Effects of soil burn severity on germination and initial establishment of maritime pine seedlings, under greenhouse conditions, in two contrasting experimentally burned soils

2011 ◽  
Vol 20 (2) ◽  
pp. 209 ◽  
Author(s):  
M. T. Fontúrbel ◽  
J. A. Vega ◽  
P. Pérez-Gorostiaga ◽  
C. Fernández ◽  
M. Alonso ◽  
...  
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Matter Content ◽  
Maritime Pine ◽  
Burn Severity ◽  
First Year ◽  
Soil C ◽  
Burned Areas ◽  
Pine Seedlings ◽  
Soil Burn Severity

The effects of soil burn severity on initial establishment of maritime pine in burned areas are not well known. Many factors may interact in the field, thus making it difficult to determine the exact role played by soil burn severity in the post-fire regeneration process. Monoliths of two contrasting soils – an acid, coarse-textured soil, with high organic matter content, and a neutral heavy-textured soil with low organic matter content – were experimentally burned to provide two markedly different levels of soil burn severity. The burned monoliths were sown with Pinus pinaster seeds and then placed in a greenhouse under a preselected water regime to determine the effect of burn severity on emergence and initial establishment of pine seedlings. High soil burn severity in the coarse-textured soils delayed germination, increased mortality and temporarily decreased the height of pine seedlings in the first year after sowing. This response was affected by: soil heating level, soil C consumption, post-fire soil C, depth of burn and post-fire duff-depth. Ash had no influence on the above processes. These factors did not explain the variability in the response of regeneration variables in the heavy-textured soils. The applicability of the results to field conditions is discussed.

Organic phosphorus speciation in Australian Red Chromosols: stoichiometric control

Soil Research ◽  
2016 ◽  
Vol 54 (1) ◽  
pp. 11 ◽  
Author(s):  
Melinda R. S. Moata ◽  
Ashlea L. Doolette ◽  
Ronald J. Smernik ◽  
Ann M. McNeill ◽  
Lynne M. Macdonald
Keyword(s):  
Organic Matter ◽  
Soil Type ◽  
Organic Phosphorus ◽  
Organic Matter Content ◽  
Matter Content ◽  
31P Nmr Spectroscopy ◽  
Chemical Forms ◽  
Organic P ◽  
Soil C ◽  
Soil P

Organic phosphorus (P) plays an important role in the soil P cycle. It is present in various chemical forms, the relative amounts of which vary among soils, due to factors including climate, land use, and soil type. Few studies have investigated co-variation between P types or stoichiometric correlation with the key elemental components of organic matter– carbon (C) and nitrogen (N), both of which may influence P pool structure and dynamics in agricultural soils. In this study we determined the organic P speciation of twenty Australian Red Chromosols soils, a soil type widely used for cropping in Australia. Eight different chemical forms of P were quantified by 31P NMR spectroscopy, with a large majority (>90%) in all soils identified as orthophosphate and humic P. The strongest correlations (r2 = 0.77–0.85, P < 0.001) between P types were found among minor components: (i) between two inositol hexakisphosphate isomers (myo and scyllo) and (ii) between phospholipids and RNA (both detected as their alkaline hydrolysis products). Total soil C and N were correlated with phospholipid and RNA P, but not the most abundant P forms of orthophosphate and humic P. This suggests an influence of organic matter content on the organic P pool consisting of phospholipid and RNA, but not on inositol P or the largest organic P pool in these soils – humic P.

scholarly journals Uptake of thallium from artificially contaminated soils by kale (Brassica oleracea L., var. acephala)

2011 ◽  
Vol 52 (No. 12) ◽  
pp. 544-549 ◽  
Author(s):  
J. Pavlíčková ◽  
J. Zbíral ◽  
M. Smatanová ◽  
P. Habarta ◽  
P. Houserová ◽  
...  
Keyword(s):  
Organic Matter ◽  
Brassica Oleracea ◽  
Contaminated Soils ◽  
Acid Soil ◽  
Organic Matter Content ◽  
Matter Content ◽  
First Year ◽  
The Third ◽  
Very High ◽  
Brassica Oleracea L

A pot experiment focused on the study of factors influencing thallium transfer from contaminated soils into kale (green cabbage, Brassica oleracea L. var. acephala, variety Winterbor F1) was evaluated. Three different types of topsoils with naturally low content of thallium (heavy, medium and medium-light soil) were used for pot experiments. The soils were contaminated with thallium sulfate to achieve five levels of contamination (0, 0.52, 2.10, 4.20 and 5.88 mg/kg). There were six replicates for each combination (90 pots in the experiment). The first part of the experiment started in the year of contamination (2001) and continued in 2003. The soil samples and the samples of kale (leaves and stalks were sampled separately) were collected and analysed. Kale was found to be able to accumulate Tl without any influence on yield. The highest thallium concentration was found in the leaves of kale in the first year of the experiment and reached 326 mg/kg dry matter. Bioaccumulation factor (Biological Absorption Coefficient &ndash; BAC) was found to be over 80 during the first year of the experiment. In the third year the BAC was around 3 for the soil with the highest pH and the highest organic matter content but as high as 15 for an acid soil with the lowest content of organic matter and the lowest Cation Exchange Capacity (CEC) of soils. The content of thallium in the leaves of kale was found to be 7 to 10 times higher than in the stalks in the third year. In the first year this ratio was up to 18. From these findings it can be concluded that the ability of some plants of Brassicacea family, that are planted as common vegetables, to accumulate thallium is very high and can be a serious danger for food chains. Neutral soils high in CEC and organic matter are able to bind thallium more effectively than poor acid soils and the transfer of Tl into plants from these soils is substantially lower. The uptake of Tl from contaminated soils into kale can be very high and without any negative effect on the plant growth. The transfer of Tl into kale decreases with the time necessary to reach the equilibrium between the added Tl and the soil (ageing of a sample).

scholarly journals High stability and metabolic capacity of bacterial community promote the rapid reduction of easily decomposing carbon in soil

2021 ◽  
Vol 4 (1) ◽  
Author(s):  
Ruilin Huang ◽  
Thomas W. Crowther ◽  
Yueyu Sui ◽  
Bo Sun ◽  
Yuting Liang
Keyword(s):  
Climate Change ◽  
Organic Matter ◽  
Organic Matter Content ◽  
Matter Content ◽  
Climate Feedback ◽  
Metabolic Capacity ◽  
Rapid Reduction ◽  
Soil C ◽  
Temperature And Precipitation ◽  
The Stability

AbstractIrreversible climate change alters the decomposition and sequestration of soil carbon (C). However, the stability of C components in soils with different initial organic matter contents and its relationship with the response of major decomposers to climate warming are still unclear. In this study, we translocated Mollisols with a gradient of organic matter (OM) contents (2%–9%) from in situ cold region to five warmer climatic regions to simulate climate change. Soil C in C-rich soils (OM >5%) was more vulnerable to translocation warming than that in C-poor soils (OM ≤ 5%), with a major loss of functional groups like O-alkyl, O-aryl C and carboxyl C. Variations of microbial β diversity with latitude, temperature and precipitation indicated that C-rich soils contained more resistant bacterial communities and more sensitive fungal communities than C-poor soils, which led to strong C metabolism and high utilization ability of the community in C-rich soils in response to translocation warming. Our results suggest that the higher sensitivity of soils with high organic matter content to climate change is related to the stability and metabolic capacity of major bacterial decomposers, which is important for predicting soil-climate feedback.

Predicting pH buffering capacity of New Zealand soils from organic matter content and mineral characteristics

Soil Research ◽  
2013 ◽  
Vol 51 (6) ◽  
pp. 494 ◽  
Author(s):  
Denis Curtin ◽  
Stephen Trolove
Keyword(s):  
Organic Matter ◽  
New Zealand ◽  
Buffer Capacity ◽  
Organic Matter Content ◽  
Clay Content ◽  
Matter Content ◽  
Soil C ◽  
Ph Buffering ◽  
Mineral Characteristics ◽  
Permanent Pasture

Information on the pH buffer capacity of soil is required to estimate changes in pH due to acidic or alkaline inputs, and to model pH-dependent processes within the soil nitrogen (N) cycle. The objective was to determine whether a model based on soil organic matter (SOM) and mineral characteristics (clay content, extractable iron (Fe) and aluminium (Al)) would be adequate to estimate the buffer capacities of New Zealand soils. We measured pH changes in 34 soils, representing a range of SOM and texture, after equilibration with several rates (range 0–15 cmol OH– kg–1 soil) of either KOH or Ca(OH)2. The Ca(OH)2 method often yielded higher buffer capacity values than the KOH method, possibly because of incomplete reaction of Ca(OH)2, especially at high addition rates. Buffer capacity (measured using KOH) of the soils was strongly correlated with soil carbon (C) (R2 = 0.76), and weakly (but significantly, P < 0.05) with clay content, and with dithionite extractable Fe and Al. A regression with soil C, clay, and P-retention (a surrogate for extractable Al and Fe) as independent variables explained 90% of the variability in pH buffering. The role of organic matter was further evaluated by measuring buffer capacity of soil from research plots at Lincoln, Canterbury, New Zealand, that differed in C (21–37 g C kg–1 in the top 7.5 cm; 19–26 g C kg–1 in the 7.5–15 cm) as a result of the treatments imposed during the 12-year trial period. A substantial decrease in pH buffering (by up to 24% in top 7.5 cm) was associated with a decline in SOM following the conversion of permanent pasture (pre-trial land use) to arable cropping. Across all treatments and sampling depths, buffer capacity was linearly related (R2 = 0.84, P < 0.001) to soil C; the estimated buffer capacity of SOM was 89 cmolc kg–1 C pH unit–1, similar to the value calculated from the previous study with different soil types. After 12 years, treatments with low soil C concentrations tended to be more acidic, possibly partly because of weaker pH buffering.

scholarly journals Decomposability of soil organic matter over time: The Soil Incubation Database (SIDb, version 1.0) and guidance for incubation procedures

2019 ◽  
Author(s):  
Christina Schädel ◽  
Jeffrey Beem-Miller ◽  
Mina Aziz Rad ◽  
Susan E. Crow ◽  
Caitlin Hicks Pries ◽  
...  
Keyword(s):  
Time Series ◽  
Organic Matter ◽  
Time Series Data ◽  
Model Development ◽  
Organic Matter Content ◽  
Matter Content ◽  
Series Data ◽  
Soil Incubation ◽  
Microbial Decomposition ◽  
Soil C

Abstract. The magnitude of carbon (C) loss to the atmosphere via microbial decomposition is a function of the amount of C stored in soils, the quality of the organic matter, and physical, chemical and biological factors that comprise the environment for decomposition. The decomposability of C is commonly assessed by laboratory soil incubation studies that measure greenhouse gases mineralized from soils under controlled conditions. Here, we introduce the Soil Incubation Database (SIDb) version 1.0, a compilation of time series data from incubations, structured into a new, publicly available database of C flux (carbon dioxide, CO2, or methane, CH4). In addition to open access, the SIDb project also provides a platform for the development of tools for reading and analysis of incubation data as well as documentation for future use and development. In addition to introducing SIDb, we provide reporting guidance for database entry and the required variables that incubation studies need at minimum to be included in SIDb. A key application of this synthesis effort is to better characterize soil C processes in Earth system models, which will in turn reduce our uncertainty in predicting the response of soil C decomposition to a changing climate. We demonstrate a framework to fit curves to a number of incubation studies from diverse ecosystems, depths, and organic matter content using a built-in model development module that integrates SIDb with the existing SoilR package to estimate soil C pools from time series data. The database will help bridge the gap between site-level measurements, which are commonly used in incubation studies, and global remote-sensed data or data products derived from models aimed at assessing global-scale rates of decomposition and C turnover. The SIDb, version 1.0, is archived and publicly available at DOI: https://doi.org/10.5281/zenodo.3470459 (Sierra et al., 2019) and the database is managed under a version-controlled system and centrally stored in GitHub (https://github.com/SoilBGC-Datashare/sidb).

scholarly journals Decomposability of soil organic matter over time: the Soil Incubation Database (SIDb, version 1.0) and guidance for incubation procedures

2020 ◽  
Vol 12 (3) ◽  
pp. 1511-1524 ◽  
Author(s):  
Christina Schädel ◽  
Jeffrey Beem-Miller ◽  
Mina Aziz Rad ◽  
Susan E. Crow ◽  
Caitlin E. Hicks Pries ◽  
...  
Keyword(s):  
Time Series ◽  
Organic Matter ◽  
Time Series Data ◽  
Model Development ◽  
Organic Matter Content ◽  
Matter Content ◽  
Series Data ◽  
Soil Incubation ◽  
Microbial Decomposition ◽  
Soil C

Abstract. The magnitude of carbon (C) loss to the atmosphere via microbial decomposition is a function of the amount of C stored in soils, the quality of the organic matter, and physical, chemical, and biological factors that comprise the environment for decomposition. The decomposability of C is commonly assessed by laboratory soil incubation studies that measure greenhouse gases mineralized from soils under controlled conditions. Here, we introduce the Soil Incubation Database (SIDb) version 1.0, a compilation of time series data from incubations, structured into a new, publicly available, open-access database of C flux (carbon dioxide, CO2, or methane, CH4). In addition, the SIDb project also provides a platform for the development of tools for reading and analysis of incubation data as well as documentation for future use and development. In addition to introducing SIDb, we provide reporting guidance for database entry and the required variables that incubation studies need at minimum to be included in SIDb. A key application of this synthesis effort is to better characterize soil C processes in Earth system models, which will in turn reduce our uncertainty in predicting the response of soil C decomposition to a changing climate. We demonstrate a framework to fit curves to a number of incubation studies from diverse ecosystems, depths, and organic matter content using a built-in model development module that integrates SIDb with the existing SoilR package to estimate soil C pools from time series data. The database will help bridge the gap between point location measurements, which are commonly used in incubation studies, and global remote-sensed data or data products derived from models aimed at assessing global-scale rates of decomposition and C turnover. The SIDb version 1.0 is archived and publicly available at https://doi.org/10.5281/zenodo.3871263 (Sierra et al., 2020), and the database is managed under a version-controlled system and centrally stored in GitHub (https://github.com/SoilBGC-Datashare/sidb, last access: 26 June 2020).

scholarly journals IMPACT OF ORGANIC FERTILIZER "DOSTATOK" ON THE SURVIVAL AND GROWTH OF PINE PLANTATIONS

2018 ◽  
Vol 28 (3) ◽  
pp. 62-66
Author(s):  
V. Yu. Yuhnovskyi ◽  
Yu. S. Urliuk ◽  
M. P. Holovetskyi ◽  
I. L. Sereda
Keyword(s):  
Organic Matter ◽  
Sandy Loam ◽  
Organic Fertilizer ◽  
Organic Matter Content ◽  
Matter Content ◽  
Pine Plantations ◽  
Organic Layer ◽  
Scotch Pine ◽  
Pine Seedlings ◽  
Survival And Growth

The survival and growth of pine plantations, created at the clear cuttings, with the use of organic fertilizer "Dostatok" are analyzed. The research was conducted in 11 forest units of the State Enterprise "Vyshche-Dubechna Forestry" in the fresh poor and rich forest sites. The plantations were created according to the following schemes: 4 rows of Scotch pine and 1 row of red oak with placement of seedlings 1.5×0.5 m and 1.5×1.0 m by planting them in a furrow formed by a plow PKL-70. The total forest pine plantations with application of fertilizer amounted to 22.2 hectares. The agrochemical analysis revealed that 40.6 % of organic matter was concentrated in the fertilizer, whereas in the organic layer of fresh poor and rich pine sites, the content of humus was 22.2 % and 30.7 % respectively. At the same time, fertilizer is characterized by a neutral environment, while the organic soil of fresh poor and rich pine sites has a very high acidity of the pH of the salt extract, which fluctuates within 3.5–3.6. The double predominance of the organic matter content in the fertilizer promotes the survival and growth of pine plantations. It was established that the introduction of fertilizer "Dostavok" in the form of tablets on the root system of pine seedlings increases the survival of forest plantations, which on sandy and sandy loam soils, respectively, reaches 90 and 95 %. Values of pH salt extraction indicate that the soils are very acid (3.5 and 3.1), with an average level of humus (2.4 and 7.4 %), low levels of ammonia and nitrate nitrogen and mobile phosphorus. Soil of fresh poor pine site has an elevated level of mobile potassium (139.87 mg·kg-1), while the fresh rich pine site is characterized by a low level of potassium, which is 46.39 mg·kg-1. Granulometric analysis of the soil showed that the poor sites are represented by sandy soils and rich sites – rough-dust sandy loam soils. Almost double the predominance of the organic matter content in the fertilizer "Dostatok" contributes to the survival and growth of pine plantations. The annual increment of pine seedlings on 4–7 cm was more than at the control. The use of bio-fertilizer also reduces the number of manual care and accelerates the closure in the rows, which in turn allows the transfer of forest crops to covered forest area a year earlier.

HEAVY METAL SPECIATION IN BOTTOM SEDIMENTS OF THE VYSHNEVOLOTSKY RESERVOIR

2018 ◽  
pp. 46-54
Author(s):  
O. A. Lipatnikova
Keyword(s):  
Heavy Metal ◽  
Organic Matter ◽  
Bottom Sediments ◽  
Metal Speciation ◽  
Organic Matter Content ◽  
Water Reservoir ◽  
Matter Content ◽  
Heavy Metal Speciation ◽  
Mobile Forms ◽  
Manganese Hydroxides

The study of heavy metal speciation in bottom sediments of the Vyshnevolotsky water reservoir is presented in this paper. Sequential selective procedure was used to determine the heavy metal speciation in bottom sediments and thermodynamic calculation — to determine ones in interstitial water. It has been shown that Mn are mainly presented in exchangeable and carbonate forms; for Fe, Zn, Pb и Co the forms are related to iron and manganese hydroxides is played an important role; and Cu and Ni are mainly associated with organic matter. In interstitial waters the main forms of heavy metal speciation are free ions for Zn, Ni, Co and Cd, carbonate complexes for Pb, fulvate complexes for Cu. Effects of particle size and organic matter content in sediments on distribution of mobile and potentially mobile forms of toxic elements have been revealed.

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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