Changes in lead, zinc, copper, dry weight, and organic matter content of the forest floor of white pine stands in central Massachusetts over 16 years

1980 ◽  
Vol 14 (1) ◽  
pp. 54-56 ◽  
Author(s):  
Thomas G. Siccama ◽  
William H. Smith ◽  
Donald L. Mader
Keyword(s):  
Organic Matter ◽  
Forest Floor ◽  
Organic Matter Content ◽  
Dry Weight ◽  
Matter Content ◽  
White Pine ◽  
Lead Zinc ◽  
Pine Stands

scholarly journals Total phosphorus and organic matter content in bottom sediments of lake under restoration measures with iron treatment

2010 ◽  
Vol 10 (3-4) ◽  
pp. 139-145 ◽  
Author(s):  
Katarzyna Kowalczewska-Madura ◽  
Renata Dondajewska ◽  
Ryszard Gołdyn
Keyword(s):  
Organic Matter ◽  
Lake Sediments ◽  
Total Phosphorus ◽  
Bottom Sediments ◽  
Organic Matter Content ◽  
Dry Weight ◽  
Matter Content ◽  
Iron Treatment ◽  
Iron Sulphate ◽  
Restoration Measures

Total phosphorus and organic matter content in bottom sediments of lake under restoration measures with iron treatmentRusałka Lake is a shallow, man-made, strongly eutrophicated reservoir, being a place of recreational activities for Poznan citizens. Restoration measures with the use of iron sulphate were conducted in years 2006-2007. Phosphorus and organic matter concentrations in lake sediments were analyzed in years 2005-2007 at two research stations (profundal and littoral) to determine its changes under the influence of restoration. Greater phosphorus concentrations were noted in profundal (max 1.55 mg P g-1dry weight (DW)) than in littoral (max 0.98 mg P g-1DW). An increase of P amount in sediment was observed after iron treatment. Among phosphorus fractions Res-P dominated, i.e. phosphorus biologically unavailable for organisms. Organic matter content reached 23.1% in profundal, while 14.8% in littoral. Its amount decreased in following years.

Organic matter and mineral distribution in an old-growth Acersaccharum forest near the northern limit of its range

1990 ◽  
Vol 20 (9) ◽  
pp. 1332-1342 ◽  
Author(s):  
I. K. Morrison
Keyword(s):  
Organic Matter ◽  
Forest Floor ◽  
Mineral Soil ◽  
Organic Matter Content ◽  
Matter Content ◽  
Parent Material ◽  
Old Growth ◽  
Northern Ontario ◽  
Cu Content ◽  
Base Soil

Two sites, both supporting old-growth Acersaccharum Marsh, dominated forest on rugged topography in central northern Ontario, were compared in terms of organic matter and N, P, K, Ca, Mg, S, Fe, Mn, Zn, and Cu content in the tree- and field-layer phytomass, the forest floor, and the mineral soil. One site was on a shallow, low-base, Precambrian-derived till, and the other was on a till of somewhat higher base status. Gross and net growth of the overstory tree layer were also determined. Total phytomass values for the two stands at the beginning of the study period were 245 000 and 210 000 kg•ha−1, respectively. Gross growth was largely offset by mortality in both stands, producing a rough equilibrium with regard to net increment. Growth before mortality was on the order of 2.4–2.5 m3•ha−1•year−1 in terms of gross total wood volume or 3700–3900 kg•ha−1•year−1 in terms of phytomass, and it was slightly greater in percent terms on the higher base site. In addition to that in the phytomass, organic matter in the forest floor and mineral soil to a depth of 1 m also contributed to the total organic matter content of 638 000–642 000 kg•ha−1 (equivalent to 34 8000–353 000 kg•ha−1 of C) on both sites and was distributed as follows: 29–34% in phytomass, 5% in the forest floor, and 61–66% in mineral soil. The order of abundance of elements in the phytomass was similar on both sites: Ca > N > K > Mg > S > Mn > P > Fe > Zn > Cu, with accumulation in the phytomass in rough proportion to occurrence in the soil. A more base-rich parent material would appear to be the origin of 1452 kg•ha−1 of Ca estimated to be in the phytomass and forest floor on the higher base soil, compared with 1250 kg•ha−1 in the phytomass and forest floor on the lower base soil.

The ability of the nematode-trapping fungus Duddingtonia flagrans to reduce the transmission of

1999 ◽  
Vol 73 (2) ◽  
pp. 115-122 ◽  
Author(s):  
A.S. Fernández ◽  
M. Larsen ◽  
P. Nansen ◽  
E. Henningsen ◽  
J. Grønvold ◽  
...  
Keyword(s):  
Organic Matter ◽  
Fungal Spores ◽  
Organic Matter Content ◽  
Gastrointestinal Nematode ◽  
Sampling Period ◽  
Dry Weight ◽  
Matter Content ◽  
Duddingtonia Flagrans ◽  
Infective Larvae ◽  
Wet Weight

The ability of two isolates of the nematode-trapping fungus Duddingtonia flagrans to reduce the numbers of gastrointestinal nematode larvae on herbage was tested in three plot studies. Artificially prepared cow pats containing Ostertagia ostertagi eggs, with and without fungal spores, were deposited on pasture plots two or three times during the grazing season in 1995, 1996 and 1997. The herbage around each pat was sampled fortnightly over a period of 2 months and the number of infective larvae was recorded. At the end of the sampling period, the remainder of the faecal pats was collected to determine the wet weight, dry weight, and content of organic matter. The infective larvae remaining in the pats were extracted. Faecal cultures showed that both fungal isolates significantly reduced the number of infective larvae. Significantly fewer larvae were recovered from herbage surrounding fungus-treated pats compared with control pats in all three experiments, reflecting the ability of the fungus to destroy free-living larval stages in the faecal pat environment. After 8 weeks on pasture there were no differences between control and fungus-treated pats with respect to wet weight, dry weight, and organic matter content. This indicates that the degradation of faeces was not negatively affected by the presence of the fungus.

scholarly journals The muddy bottom sediments of the old river beds of the lower Vistula

2016 ◽  
Vol 16 (3) ◽  
pp. 141-146
Author(s):  
Daria Mimier ◽  
Janusz Żbikowski
Keyword(s):  
Organic Matter ◽  
Water Content ◽  
Bottom Sediments ◽  
Organic Matter Content ◽  
Oxygen Demand ◽  
Dry Weight ◽  
Matter Content ◽  
Sediment Oxygen Demand ◽  
Muddy Bottom ◽  
High Sediment

Abstract The main objective of this study was to characterize the muddy bottom sediments of three hydrologically different old river beds of the lower Vistula, located in the vicinity of Toruń: Port Drzewny, Martwa Wisła and Przybysz. Samples were taken at monthly intervals from April to November 2015 from two (Martwa Wisła and Przybysz) or three sampling sites (Port Drzewny) located in the central parts of the reservoirs. The bottom sediments of these water bodies were characterized by a low water content and organic matter content expressed as a percentage of dry weight, high organic matter content expressed in units of weight, as well as a high sediment oxygen demand. The most distinct reservoir was Martwa Wisła, most likely due to the lack of a connection with the River Vistula.

scholarly journals Soil Organic Matter Content Effects on Apple Root Dynamics

HortScience ◽  
2004 ◽  
Vol 39 (4) ◽  
pp. 842D-842
Author(s):  
Dario Stefanelli* ◽  
Giovambattista Sorrenti ◽  
Ronald L. Perry
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Root Length ◽  
Organic Matter Content ◽  
Mineral Fertilizer ◽  
Dry Weight ◽  
Matter Content ◽  
Root Dynamics ◽  
Shoot Ratio ◽  
Root Shoot Ratio

Soil organic matter is a critical component which is fundamental in plant growth. Several soil factors are influenced by organic matter such as slow release of nutrients, increased water holding capacity, improved soil physical characteristics and improved environment for soil microorganisms. The aim of this work is to investigate the physical effect of organic matter content in the soil on apple root growth and development. Twenty five two-year old apple trees (Malus domestica, Borkh) cv. `Buckeye Gala' on M.9 NAKB 337 rootstock were planted in completely transparent acrylic boxes. Plants have been grown in a green house to avoid external rain in a complete randomized design. Trees were planted in a sandy-mix soil amended with soil high in organic matter, “muck”, at four incremental levels. Treatments compared were a control (sandy soil with 0% organic matter) and 1%, 2%, 4% and 8% soil organic matter. The amount of water applied by automatic drip irrigation was comparable for all the treatments to avoid high fluctuation of soil moisture on root dynamics. All treatments have been fertilized with the same amount of mineral fertilizer to avoid the nutrition effect on root dynamics. Digital photos of roots were taken to study their dynamics every one to two weeks during a period of five months. Roots have been highlighted with Photoshop and then analyzed with WinRhizo to measure root length, area, lifespan and dynamics. At the end of the growing period plants have been harvested and fresh and dry weight was evaluated to asses the root/shoot ratio. The effects of the treatments on root length, area, lifespan and dynamics, and root/shoot ratio will be discussed.

On the biology of Calanus finmarchicus: XIII. Seasonal change in weight, calorific value and organic matter

1966 ◽  
Vol 46 (1) ◽  
pp. 1-17 ◽  
Author(s):  
G. W. Comita ◽  
S. M. Marshall ◽  
A. P. Orr
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Calorific Value ◽  
Dry Weight ◽  
Matter Content ◽  
Calanus Finmarchicus ◽  
Bomb Calorimetry ◽  
Males And Females ◽  
Autumn And Winter ◽  
Spring Maximum

The length, weight, calorific value and organic matter content of Calanus finmarchicus, Stage V, males and females, were measured in monthly samples taken from April 1962 to June 1963.There is considerable variation throughout the year and all stages had their maxima of weight and calorific value in spring, 1962, and winter 1962–63.The calorific value and weight are closely correlated so that, knowing the dry weight, the calorific value can be calculated from it. The correlation is closest in Stage V and, for these, only the dry weight need be known. Since the relation-ship is slightly different for males and females the sex of the adult must be known as well as the dry weight; curves showing these relationships are given.The calorific value obtained from organic-matter analysis at times deviates widely from the values obtained in direct bomb calorimetry, and it is concluded that in the method used not all the fat is accounted for.In weight, calorific value, and organic matter, but not in length, Stage V for a good part of the year show higher figures than adults.In comparing the weights with those of other years and other places, the annual pattern is found to vary considerably. The spring maximum seems to occur every year, but there may be either a maximum or a minimum in autumn and winter.

scholarly journals Chemical and Biochemical Properties of Oxisols after Sewage Sludge Application for 16 Years

2015 ◽  
Vol 39 (5) ◽  
pp. 1303-1310 ◽  
Author(s):  
Marcela Midori Yada ◽  
Wanderley José de Melo ◽  
Fábio Luiz Checchio Mingotte ◽  
Valéria Peruca de Melo ◽  
Gabriel Maurício Peruca de Melo
Keyword(s):  
Organic Matter ◽  
Sewage Sludge ◽  
Block Design ◽  
Organic Matter Content ◽  
Nutrient Deficiency ◽  
Dry Weight ◽  
Biochemical Properties ◽  
Matter Content ◽  
Weight Basis ◽  
Mineral Fertilization

ABSTRACT The large production of sewage sludge (SS), especially in large urban centers, has led to the suggestion of using this waste as fertilizer in agriculture. The economic viability of this action is great and contributes to improve the environment by cycling the nutrients present in this waste, including high contents of organic matter and plant nutrients. This study evaluated the chemical and biochemical properties of Dystrophic and EutroferricLatossolos Vermelhos (Oxisols) under corn and after SS application at different rates for 16 years. The field experiment was carried out in Jaboticabal, São Paulo State, Brazil, using a randomized block design with four treatments and five replications. Treatments consisted of control - T1 (mineral fertilization, without SS application), 5 Mg ha-1 SS - T2, 10 Mg ha-1 SS - T3, and 20 Mg ha-1 SS - T4 (dry weight base). The data were submitted to variance analysis and means were compared by the Duncan test at 5 %. Sewage sludge increased P extracted by resin in both theLatossolos Vermelhos, Dystrophic and Eutroferric, and the organic matter content in the Dystrophic Latossolo Vermelho. The waste at the rate 20 Mg ha-1 on a dry weight basis promoted increases in acid phosphatase activity in Eutroferric Latossolo Vermelho, basal respiration and metabolic quotient in DystrophicLatossolo Vermelho. The rate 20 Mg ha-1 sewage sludge on a dry weight basis did not alter the soil microbial biomass in both the Latossolos Vermelhos; in addition, it improved corn yields without inducing any symptoms of phytotoxicity or nutrient deficiency in the plants.

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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