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One of the bioindicators most often applied to assess the quality of soil is its enzymatic activity. Undesirable changes in the activity of enzymes can imply excessive presence of substances which are harmful to soil environment, such as heavy metals. Being a heavy metal, zinc is also an element essential for maintaining proper functions of live organisms. The purpose of this study has been to determine the significance of changes occurring in moderately heavy soil under the influence of zinc. The experiment was carried out in three replicates under laboratory conditions. Sandy loams of pH 5.5 and 7.0 were used for the trials. The soils were contaminated with zinc according to the following design: control (natural content), raised content (70 mg Zn2+ kg–1), weakly polluted (200 mg Zn2+ kg–1 ), moderately polluted (500 mg Zn2+ kg–1), heavily polluted (1,500 mg Zn2+ kg–1) and very heavily polluted soil (5,000 mg and 10,000 mg Zn2+ kg–1). The soil samples prepared as above were brought to the moisture content of 50% maximum water capacity and incubated at 25oC for 120 days. On day 30, 60 and 120, the activity of dehydrogenases, β-glucosidase, urease, acid phosphatase and arylsulphatase was determined. Based on these determinations, the following indices were calculated: ED50, the index for resistance (RS) and the index for resilience (RL). The tests have demonstrated that as the rate of soil contamination with zinc increased, the activity of all the analyzed enzymes was significantly depressed. The negative influence of zinc contamination on the activity of particular enzymes, irrespective of the soil pH, persisted throughout the whole experiment. In respect of their sensitivity to zinc, the enzymes can be ordered as follows: arylsulphatase > dehydrogenases > acid phosphatase > urease > β-glucosidase. Zinc contamination caused lasting changes in the soil environment, but the return to the state of equilibrium was the quickest in the case of dehydrogenases (RL = 0.276), less rapid for arylsulphatase (RL = 0.173) and the slowest for acid phosphatase (RL = 0.064). In contrast, the activity of urease, instead of regenerating, was increasingly disturbed (RL = 0.350). Soil acidification was the factor that most evidently exacerbated the negative influence of zinc on the activity of β-glucosidase and arylsulphatase. Values of ED50 for the activity of particular enzymes were varied. In the soil of pH 7.0, they ranged from 3,324 mg Zn2+ kg–1 for β-glucosidase to 412 mg Zn2+ kg–1 for dehydrogenases, and in the soil of pH 5.5, they varied from 1,008 Zn2+ kg–1 for β-glucosidase to 280 mg Zn2+ kg–1 for arylsulphatase.
Taking into account the progressive degradation of soils it is important to assess their quality. Soil quality depends on a large number of physical, chemical, biological and biochemical properties. In the publications available, there are presented three approaches regarding the use of soil properties to estimate soil quality: (1) the use of individual properties, (2) the use of simple indexes and (3) the use of complex indexes derived from combinations of different properties. The purpose of this study was to investigate the possibility to use enzymes as indicators of forest soil quality. Experimental plots (43) were located in central Poland. The study was carried out in a number of diverse fresh forest sites. To assess the quality of forest soils dehydrogenase and urease activity and the degree of base saturation were used. One of the final conclusions point out that enzymatic activity indicates current site condition as well as the changes that occur in soil better than soil physical and chemical properties. In other words, in comparison to soil enzymatic activity, soil physico-chemical properties constitute a less sensitive indicator of soil changes.
The aim of this study was to assess the possibility of using biological and biochemical parameters in the evaluation of forest soil quality and changes caused by land use. The study attempted to determine a relationship between the enzymatic activity of soil, the number of earthworms and soil physico-chemical properties. The study was carried out in central Poland in adjoining Forest Districts (Przedbórz and Smardzewice). In soil samples taken from 12 research plots, basic physico-chemical properties, enzyme activity (dehydrogenase, urease) and density and biomass of earthworms were examined. Enzyme activity showed a large diversity within the forest site types studied. The correlations between the activity of the enzymes studied and C/N ratio indicated considerable importance of these enzymes in metabolism of essential elements of organic matter of forest soils. Urease and dehydrogenase activity and earthworm number showed susceptibility to soil pH, which confirmed relationships between enzyme activity and abundance of earthworms and soil pH in H2O and KCl.
For sustainable soil use soil quality is essential presumption. Soil quality does not depend only on the physical and chemical properties of soil but it is very closely linked with the biological properties of soil mostly on microbiological processes. Soil quality is a dynamic feature, and any significant indicators must be sensitive to small changes in key soil properties. During the years 1991-2002 soil samples were collected at four Cambisol localities (totally 184 samples) and five Luvisol localities (totally 230 samples). Chemical (soil organic carbon [Corg], total nitrogen [Nt], pH KCl), textural (content of sand, silt, clay particles) and biological characteristics (microbial biomass carbon [Cmb], K2SO4 extractable microbial carbon [Cex]), respiration, ammonification, nitrification) were studied. The higher level of Corg (1.20-1.76%) characterised Cambisols and resulted in quite high microbial biomass carbon content (396—625 ug/g dry soil, average 556, SD 167). For these soils high control respiration (0.45-0.80 mg C02/h/100 g dry soil) and potential nitrification with (NH4)2S04 (6.7-18.4 mg N-NO3/8 days/100 g dry soil) were typical. Studied Luvisols reached lower levels: Corg (0.97-1.22%), Cmb (398-503 eg/g dry soil, average 455, SD 98), control respiration (0.46-0.57 mg C02/h/100 g dry soil), potential nitrification with (NH2)4SO4 (3.2-9.9 mg N-NO3/8 days/100 g dry soil). Mentioned lower level of organic carbon and medium level of microbial biomass raised in higher ratio Cmb/Corg (average 4.0%).
Gasification biochar represents one of the biochar types tested for agricultural needs. The aim of this study was to clarify the physico-chemical and biological changes occurring in a peat-sand substrate amended with hardwood-derived gasification biochar in the rates of 2, 4 and 20 g l-1. The pH(H2O) of the substrate with 4 g l-1 and 20 g l-1 biochar was increased from 5.6 to 6.2 and 6.7, respectively. The testing of the substrate in the re- spirometry device showed that the increase in the biochar rate led to a decrease in the amount of CO2 evolved at the maximum pressure drop. The continuous decrease in pressure observed in the respirometry bottles filled with pure biochar allows explaining this effect by biochar sorption activity. Addition of 2 and 4 g l-1 biochar to the peat-sand substrate stimulated the growth of cucumbers in an 18-day pot vegetation experiment. An increase in the number of root tips and root volume with a decreasing average root diameter was shown in the presence of biochar. Stimulation of plant growth on the background of low rates of biochar requires a further study with emphasis on the specific combination of biochar, soil type, plant species, and climatic conditions.
Adoption of sustainable tillage can protect soils from biological degradation and maintain soil quality, as compared with conventional management. This paper presents findings from a long-term tillage experiment carried out in Endocalcari-Endohypogleyic Cambisols on a sandy loam soil in Lithuania. The tillage systems were: conventional (CT), moderate (MT), and no tillage (NT). Tillage intensity positively affected microbial substrate utilization and urease activity, as well as, negatively, dehydrogenase activity, bacteria and fungi amounts, and Shannon diversity index of microbiological community. Higher total porosity provoked higher enzyme activity; but, microbial activity correlated negatively with bulk density.
Quantifying soil quality is important for asses- sing soil management practices effects on spatial and temporal variability of soil quality at the field scale. We studied the pos- sibility of defining a simple and practical fuzzy soil quality index based on biological, chemical and physical indicators for assessing quality variations of soil irrigated with well water and treated urban wastewater during two experimental years. In this study 6 proper- ties considered as minimum data set were selected out of 18 soil properties as total data set using the principal component analysis. Treated urban wastewater use had greater impact on biological and chemical quality. The results showed that the studied minimum data set could be a suitable representative of total data set. Significant correlation between the fuzzy soil quality index and crop yield (R 2 = 0.72) indicated the index had high biological significance for studied area. Fuzzy soil quality index approach (R 2 = 0.99) could be effectively utilized as a tool leading to better understanding soil quality changes. This is a first trial of creation of a universal index of soil quality undertaken.
This paper presents the introductory considerations for soil monitoring to be established in the forested zone of the Karkonosze National Park. The strategy and techniques of soil sampling are discussed with reference to the variability of soil properties. Based on the examples of 12 monitoring areas and the detailed analysis made for 5 of them, it was found that particularly high spatial differentiation (with SD> 50%) was typical for several soil parameters, i.e. the thickness of organic horizon, concentrations of available nutrients and total concentrations of heavy metals. On the contrary, the soil pH reaction did not vary significantly. Calculated total pools of nutrients and pollutants present in soil organic layers were comparable with those accumulated in mineral soil horizons to a depth of 20 cm. The data proved that such parameters as mean thickness of organic layer, surface coverage with rocks and the contribution of skeletal fractions in the mineral soil are of great importance for correct estimation of soil quality, in particular for the correct assessment of nutrient supply and the amount of pollutants accumulated in soils.
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