamination treatments (3000 and 9000 mg of diesel oil per kg of soil) were prepared for four horizons from two forest study sites with different initial levels of soil water repellency. CO2 emissions were measured using a portable infrared gas analyser (LCpro+, ADC BioScientific, UK) while the soil samples were drying under laboratory conditions (from saturation to air-dry). The assessment of soil water repellency was performed using the water drop penetration time test. An analysis of variance (ANVOA) was conducted for the CO2 efflux data. The obtained results show that CO2 efflux from diesel-contaminated soils is higher than efflux from uncontaminated soils. The initially water-repellent soils were found to have a bigger CO2 efflux. The non-linear relationship between soil moisture content and CO2 efflux only existed for the upper soil horizons, while for deeper soil horizons, the efflux is practically independent of soil moisture content. The contamination of soil by diesel leads to increased soil water repellency.
Edyta Hewelke; Jan Szatyłowicz; Piotr Hewelke; Tomasz Gnatowski; Rufat Aghalarov. The Impact of Diesel Oil Pollution on the Hydrophobicity and CO2 Efflux of Forest Soils. Water, Air, & Soil Pollution 2018, 229, 1 -11.
AMA StyleEdyta Hewelke, Jan Szatyłowicz, Piotr Hewelke, Tomasz Gnatowski, Rufat Aghalarov. The Impact of Diesel Oil Pollution on the Hydrophobicity and CO2 Efflux of Forest Soils. Water, Air, & Soil Pollution. 2018; 229 (2):1-11.
Chicago/Turabian StyleEdyta Hewelke; Jan Szatyłowicz; Piotr Hewelke; Tomasz Gnatowski; Rufat Aghalarov. 2018. "The Impact of Diesel Oil Pollution on the Hydrophobicity and CO2 Efflux of Forest Soils." Water, Air, & Soil Pollution 229, no. 2: 1-11.
Leaf surface wetness has numerous physiological and ecological consequences, and the morphological structures on the leaf surface can affect its extent and duration, contributing to interception rates in the scale of the whole ecosystem. Wetland plants have developed morphological adaptations to high water level allowing them to avoid water excess. Droplet contact angle and surface free energy are measurable parameters which relate to how the plant influences water usage and redistribution. We analysed patterns of contact angle and the surface free energy of the adaxial and abaxial surface of 10 wetland plant species and related them to the optimal habitat conditions and functional traits of the plants. Despite the consistent environment of these plants, we found them to vary greatly in terms of leaf surface wettability and surface free energy, with contact angles ranging from 75 to 169° and surface free energy, from 1.32 to 30.38 mJ/m2. Canopy height and leaf longevity were significantly correlated to leaf wettability, whilst SLA (Specific Leaf Area) and leaf shape were not related to hydrophobicity. Investigating adaptations of wetland plants to their environment showed that including wettability and surface free energy in combination with other plant traits improves our understanding of water plant-soil-water interactions in wetland habitats.
Daria Sikorska; Ewa Papierowska; Jan Szatyłowicz; Piotr Sikorski; Katarzyna Suprun; Richard Hopkins. Variation in Leaf Surface Hydrophobicity of Wetland Plants: the Role of Plant Traits in Water Retention. Wetlands 2017, 37, 997 -1002.
AMA StyleDaria Sikorska, Ewa Papierowska, Jan Szatyłowicz, Piotr Sikorski, Katarzyna Suprun, Richard Hopkins. Variation in Leaf Surface Hydrophobicity of Wetland Plants: the Role of Plant Traits in Water Retention. Wetlands. 2017; 37 (5):997-1002.
Chicago/Turabian StyleDaria Sikorska; Ewa Papierowska; Jan Szatyłowicz; Piotr Sikorski; Katarzyna Suprun; Richard Hopkins. 2017. "Variation in Leaf Surface Hydrophobicity of Wetland Plants: the Role of Plant Traits in Water Retention." Wetlands 37, no. 5: 997-1002.
The aim of this study is to present the research results on the water retention of green roof on the example of a facility located in the district of Ursynów, Capital City Warsaw. The experimental site was a fragment of green patio of 25 cm substrate thickness which is a mixture of peat, sand and gravelite. Green roof area is overgrown with a mixture of grasses as well as conifers and deciduous bushes. The components of the water balance during the growing season of 2008 were calculated using the GreenRoof model. Performed studies have shown that the examined green roof retain more than 99% of water from rainfall.
Daniel Szejba; Tomasz Gnatowski; Jan Szatyłowicz. Bilans wodny zielonego dachu na przykładzie obiektu w dzielnicy Ursynów m.st. Warszawy. Przegląd Naukowy Inżynieria i Kształtowanie Środowiska 2017, 26, 66 -74.
AMA StyleDaniel Szejba, Tomasz Gnatowski, Jan Szatyłowicz. Bilans wodny zielonego dachu na przykładzie obiektu w dzielnicy Ursynów m.st. Warszawy. Przegląd Naukowy Inżynieria i Kształtowanie Środowiska. 2017; 26 (1):66-74.
Chicago/Turabian StyleDaniel Szejba; Tomasz Gnatowski; Jan Szatyłowicz. 2017. "Bilans wodny zielonego dachu na przykładzie obiektu w dzielnicy Ursynów m.st. Warszawy." Przegląd Naukowy Inżynieria i Kształtowanie Środowiska 26, no. 1: 66-74.
Agricultural soil maps were created to facilitate the management of fields. Such maps, at very large scale (1:5000), cover almost the entire agricultural land in Poland. These maps can be very useful for precision field management. However, they were prepared about 40–50 years ago using old mapping techniques with mainly field (organoleptic) examination of soil. For this reason it is necessary to verify agreement between such maps with the current soil status. In the case of detection of disagreements it is important to identify the causes and propose methods for improving soil maps. Only few studies were made in this aspect. The soil texture (ST) of the upper layer, as presented on the agricultural soil maps from the 1960s and 1970s, was compared with the actual ST of the same four fields in northern and central Poland. For laboratory ST determination, soil samples were collected in a dense sampling network. On average, the agreement of the ST presented on the agricultural soil maps and determined in this study was classified as medium for three fields and good for one field. However, the presence of field areas with poor agreement between the ST determined in this study and that shown on the agricultural maps was detected in all investigated fields. Identified causes for this comprised imprecision of ST determination using the organoleptic method, the generalization of the soil quality maps, and erosion processes during the years between soil mapping and this investigation. The improvement of ST presentation on the large scale soil maps might be achieved by quite denser soil sampling for ST analysis supported by ECa, yield and NDVI maps.
Michał Stępień; Dariusz Gozdowski; Stanisław Samborski; Eike Stefan Dobers; Jan Szatyłowicz; Jarosław Chormański. Validation of topsoil texture derived from agricultural soil maps by current dense soil sampling. Journal of Plant Nutrition and Soil Science 2016, 179, 618 -629.
AMA StyleMichał Stępień, Dariusz Gozdowski, Stanisław Samborski, Eike Stefan Dobers, Jan Szatyłowicz, Jarosław Chormański. Validation of topsoil texture derived from agricultural soil maps by current dense soil sampling. Journal of Plant Nutrition and Soil Science. 2016; 179 (5):618-629.
Chicago/Turabian StyleMichał Stępień; Dariusz Gozdowski; Stanisław Samborski; Eike Stefan Dobers; Jan Szatyłowicz; Jarosław Chormański. 2016. "Validation of topsoil texture derived from agricultural soil maps by current dense soil sampling." Journal of Plant Nutrition and Soil Science 179, no. 5: 618-629.
Michał Stępień; Stanisław Samborski; Dariusz Gozdowski; Eike Stefan Dobers; Jarosław Chormański; Jan Szatyłowicz. Assessment of soil texture class on agricultural fields using ECa, Amber NDVI, and topographic properties. Journal of Plant Nutrition and Soil Science 2015, 178, 523 -536.
AMA StyleMichał Stępień, Stanisław Samborski, Dariusz Gozdowski, Eike Stefan Dobers, Jarosław Chormański, Jan Szatyłowicz. Assessment of soil texture class on agricultural fields using ECa, Amber NDVI, and topographic properties. Journal of Plant Nutrition and Soil Science. 2015; 178 (3):523-536.
Chicago/Turabian StyleMichał Stępień; Stanisław Samborski; Dariusz Gozdowski; Eike Stefan Dobers; Jarosław Chormański; Jan Szatyłowicz. 2015. "Assessment of soil texture class on agricultural fields using ECa, Amber NDVI, and topographic properties." Journal of Plant Nutrition and Soil Science 178, no. 3: 523-536.
Mateusz Grygoruk; Okke Batelaan; Dorota Mirosław-Świątek; Jan Szatyłowicz; Tomasz Okruszko. Evapotranspiration of bush encroachments on a temperate mire meadow – A nonlinear function of landscape composition and groundwater flow. Ecological Engineering 2014, 73, 598 -609.
AMA StyleMateusz Grygoruk, Okke Batelaan, Dorota Mirosław-Świątek, Jan Szatyłowicz, Tomasz Okruszko. Evapotranspiration of bush encroachments on a temperate mire meadow – A nonlinear function of landscape composition and groundwater flow. Ecological Engineering. 2014; 73 ():598-609.
Chicago/Turabian StyleMateusz Grygoruk; Okke Batelaan; Dorota Mirosław-Świątek; Jan Szatyłowicz; Tomasz Okruszko. 2014. "Evapotranspiration of bush encroachments on a temperate mire meadow – A nonlinear function of landscape composition and groundwater flow." Ecological Engineering 73, no. : 598-609.
The proper delineation of management zones (MZs) is very important in site-specific crop management. The aim of this study was to determine the soil attributes that are most relevant in the delineation process of MZs. Two fields of 22 ha and 45 ha located in northern Poland were examined. The analyses were based on MZs delineated using standardized multiyear yield data and logistic regression, which was applied to select the variables that discriminate the yield-based MZs to the greatest degree. The effects of several variables, including soil chemical and physical properties and topographic attributes, on the discrimination of yield-based MZs were investigated. The sand and organic carbon content in the soil produced the most relevant delineation of MZs. Highly correlated variables should be not included in analyses for MZ delineation because they can strongly affect the results of cluster analyses that are used for the delineation of MZs.
Dariusz Gozdowski; Michał Stępień; Stanisław Samborski; Eike Stefan Dobers; Jan Szatyłowicz; Jarosław Chormański. Determination of the Most Relevant Soil Properties for the Delineation of Management Zones in Production Fields. Communications in Soil Science and Plant Analysis 2014, 45, 2289 -2304.
AMA StyleDariusz Gozdowski, Michał Stępień, Stanisław Samborski, Eike Stefan Dobers, Jan Szatyłowicz, Jarosław Chormański. Determination of the Most Relevant Soil Properties for the Delineation of Management Zones in Production Fields. Communications in Soil Science and Plant Analysis. 2014; 45 (17):2289-2304.
Chicago/Turabian StyleDariusz Gozdowski; Michał Stępień; Stanisław Samborski; Eike Stefan Dobers; Jan Szatyłowicz; Jarosław Chormański. 2014. "Determination of the Most Relevant Soil Properties for the Delineation of Management Zones in Production Fields." Communications in Soil Science and Plant Analysis 45, no. 17: 2289-2304.
Edyta Hewelke; Jan Szatyłowicz; Tomasz Gnatowski; Ryszard Oleszczuk. Effects of Soil Water Repellency on Moisture Patterns in a Degraded Sapric Histosol. Land Degradation & Development 2014, 27, 955 -964.
AMA StyleEdyta Hewelke, Jan Szatyłowicz, Tomasz Gnatowski, Ryszard Oleszczuk. Effects of Soil Water Repellency on Moisture Patterns in a Degraded Sapric Histosol. Land Degradation & Development. 2014; 27 (4):955-964.
Chicago/Turabian StyleEdyta Hewelke; Jan Szatyłowicz; Tomasz Gnatowski; Ryszard Oleszczuk. 2014. "Effects of Soil Water Repellency on Moisture Patterns in a Degraded Sapric Histosol." Land Degradation & Development 27, no. 4: 955-964.
See Soil Penetrability, Effect on Animal Burrowing; Soil Penetrometers and Penetrability
Andrzej Mocek; Wojciech Owczarzak; Michael Glenn; Tadeusz J. Chmielewski; Danuta Urban; Lech Wojciech Szajdak; Jan Szatyłowicz; Raimo Kõlli; Yakov A. Pachepsky; Martinus Th. Van Genuchten; Winfried E. H. Blum; Wojciech Skierucha; Marcin Widomski; Witold Stepniewski; Bogusław Usowicz; Marek Molenda; Martin G. Scanlon; Bohdan Dobrzanski; Rafał Rybczyński; Johan Bouma; Tiphaine Chevallier; Stefan Skiba; Toshko Raytchev; Svetla Rousseva; Evgeny V. Shein; Tatiana A. Arkhangelskaya; Tomasz Rusin; Paweł Kojs; Anyela Valentina Camargo Rodriguez; Jan T. Kim; Istvan Farkas; Grażyna Podolska; Bogusław Szot; Wojciech Rybiński; Sekhar Lukose Kuriakose; L. P. H. Van Beek; A. Pierret; C. J. Moran; Piotr Baranowski; Fernando Migliaccio; Alessio Fortunati; Paola Tassone; Tiina Roose; Marcello Pagliai; Miroslav Kutílek; Mieczysław Hajnos; Viacheslav I. Adamchuk; Raphael A. Viscarra Rossel; Evgenia Blagodatskaya; Yakov Kuzyakov; Gabriele E. Schaumann; Gunnar Kirchhof; T. P. Tuong; H. B. So. Penetrability. Encyclopedia of Solid Earth Geophysics 2011, 561 -561.
AMA StyleAndrzej Mocek, Wojciech Owczarzak, Michael Glenn, Tadeusz J. Chmielewski, Danuta Urban, Lech Wojciech Szajdak, Jan Szatyłowicz, Raimo Kõlli, Yakov A. Pachepsky, Martinus Th. Van Genuchten, Winfried E. H. Blum, Wojciech Skierucha, Marcin Widomski, Witold Stepniewski, Bogusław Usowicz, Marek Molenda, Martin G. Scanlon, Bohdan Dobrzanski, Rafał Rybczyński, Johan Bouma, Tiphaine Chevallier, Stefan Skiba, Toshko Raytchev, Svetla Rousseva, Evgeny V. Shein, Tatiana A. Arkhangelskaya, Tomasz Rusin, Paweł Kojs, Anyela Valentina Camargo Rodriguez, Jan T. Kim, Istvan Farkas, Grażyna Podolska, Bogusław Szot, Wojciech Rybiński, Sekhar Lukose Kuriakose, L. P. H. Van Beek, A. Pierret, C. J. Moran, Piotr Baranowski, Fernando Migliaccio, Alessio Fortunati, Paola Tassone, Tiina Roose, Marcello Pagliai, Miroslav Kutílek, Mieczysław Hajnos, Viacheslav I. Adamchuk, Raphael A. Viscarra Rossel, Evgenia Blagodatskaya, Yakov Kuzyakov, Gabriele E. Schaumann, Gunnar Kirchhof, T. P. Tuong, H. B. So. Penetrability. Encyclopedia of Solid Earth Geophysics. 2011; ():561-561.
Chicago/Turabian StyleAndrzej Mocek; Wojciech Owczarzak; Michael Glenn; Tadeusz J. Chmielewski; Danuta Urban; Lech Wojciech Szajdak; Jan Szatyłowicz; Raimo Kõlli; Yakov A. Pachepsky; Martinus Th. Van Genuchten; Winfried E. H. Blum; Wojciech Skierucha; Marcin Widomski; Witold Stepniewski; Bogusław Usowicz; Marek Molenda; Martin G. Scanlon; Bohdan Dobrzanski; Rafał Rybczyński; Johan Bouma; Tiphaine Chevallier; Stefan Skiba; Toshko Raytchev; Svetla Rousseva; Evgeny V. Shein; Tatiana A. Arkhangelskaya; Tomasz Rusin; Paweł Kojs; Anyela Valentina Camargo Rodriguez; Jan T. Kim; Istvan Farkas; Grażyna Podolska; Bogusław Szot; Wojciech Rybiński; Sekhar Lukose Kuriakose; L. P. H. Van Beek; A. Pierret; C. J. Moran; Piotr Baranowski; Fernando Migliaccio; Alessio Fortunati; Paola Tassone; Tiina Roose; Marcello Pagliai; Miroslav Kutílek; Mieczysław Hajnos; Viacheslav I. Adamchuk; Raphael A. Viscarra Rossel; Evgenia Blagodatskaya; Yakov Kuzyakov; Gabriele E. Schaumann; Gunnar Kirchhof; T. P. Tuong; H. B. So. 2011. "Penetrability." Encyclopedia of Solid Earth Geophysics , no. : 561-561.
See Physical Properties as Indicators of Food Quality; Agrophysical Properties and Processes; Agrophysics: Physics Applied to Agriculture; Physical Properties of Raw Materials and...
Andrzej Mocek; Wojciech Owczarzak; Michael Glenn; Tadeusz J. Chmielewski; Danuta Urban; Lech Wojciech Szajdak; Jan Szatyłowicz; Raimo Kõlli; Yakov A. Pachepsky; Martinus Th. Van Genuchten; Winfried E. H. Blum; Wojciech Skierucha; Marcin Widomski; Witold Stepniewski; Bogusław Usowicz; Marek Molenda; Martin G. Scanlon; Bohdan Dobrzanski; Rafał Rybczyński; Johan Bouma; Tiphaine Chevallier; Stefan Skiba; Toshko Raytchev; Svetla Rousseva; Evgeny V. Shein; Tatiana A. Arkhangelskaya; Tomasz Rusin; Paweł Kojs; Anyela Valentina Camargo Rodriguez; Jan T. Kim; Istvan Farkas; Grażyna Podolska; Bogusław Szot; Wojciech Rybiński; Sekhar Lukose Kuriakose; L. P. H. Van Beek; A. Pierret; C. J. Moran; Piotr Baranowski; Fernando Migliaccio; Alessio Fortunati; Paola Tassone; Tiina Roose; Marcello Pagliai; Miroslav Kutílek; Mieczysław Hajnos; Viacheslav I. Adamchuk; Raphael A. Viscarra Rossel; Evgenia Blagodatskaya; Yakov Kuzyakov; Gabriele E. Schaumann; Gunnar Kirchhof; T. P. Tuong; H. B. So; Józef Horabik. Physical Properties. Encyclopedia of Solid Earth Geophysics 2011, 573 -573.
AMA StyleAndrzej Mocek, Wojciech Owczarzak, Michael Glenn, Tadeusz J. Chmielewski, Danuta Urban, Lech Wojciech Szajdak, Jan Szatyłowicz, Raimo Kõlli, Yakov A. Pachepsky, Martinus Th. Van Genuchten, Winfried E. H. Blum, Wojciech Skierucha, Marcin Widomski, Witold Stepniewski, Bogusław Usowicz, Marek Molenda, Martin G. Scanlon, Bohdan Dobrzanski, Rafał Rybczyński, Johan Bouma, Tiphaine Chevallier, Stefan Skiba, Toshko Raytchev, Svetla Rousseva, Evgeny V. Shein, Tatiana A. Arkhangelskaya, Tomasz Rusin, Paweł Kojs, Anyela Valentina Camargo Rodriguez, Jan T. Kim, Istvan Farkas, Grażyna Podolska, Bogusław Szot, Wojciech Rybiński, Sekhar Lukose Kuriakose, L. P. H. Van Beek, A. Pierret, C. J. Moran, Piotr Baranowski, Fernando Migliaccio, Alessio Fortunati, Paola Tassone, Tiina Roose, Marcello Pagliai, Miroslav Kutílek, Mieczysław Hajnos, Viacheslav I. Adamchuk, Raphael A. Viscarra Rossel, Evgenia Blagodatskaya, Yakov Kuzyakov, Gabriele E. Schaumann, Gunnar Kirchhof, T. P. Tuong, H. B. So, Józef Horabik. Physical Properties. Encyclopedia of Solid Earth Geophysics. 2011; ():573-573.
Chicago/Turabian StyleAndrzej Mocek; Wojciech Owczarzak; Michael Glenn; Tadeusz J. Chmielewski; Danuta Urban; Lech Wojciech Szajdak; Jan Szatyłowicz; Raimo Kõlli; Yakov A. Pachepsky; Martinus Th. Van Genuchten; Winfried E. H. Blum; Wojciech Skierucha; Marcin Widomski; Witold Stepniewski; Bogusław Usowicz; Marek Molenda; Martin G. Scanlon; Bohdan Dobrzanski; Rafał Rybczyński; Johan Bouma; Tiphaine Chevallier; Stefan Skiba; Toshko Raytchev; Svetla Rousseva; Evgeny V. Shein; Tatiana A. Arkhangelskaya; Tomasz Rusin; Paweł Kojs; Anyela Valentina Camargo Rodriguez; Jan T. Kim; Istvan Farkas; Grażyna Podolska; Bogusław Szot; Wojciech Rybiński; Sekhar Lukose Kuriakose; L. P. H. Van Beek; A. Pierret; C. J. Moran; Piotr Baranowski; Fernando Migliaccio; Alessio Fortunati; Paola Tassone; Tiina Roose; Marcello Pagliai; Miroslav Kutílek; Mieczysław Hajnos; Viacheslav I. Adamchuk; Raphael A. Viscarra Rossel; Evgenia Blagodatskaya; Yakov Kuzyakov; Gabriele E. Schaumann; Gunnar Kirchhof; T. P. Tuong; H. B. So; Józef Horabik. 2011. "Physical Properties." Encyclopedia of Solid Earth Geophysics , no. : 573-573.
See Soil Compactibility and Compressibility
Andrzej Mocek; Wojciech Owczarzak; Michael Glenn; Tadeusz J. Chmielewski; Danuta Urban; Lech Wojciech Szajdak; Jan Szatyłowicz; Raimo Kõlli; Yakov A. Pachepsky; Martinus Th. Van Genuchten; Winfried E. H. Blum; Wojciech Skierucha; Marcin Widomski; Witold Stepniewski; Bogusław Usowicz; Marek Molenda; Martin G. Scanlon; Bohdan Dobrzanski; Rafał Rybczyński; Johan Bouma; Tiphaine Chevallier; Stefan Skiba; Toshko Raytchev; Svetla Rousseva; Evgeny V. Shein; Tatiana A. Arkhangelskaya; Tomasz Rusin; Paweł Kojs; Anyela Valentina Camargo Rodriguez; Jan T. Kim; Istvan Farkas; Grażyna Podolska; Bogusław Szot; Wojciech Rybiński; Sekhar Lukose Kuriakose; L. P. H. Van Beek; A. Pierret; C. J. Moran; Piotr Baranowski; Fernando Migliaccio; Alessio Fortunati; Paola Tassone; Tiina Roose; Marcello Pagliai; Miroslav Kutílek; Mieczysław Hajnos; Viacheslav I. Adamchuk; Raphael A. Viscarra Rossel; Evgenia Blagodatskaya; Yakov Kuzyakov; Gabriele E. Schaumann; Gunnar Kirchhof; T. P. Tuong; H. B. So. Plate Sinkage Test. Encyclopedia of Solid Earth Geophysics 2011, 639 -639.
AMA StyleAndrzej Mocek, Wojciech Owczarzak, Michael Glenn, Tadeusz J. Chmielewski, Danuta Urban, Lech Wojciech Szajdak, Jan Szatyłowicz, Raimo Kõlli, Yakov A. Pachepsky, Martinus Th. Van Genuchten, Winfried E. H. Blum, Wojciech Skierucha, Marcin Widomski, Witold Stepniewski, Bogusław Usowicz, Marek Molenda, Martin G. Scanlon, Bohdan Dobrzanski, Rafał Rybczyński, Johan Bouma, Tiphaine Chevallier, Stefan Skiba, Toshko Raytchev, Svetla Rousseva, Evgeny V. Shein, Tatiana A. Arkhangelskaya, Tomasz Rusin, Paweł Kojs, Anyela Valentina Camargo Rodriguez, Jan T. Kim, Istvan Farkas, Grażyna Podolska, Bogusław Szot, Wojciech Rybiński, Sekhar Lukose Kuriakose, L. P. H. Van Beek, A. Pierret, C. J. Moran, Piotr Baranowski, Fernando Migliaccio, Alessio Fortunati, Paola Tassone, Tiina Roose, Marcello Pagliai, Miroslav Kutílek, Mieczysław Hajnos, Viacheslav I. Adamchuk, Raphael A. Viscarra Rossel, Evgenia Blagodatskaya, Yakov Kuzyakov, Gabriele E. Schaumann, Gunnar Kirchhof, T. P. Tuong, H. B. So. Plate Sinkage Test. Encyclopedia of Solid Earth Geophysics. 2011; ():639-639.
Chicago/Turabian StyleAndrzej Mocek; Wojciech Owczarzak; Michael Glenn; Tadeusz J. Chmielewski; Danuta Urban; Lech Wojciech Szajdak; Jan Szatyłowicz; Raimo Kõlli; Yakov A. Pachepsky; Martinus Th. Van Genuchten; Winfried E. H. Blum; Wojciech Skierucha; Marcin Widomski; Witold Stepniewski; Bogusław Usowicz; Marek Molenda; Martin G. Scanlon; Bohdan Dobrzanski; Rafał Rybczyński; Johan Bouma; Tiphaine Chevallier; Stefan Skiba; Toshko Raytchev; Svetla Rousseva; Evgeny V. Shein; Tatiana A. Arkhangelskaya; Tomasz Rusin; Paweł Kojs; Anyela Valentina Camargo Rodriguez; Jan T. Kim; Istvan Farkas; Grażyna Podolska; Bogusław Szot; Wojciech Rybiński; Sekhar Lukose Kuriakose; L. P. H. Van Beek; A. Pierret; C. J. Moran; Piotr Baranowski; Fernando Migliaccio; Alessio Fortunati; Paola Tassone; Tiina Roose; Marcello Pagliai; Miroslav Kutílek; Mieczysław Hajnos; Viacheslav I. Adamchuk; Raphael A. Viscarra Rossel; Evgenia Blagodatskaya; Yakov Kuzyakov; Gabriele E. Schaumann; Gunnar Kirchhof; T. P. Tuong; H. B. So. 2011. "Plate Sinkage Test." Encyclopedia of Solid Earth Geophysics , no. : 639-639.