Influence of fine quartz sand faction on the properties of composite material

Author(s):  
Igor Romanenko ◽  
Alexey Fadin ◽  
Irina Petrovnina ◽  
Maria Romanenko
2010 ◽  
Vol 26 (1) ◽  
pp. 31-37 ◽  
Author(s):  
Frank Forcella ◽  
Trevor James ◽  
Anis Rahman

AbstractCorn gluten meal (CGM) is an approved organic fertilizer and pre-emergence herbicide that can be manufactured in the form of grit. This grit was tested for its ability to abrade seedlings of the summer annual weedy grass, Setaria pumila, when plants were in the 1- to 5-leaf stages of growth. CGM was propelled at air pressures of 250–750 kPa at distances of 30–60 cm from the plants. Established seedlings of S. pumila were controlled more effectively when grit was applied at 500 and 750 kPa than at 250 kPa, as well as when the applicator's nozzle was 30 cm from the plants compared to 60 cm distance. Seedling growth and dry weights were greatly reduced by exposures to grit at 60 cm and 500 kPa for 2 s or less, and seedlings were nearly completely destroyed at 30 cm distance and 750 kPa. CGM, a soft grit, was as effective for abrading seedlings as fine quartz sand, a hard grit. CGM had little pre-emergence herbicidal effect on S. pumila. Although regrowth can occur in S. pumila after abrasion by grit, the initial grit-induced stunting is sufficient to allow competing crop plants, like maize, to escape competition and suppress the weed. Consequently, CGM may be an effective form of soft grit for post-emergence abrasion of seedlings of summer annual grass weeds in organic row crops, while simultaneously supplying the crop with fertilizer.


Refractories ◽  
1982 ◽  
Vol 23 (9-10) ◽  
pp. 553-555
Author(s):  
V. M. Soifer ◽  
N. I. Mosolova ◽  
T. G. Bogomolova ◽  
V. S. Kozlova

2021 ◽  
Vol 9 ◽  
Author(s):  
Heng Li ◽  
Zhao Duan ◽  
Yanbin Wu ◽  
Chenxi Dong ◽  
Fasuo Zhao

The frequency of catastrophic geological disasters has been increasing significantly, causing tremendous losses of life and property. The study of landslide motion remains incomplete. The variables H/L (ratio of landslide height to length) are often used to describe landslide motion; however, they may also be affected by the height of the landslide itself. To better understand landslide dynamics, this paper aimed to 1) identify the process of landslide motion in relation to height; 2) understand the range of influence of sliding bodies according to height; and 3) construct a formula of landslide disaster range based on the travel distance of the slide center and changes in the center and shape of the sliding body. In this paper, medium-fine quartz sand was used in experiments to observe the movement patterns and sliding body barycenter variations occurring during landslides. We describe the changes that occur during landslides and their deposits’ morphological characteristics and barycenter variations with height. Based on these observations, a landslide model is derived. This paper proposes a new method of estimating the effects of landslides, which can help to mitigate the effects of disasters.


2016 ◽  
Vol 24 (2) ◽  
pp. 55
Author(s):  
Hananto Kurnio ◽  
Yudi Darlan

Biogenic gas within a deltaic deposition environment in the Kapuas rivermouth of West Kalimantan occurred in fine to very fine quartz sand reservoir of shallow boreholes of having the depth of 1-12 m below ground surface. This reservoir is covered by peaty layers of semi-impermeable property. During high tide, gas bubbling took place in the water column above the ground of these semi-impermeable layers. Utilizations of biogenic gas had been done succesfully. These works were carried out through drilling, piping, gas storage and installations for gas stove and gas electricity generator of 500 watt capacity at chief village house as an example before widely used to the local community. Keywords: Biogenic Gas; Deltaic Deposition Environment; Kapuas River; west Kalimantan, Utilization. Gas biogenik dalam suatu lingkungan pengendapan delta di muara Sungai Kapuas Kalimantan Barat terdapat dalam reservoar pasir kuarsa berukuran halus hingga sangat halus pada kedalaman bor dangkal 1-12 m di bawah permukaan tanah. Reservoar ini ditutupi oleh lapisan gambut semiimpermeabel. Selama pasang naik, gelembung gas teramati dalam kolom air di atas permukaan lapisan semi-impermeabel ini. Pemanfaatan gas biogenik telah dilaksanakan dengan sukses. Pemanfaatan ini dilakukan melalui pemboran, pipanisasi, penampungan gas dan instalasi untuk kompor gas dan generator listrik berbahan bakar gas kapasitas 500 watt di rumah Kepala Desa sebagai contoh sebelum dimanfaatkan secara luas oleh masyarakat setempat. Kata kunci: Gas Biogenik, Lingkungan Pengendapan Delta, Sungai Kapuas, Kalimantan Barat, Pemanfaatan


1979 ◽  
Vol 25 (9) ◽  
pp. 1021-1026 ◽  
Author(s):  
W. A. Ayers ◽  
P. B. Adams

Macroconidia of Sporidesmium sclerotivorum, a mycoparasite of Sclerotinia spp., germinated after 3 days in soil adjacent to sclerotia of S. minor and on membrane filters placed on soil containing sclerotia. Germination increased with time up to 18 days and with concentration of sclerotia. Conidia as distant as 9 mm from single sclerotia germinated. Germination of conidia was maximum on a sclerotial agar medium in the range of pH 5 to pH7. Cultivation of S. sclerotivorum parasitically on living sclerotia proceeded optimally in moist, fine quartz sand amended with 1 to 2% (w/w) sclerotia and 0.07% (w/w) CaCO3, at 25 °C. Infection of sclerotia in sand reached 100% by 5 weeks. Conidia production paralleled infection resulting in logarithmic increase in numbers; a maximum of 3 × 105 to 4 × 105 conidia/g was reached in 6 to 12 weeks. Viability of air-dried sand–sclerotial cultures of S. sclerotivorum was reduced after 1 and 6 days, but viability was undiminished in air-dried soil. Sporidesmium sclerotivorum survived in moist and air-dried soils stored at room temperature for 15 months.


Author(s):  
K. W. Wilson ◽  
P.M. Connor

INTRODUCTIONDuring the production of china clay, a waste of fine quartz, sand kaolin and mica flakes in suspension is produced. Until recently, only a small proportion of this fine material was retained and settled in lagoons and consequently most of the effluent was discharged. Waste produced in the St Austell area was carried by the Par and White Rivers into Mevagissey Bay (see Fig. 1). In 1968 the china clay industry considered a proposal to combine all its wastes arising in the area and to discharge them into the sea via the White River or if necessary further out to sea by a pipeline. The precise location of the pipeline was not denned at that time but, irrespective of position, deterioration of conditions in St Austell and Mevagissey Bays seemed inevitable.


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