scholarly journals Pidsolic-peat soils of Nadsyanya plain

Author(s):  
Volodymyr Haskevych ◽  
Olena Lutsishin

The results of field and laboratory studies pidsolic-peat soils Nadsanya plains were shown. The characteristics of geography, morphological peculiarities, physical and physical-chemical properties, agroecological state of soils were given. The event of management and protection of pidsolic-peat soils were examined. Key words: pidsolic-peat soil, morphological peculiarities, granulometric composition, structure, humus, degradation, soil protection.

Author(s):  
Volodymyr Gaskevych ◽  
Maria Netzyk

The characteristic of the genetic and geographic features of peat soils of Small Polissya was done. The geography of peat soils was outlined on the results of field and laboratory studies. Morphological structure, physical and physical-chemical properties of peat soils were analyzed. The current agroecological status of peat soil and the measures of the rational use and protection were considered. Key words: peat soils, peat, geography of peat soils, morphological features, drainage, degradation, soil protection.


2019 ◽  
Vol 14 (1) ◽  
pp. 20-34
Author(s):  
T. G. RYASHCHENKO ◽  
N. N. UKHOVA ◽  
S. I. SHTELMAKH ◽  
N. I. BELYANINA ◽  
P. S. BELYANIN

The article considers the study results of composition, microstructure and physical-chemical properties of the quaternary clays of the Prikhankayskaya depression in district of the lake Khanka (Primorye) on the example of air-dry samples of geological borehole 45-b in the range of 18–62 m. The objective of research was to obtain new information about the properties of widespread clay sediments in this area using geologic-lithological materials and laboratory data. The schematic geologic-lithological column was composed with the selection of various zones in the quaternary clay sediments section and the border with sediments of the Neogene System. The methodological scheme of laboratory studies of clays was proposed. This scheme includes the determination of chemical and microelement composition, clay minerals, contents of carbonates, water-soluble salts, mobile forms of aluminum oxide, humus, as well as microstructural parameters (method «Microstructure») and some physical-chemical properties. Geochemical coefficients (Kz, CIA, CIW, ICV) determined the degree of chemical maturity of clays and confirmed the results of palynological studies reflecting the fluctuations of the climatic conditions of their formation. For the group of toxic microelements for the first time the special indicator (Zc) was calculated. Which was the criterion for a degree of pollution of the clay sediments section. Clay minerals of the quaternary clays are represented by smectite and hydromica. The clear change in the mineral association was found when passing to the Neogene sediments (kaolinite prevails). The method «Microstructure» revealed the aggregated type of clays microstructure, the domination of the particles of coarse dust fraction among the primary (free) particles and the almost complete absence of the particles of fine-grained sand fraction, the participation of various fractions in the composition of aggregates. The variants of the formation of certain types of aggregates (on sizes) in the fluviolacustrine «khankayskiy» clays are presented. Solid part density, water resistance (soaking time), sedimentation volume, plasticity, relative swelling (samples-pastes) were determined using standard methods for clays. By special methods, the cation exchange capacity was measured and the calculated values of the plasticity index were obtained from forecasting formulas using the yield limit. The proposed methodological scheme of complex laboratory studies of clay sediments can be recommended for problematic geologic-lithological and engineering-geological sections.


Author(s):  
V. Haskevych ◽  
M. Netsyk

Results of the studies of vegetation of lowland peats and on pyrogenically degraded peat soils of Small Polissya have been presented. It has been stated that the change of physical and physical-chemical characteristics of pyrogenic substrate is reflected on species and genus of composition of vegetation cover. It has been ascertained that the most essential changes of qualitative composition of vegetation occur within two-three years after the fire. Peculiarities of pyrogenic formation increase in postpyrogenic period have been characterized. Key words: peat soils, pyrogenic degradation, pyrogenic formations, physical and physical-chemical features, plants-pioneers, vegetation cover.


2019 ◽  
Vol 70 (1) ◽  
pp. 278-282 ◽  
Author(s):  
Diana Puiu ◽  
Mariana Popescu ◽  
Marcela Niculescu ◽  
Luoana Florentina Pascu ◽  
Toma Galaon ◽  
...  

The fate of organochlorine compounds in soil ecosystem is shaped by their physical-chemical properties and by environmental conditions. The high persistence of polychlorobiphenyls (PCBs) in soil is given by a slow degradation which varies from months to years (the half-life of PCB 28 is 10.9 years, and PCB 52, 11.2 years). Due to high lipophilicity, these carcinogenic compounds can be easily uptaken by plants and transferred to the food chain. The widespread use of medicinal plant, Mentha Piperita, in pharmaceutical and food industry represents a risk of contamination and pollution. Through laboratory studies, we worked to identify the chemical behavior in soil and plants of some PCB congeners: 28, 52, 138, 153 and 180). The compounds mobility from soil to the roots and then through plant was monitored for 5 weeks. By optimizing the analytical method the contaminants were determined from soil and plant with good recoveries and with reduced limit of detection, below 0.01 mg/kg. It was reported that usually are uptaken into the plant high chlorinated PCBs like PCB 153 and PCB 180 but this study shows that after 5 weeks of PCB application, the concentration of PCB 28, a trichlorobiphenyl, is increasing. Fortunately, calculating the bioconcentration factor (BCF) of the selected PCBs in roots, it was shown that is similar to BCF of other plants like poplar and zucchini. The obtained value of 0.2 is assessed as being low.


2020 ◽  
Vol 2 (2) ◽  
pp. 86-100
Author(s):  
Eko Kurniawan ◽  
Nelvia Nelvia ◽  
Wawan Wawan

 Planting of oil palm in peatland has been limited by soil physical, chemical properties, and hydrology, that`s way needed improvement on those matters to increase the productivity of peat and oil palm in peat soil by compacting. The purpose of this compacting is to improve the soil's physical, chemical properties, and soil moisture. A sampling of soil, water, and leaf were done in consecutive block 5,4,3,2,1,0 year after compacting and of planting done 4 years 10 months, 3 years  9 months, 2 years 9 months, 1 year 10 months, 11 months and 2 months, control used in this trial are origin condition (forest). Increasing bulk density was found at compacting block with 30 cm depth from the surface with the lower in 2 years after compacting at 0.09 g/cm3 and highest 4 years after compacting 0.4 g/cm3. In-depth of 60 cm from surface was found no increasing the bulk density 3 years after compacting 0.0 g/cm3 and the highest on 5 years after compacting 0.3 g/cm3 compared to forest. Decreasing on permeability in-depth 30 cm at 4 years after compacting 7.47 cm/jam and close to forest permeability 51.11 cm/hour is  2 years  43.6 cm/hour. As represent rise capillary consistently water content ≥ 80% achieved at depth 20 cm of surfaces on all block. Compaction doesn't regard pH, C organic, basa's saturation, capacity exchange cation. On depth 30 cm  P-total lower  on s without compaction at  599.6 ppm and above 871.6 ppm on 5 yr than forest 585 ppm.  P available most low 58.1 ppm happens on 4 yr afters is compacted and p available forest 53.9 ppm. Nutrient content B, Cu and Zn at soil not influenced by compaction. Fosfor (P) in water increases with added years after compaction lower at 39.1 mg/L  in the block without compaction compare  of forest that 40.8 mg/L. Leaf nutrient rate on compacted block on optimum until excess where N (2. 69 – 3.15 %) , P (0. 170 – 0.209 %) , K( 0. 952 – 1.11%) , Mg ( 0. 377 – 0.497%) , except  on block without compacting K (0. 830 %)  and Mg (0. 190%)  at deficiency and 0 years afters compaction Mg leaf on level deficiency 0. 230%. Nutrient content of  B, Cu and Zn at various level and not influenced  by compacting.


Author(s):  
Roman Semashchuk

Results of studies of key morphological, physical-chemical and chemical properties of underdeveloped carbonate soils, which are influenced by woody, herbaceous and agricultural plant formations on eluvium-delluvium carbonate rocks, were given. Key words: initial soils, morphological properties, physical and chemical properties, gross chemical analysis.


2020 ◽  
Vol 8 (3) ◽  
pp. 315
Author(s):  
Marinus Kristiadi Harun ◽  
Syaiful Anwar ◽  
Eka Intan Kumala Putri ◽  
Hadi Susilo Arifin

This study aims to: (1) determine the chemical properties of peat soils in 3 types of land cover in 2 physiographies; (2) find out water level fluctuations (WLF) on peat soils covered by agroforestry and horticulture in the physiography of peat dome and backswamp during the rainy season, transitions and drought. This research was conducted in January until December 2018 in Kahayan-Sebangau Peat Hidrological Unit, in the Kalampangan Vilagge. The results showed that differences in peat soil cover conditions at different physiographies affected chemical properties and WLF. The three types of peatland cover on both physiographic types of peatlands have a pH that categories into the very acid (<4.5). The results of this study indicate that nutrients (N, P, Kd, C, Mg, Al, Na and SO4) that are formed in each type of land cover in 2 physiographies indicate that these elements in peatlands are influenced by a layer of peat which obtains input of organic material from the plants above it. Peat fertility depends on the contribution of organic material from plants on it. Peatland cation exchange capacity values for all types are in the very high category (> 40). In addition to the chemical elements of the soil, the peat ground water level is highly volatile following rainfall so that during the peak of the dry season (MK) the WLF can reach 200 cm below the ground surface, and vice versa during the peak of the rainy season (MH) the WLF can inundate all peat soils.


2020 ◽  
Vol 9 (2) ◽  
pp. 81-87
Author(s):  
Maya Rahmayanti ◽  
Sri Juari Santosa ◽  
Sutarno Sutarno

Sonochemical technology is a technology that involves ultrasonic waves in chemical reactions. In this study, humic acid isolated from peat soil has been successfully modified with magnetite (HA-Fe3O4) using sonochemical technology. Characterization of the physical and chemical properties of HA-Fe3O4 was carried out using FTIR, XRD, SEM and VSM. HA-Fe3O4 was used for recovery of gold from simulated gold waste (HAuCl4). FTIR characterization showed that the interaction between HA and Fe3O4 was through hydrogen bonds. The crystal size of HA-Fe3O4 using the Debye-Scherrer equation based on the XRD diffractogram was 12.4 nm. The saturation magnetization value of HA-Fe3O4 obtained was 52.80 emu/g. Adsorption studies at various pH showed that HA-Fe3O4 has been successful in recovering of gold from simulated gold waste. The % recovery of gold was 99%. Gold recovery occurs through the adsorption process followed by reduction of Au (III) to Au(0).


2020 ◽  
Vol 2 (1) ◽  
pp. 6-14
Author(s):  
Luisa Madolyn Alvarez-Benaute ◽  

Currently, there are innumerable environmental technologies in the recovery of disturbed soils, including the use of leguminous plants that provide physical, chemical and biological improvements. The present investigation was based on evaluating the behavior of Sacha inchi (Plukenetia volubilis L. and Erythrina fusca Lour). under conditions of fertilization and densities and its contribution to the recovery of disturbed soils in the Monzón district. The method used was experimental in Design of Divided Plots (DPD) in Complete Blocks at Random 2 densities (DS1: 1666 and 1111 plants ha-1) x 4 (N1: 0-0-0, N2: 20-30-20, N3: 25-40-20 and N4: 40-60- 40) x 3 repetitions. The results indicate that the levels of fertilization N2, N3 and N4 produced a significant effect on the parameters of the vegetative characteristics of Plukenetia volubilis L, for the vegetative characteristics of Erythrina fusca evidence of AB interaction in the number of shoots at 5 months; the integration of both species achieved the improvement in the chemical properties of the soil. Like the reduction of aluminum by 30%, increase of p H by 5%, increase of potassium and phosphorus. Key words: Plukenetia volubilis L., Erythrina fusca Lour, fertilization, soil


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