Composition of the Water-Soluble Soil Fraction on the Barents Sea Coast: Organic Carbon and Nitrogen, Low-Molecular Weight Components

2019 ◽  
Vol 52 (11) ◽  
pp. 1347-1362 ◽  
Author(s):  
E. V. Shamrikova ◽  
O. S. Kubik ◽  
S. V. Deneva ◽  
V. V. Punegov
Keyword(s):  
Molecular Weight ◽  
Organic Carbon ◽  
Barents Sea ◽  
Water Soluble ◽  
Low Molecular Weight ◽  
Carbon And Nitrogen ◽  
Soil Fraction ◽  
The Barents Sea ◽  
Sea Coast

ANALISA KANDUNGAN BETA-GLUKAN LARUT AIR DAN LARUT ALKALI DARI TUBUH BUAH JAMUR TIRAM (Pleurotus ostreatus) DAN SHIITAKE (Lentinus edodes)

2013 ◽  
Vol 13 (3) ◽  
Author(s):  
Netty Widyastuti ◽  
Teguh Baruji ◽  
Henky Isnawan ◽  
Priyo Wahyudi ◽  
Donowati Donowati
Keyword(s):  
Molecular Structure ◽  
Molecular Weight ◽  
Immune System ◽  
Pleurotus Ostreatus ◽  
Water Soluble ◽  
Low Molecular Weight ◽  
Lentinus Edodes ◽  
Beta Glucan ◽  
Oyster Mushrooms ◽  
The Difference

Beta glucan is a polysaccharide compound, generally not soluble inwater and resistant to acid. Beta glucan is used as an immunomodulator (enhancing the immune system) in mammals is usually a beta-glucan soluble in water, easily absorbed and has a low molecular weight. Several example of beta-glucan such as cellulose (β-1 ,4-glucan), lentinan (β-1 0.6-glucan) and (β-1 ,3-glucan), pleuran (β-1, 6 and β-1 ,3-glucan) are isolated from species of fungi Basidiomycota include mushrooms (Pleurotus ostreatus) and shiitake (Lentinus edodes).The purpose of thisresearch activity is to obtain beta-glucan compound that can be dissolved in water and in alkali derived from fungi Basidiomycota, i.e, Oyster mushrooms (Pleurotus ostreatus) and shiitake (Lentinus edodes). The result of beta-glucan compared to characterize the resulting beta glucan that is molecular structure . The difference of beta glucan extraction is based on the differences in solubility of beta-glucan. Beta glucan could be water soluble and insoluble water.

scholarly journals Water-soluble low-molecular-weight cellulose chains radially oriented on gold nanoparticles

Cellulose ◽  
2011 ◽  
Vol 18 (4) ◽  
pp. 929-936 ◽  
Author(s):  
Yukiko Enomoto-Rogers ◽  
Hiroshi Kamitakahara ◽  
Arata Yoshinaga ◽  
Toshiyuki Takano
Keyword(s):  
Molecular Weight ◽  
Gold Nanoparticles ◽  
Water Soluble ◽  
Low Molecular Weight

Water-soluble low-molecular-weight organic acids in automorphic loamy soils of the tundra and taiga zones

2013 ◽  
Vol 46 (6) ◽  
pp. 654-659 ◽  
Author(s):  
E. V. Shamrikova ◽  
I. V. Gruzdev ◽  
V. V. Punegov ◽  
F. M. Khabibullina ◽  
O. S. Kubik
Keyword(s):  
Molecular Weight ◽  
Organic Acids ◽  
Water Soluble ◽  
Low Molecular Weight

Structural influences of low-molecular-weight dissolved organic carbon mimics on the photolytic fate of atrazine

1998 ◽  
Vol 17 (6) ◽  
pp. 975-981 ◽  
Author(s):  
Cathleen J. Hapeman ◽  
Susanna Bilboulian ◽  
Brent G. Anderson ◽  
Alba Torrents
Keyword(s):  
Molecular Weight ◽  
Organic Carbon ◽  
Dissolved Organic Carbon ◽  
Low Molecular Weight

scholarly journals Soil organic carbon and nitrogen characteristics in differently used grasslands at sites with drainage and without drainage

2011 ◽  
Vol 51 (No. 4) ◽  
pp. 165-172 ◽  
Author(s):  
R. Dufková ◽  
T. Kvítek ◽  
J. Voldřichová
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Soil Microorganisms ◽  
Chemical Properties ◽  
Fulvic Acids ◽  
Drainage Water ◽  
Water Soluble ◽  
Hot Water ◽  
Carbon And Nitrogen ◽  
Thermal Combustion

Extensive management (absence of management) of unfertilized permanent grasslands was examined for five years from the aspect of its influence on soil chemical properties of horizon A in a floodplain locality of the Crystalline Complex, in relation to water regime regulation, reclamations and liming. These treatments: without mowing (0), one cut (1) and two cuts (2) per year were used at sites without drainage (WD), with drainage (D) and with drainage water retardation (R). These average values were measured at all sites and for all treatments: content of soil organic carbon C<sub>org</sub> 2.3&ndash;3.4%, combustible substances CS 12&ndash;15%, humic to fulvic acids ratio C<sub>HA</sub>/C<sub>FA</sub> 0.81&ndash;0.94, C/N 8&ndash;9, humification rate 0.6&ndash;0.7, exchange pH 3.9&ndash;5.1. All sites have deteriorated conditions for the activity of soil microorganisms (low pH). Determinations of the contents of organic carbon (C<sub>org</sub> by thermal combustion, water soluble and hot water soluble carbon, C<sub>HA</sub> and C<sub>FA</sub>), CS and total nitrogen indicated decreases as a result of the influence of factors (drainage, liming, mowing) supporting mineralization and the cycle of soil organic matter. Mowing improved humus quality

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