House Heating by Hot Water Circulation

1888 ◽  
Vol 6 (2build) ◽  
pp. 44-44
Keyword(s):  
2020 ◽  
Vol 172 ◽  
pp. 12009
Author(s):  
Stephen Burke ◽  
Jonatan von Seth ◽  
Tomas Ekström ◽  
Christoffer Maljanovski ◽  
Magnus Wiktorsson

The hot water circulation system in a building is a system which helps prevent Legionella problems whilst ensuring that tenants have access to hot water quickly. Poorly designed or implemented systems not only increase the risk to people’s health and thermal comfort, but even result in an increase in the energy needed for this system to function properly. Results from previous studies showed that the total hot water circulation system loss can be as high as 25 kWh/m2 heated floor area per year. The purpose of this project is to measure the total energy use per year of the hot water circulation system in about 200 multifamily dwellings of different ages to verify that a system loss of 4 kWh/m2, year is a realistic assumption for both newer and older/retrofitted buildings. The preliminary results from the first 134 measurements showed that the assumption of 4 kWh/m2, year is rarely fulfilled. An average energy use of more than three times this is more common, even in newer buildings. Whilst some of the total energy lost is used to heat the buildings, it is not desirable because it is an uncontrolled energy flow.


1987 ◽  
Vol 124 (3) ◽  
pp. 261-271 ◽  
Author(s):  
Julian E. Andrews

AbstractClay minerals from Middle Jurassic lagoonal mudrocks, siltstones and silty fine-grained sandstones of the upper Great Estuarine Group (Bathonian) are divided into four assemblages. Assemblage 1, the most common assemblage, is rich in mixed-layer illite–smectite with attendant illite and kaolinite. Assemblage 2 is dominated by smectitic clay. These assemblages are indicative of primary Jurassic deposition. Illite and kaolinite were probably derived from the weathering of older rocks and soils in the basin hinterland and were deposited in the lagoons as river-borne detritus. The majority of smectite and mixed-layer illite–smectite is interpreted as the argillization product of Jurassic volcanic dust, also deposited in the lagoons by rivers. Near major Tertiary igneous intrusions these depositional clay mineral assemblages have been altered. Assemblage 3 contains smectite-poor mixed-layer illite–smectite, whilst Assemblage 4 contains no smectitic clay at all. Destruction of smectite interlayers occurred at relatively shallow burial depths (< 2500 m) due to enhanced geothermal gradients and local convective hot-water circulation cells associated with the major Tertiary igneous intrusions.


2015 ◽  
Author(s):  
Kirk Duval ◽  
Dubert Gutiérrez ◽  
Dino Petrakos ◽  
Pierre Ollier ◽  
Darren Johannson

1989 ◽  
Vol 55 (515) ◽  
pp. 2018-2023
Author(s):  
Tadayoshi TANAKA ◽  
Yukio YAMADA ◽  
Hiroshi ISHIGURO ◽  
Masaaki TAKEUCHI ◽  
Mamoru YAMASHITA ◽  
...  

2014 ◽  
Vol 899 ◽  
pp. 131-134
Author(s):  
Katarina Knizova ◽  
Martin Kovac

The content of this submission is to define the operation time of a hot water circulation loop in term of the hot water temperature drop in a time depending on several factors. Type and diameter of a pipe, thickness of a thermal pipe insulation, location of distribution pipes and ambient temperature around the pipes belong among these significant factors. All these parameters and others are used in the analytic calculation of the hot water temperature drop in a time according to the standard STN EN 15316-3-2. So we can use the calculated time of hot water temperature drop in order to define time intervals of the water circulation in hot water distribution pipes. The aim of this submission is to determine heat losses from hot water distribution pipes and calculate the electric energy consumption of the circulation pump for this design state. The study results are demonstrated on the model object of a multi-dwelling house.


Sign in / Sign up

Export Citation Format

Share Document