1. Introduction
To fulfill the requirement of housing for all, high-rise building construction has become a necessity, especially in urban and metropolitan cities. It is essential to evaluate wind impact on such high-rise buildings for the safety of the structure and comfort of the users. In its most basic form, wind flow consists of a succession of gusts that vary greatly in amplitude and direction. Strong wind may cause discomfort to the users and damage to the structure. Extreme winds such as hurricanes, cyclones, and tornados can cause extensive damage to buildings due to the heavy load produced by such winds. The shape and size of the building play an important role in modifying wind-produced load on the building. As the height of the building increases (62 m and above) wind load is more pronounced than the seismic load [
1]. As such, it is important to study the wind environment on all types of high-rise buildings.
When the wind is motionless, normal air pressure acts everywhere around the building, balancing the load on the building in totality. Pressure changes from point to point on the building's surface as the wind picks up speed. Theoretically, according to Bernoulli's equation, at the stagnation point on the windward face, where velocity becomes zero, maximum pressure is developed. This pressure is equal to
, where
and
are air density and wind speed respectively. This is known as velocity/impact pressure [
2]. Using Bernoulli’s equation, pressure differences at a point can be represented as:
Where,
is a dimensionless entity called pressure coefficient and
is the pressure difference between actual pressure at the point,
and the normal atmospheric pressure
acting at that point. In the separated flow and wake regions where shear layers and vorticity do exist, Bernoulli’s equation does not hold good due to an increase in flow velocity [
3]. However, a good prediction of the pressure coefficient can be made by equation (1). In atmospheric boundary layer (ABL) flow where the exponential rise in velocity field along height occurs due to frictional resistance from the surface of the earth, pressure gradient, Coriolis effect, and earth’s rotation, defining the velocity field is not an easy task. ABL is the distance from the mean surface of the earth up to which the exponential gradient velocity field exists. It is up to 300 m to 400 m above the mean surface of the earth. So,
is set at a reference height. The greatest velocity at the rooftop of the model was used to calculate all
values in the current investigation. Points corresponding to the highest
, where impact pressure is greatest, can be found in this manner. A larger pressure drop caused by gustiness of wind at any point causes the average pressure distribution over the windward surface to be greater than the impact pressure. The resulting coefficient is mostly unaffected by wind speed and model scale [
2]. It is, however, influenced by the form of the building, wind flow direction, terrain roughness, and proximity to other structures [
4]. For structural design purposes, we can find
values for regular plan-shaped buildings in different international codes/standards, but the data are available only for orthogonal directions of wind flow. The value of pressure coefficients given in the codes for structural design are on the conservative side and provide uneconomical construction. For various unconventional architectural shapes, nowadays being used by architects, the values of
are either presumed from the codes, which are relatively inaccurate being approximated from the shapes given in codes, or from wind tunnel experiments, which are costly and time consuming. With the invention of complex computational facilities available nowadays, it is possible to know
values on buildings of different architectural shapes.
Baines [
5] was the first to demonstrate how wind velocity distribution and fluid pressure affect tall buildings. He demonstrated the isobars of the mean wind pressure on the windward face to be positive and suction pressures on the side faces, lee face, and rooftop of a tall square structure. Researchers have published a number of scientific papers on the subject of wind effects on various shapes of tall buildings. Gomes [
6] used CFD modeling to examine how the flow patterns on L and U shape models changed across a wide range of wind incidence angles. The surface pressure distributions were studied in a wind tunnel test. Wind flow in the recessed cavity of an H-shaped tall building using CFD was studied by [
7]. investigate the wind induced response and equivalent wind load on super tall buildings using experimental methods and measured pressure on building models [
8]. The flow between the cavity and outside of the cavity for different aspect ratio were studied. The flow within the cavity was found to be neither simply a cross-flow nor a stagnation flow. It is reported that the flow pattern was complex within the cavity and dependent upon the height and formation of two circulation vortices inside the cavity. [
9] studied L-shape and T-shape models of similar cross-sectional area and height but different limb lengths. They observed that the cross-sectional shapes and limb lengths are crucial for pressure distribution on faces. However, the magnitude of peak pressure and peak suction on the faces largely depends on wind direction. Mean interference of close proximity rectangular buildings placed in L and T plan shaped building were studied by [
10] in the wind tunnel for boundary layer wind flow over extended wind angles and a comparison was made with the response of similar buildings in isolation. Interference effects were reported to be influenced by the position and arrangements of models and wind incidence angles. Wind tunnel studies were used to illustrate the aerodynamic properties of several irregular plan shaped tall buildings [
11]. Presented a review of wind effects, instruments are not accurate enough to identify wind load parameter in the nonlinear region [
12], CFD study on ANSYS (CFX) was carried out at different wind angles on a rectangular model for interference effect due to another upstream rectangular model similar in plan area by [
13].[
14] Studied wind effects on tall buildings and observed that the positive wind effects will be on the wind ward side while negative pressure is on the leeward side. They varied aspect ratio of interfering and principal building models gradually from 1:5 to 5:5. Validity of the work was determined by comparing the pressure coefficients on the surfaces of the building in isolation with IS:875 (part-3)-1987. It was revealed that the wind load on the principal building largely depends upon the aspect ratios of the principal and interfering buildings and wind incident angles. Wind pressure variations on the octagonal plan shape building model in isolated and interfering conditions from three square building models placed at different locations at distances between 0.4 to 2 of the height of the octagonal building were studied by using ANSYS (CFX) [
15]. Investigated the wind pressure by varying the geometry or exposure condition, [
16] investigated the wind effects on super tall buildings using an experimental method, observing that the twisted wind flow will vary the vortex shedding mainly on the wind ward and side faces. [
17] A comparison of pressure on the faces and roofs of a square-tall building and a square tall building with a setback of 0.2L at 0.5H was studied by [
18] through ANSYS (CFX). The setback roof was found to be subjected to higher pressure than the top of the roof. [
19] used ANSYS (CFX) solver to examine the distribution of wind pressure on an E-plan-shape model. According to reports, values of the coefficient of pressure on faces for different element meshing sizes differ from wind tunnel measurements by 17 to 24%. Interference effects on an H-shape building model with similar building models placed at various positions were investigated by [
20]. At full blockage suction produced on the main building was found to be higher than other blockage conditions. Modification of wind flow around two plus shape tall building models in close proximity for interference effects was studied in an open circuit wind tunnel by [
21]. According to reports, the increase or decrease in wind load on the building façade was dependent on the relative positioning of the building models. In full blockage condition more suction was reported to occur on the gap faces and severe interference effect was reported at half and no blockage.
Not much study of wind effect on C-shape building models has been found in the available literature. Performed the test to investigate the structural behavior of super tall buildings under strong wind effects it was observed that the turbulent intensity and gust factor decreased as the mean wind speed increased [
22]. [
23] studied C-shape building models of similar plan areas but different heights. They predicted mean pressure coefficients on the faces through experimental as well as numerical analysis. It has been reported that geometry, aspect ratio, and wind flow pattern have a significant influence on pressure variations on faces. The goal of the current study was to determine how wind loads would affect a structure with a diamond C-plan shape building having a 300 sqm plan area and 50 m height (
Figure 1 a) by numerical simulation of building model done on ANSYS (CFX) software using standard k-ε turbulent model.
values obtained on the faces were evaluated for 0° to 180° @ 15° wind attack angles. However, a brief description of the wind flow pattern and typical (critical) values of the coefficient of wind pressure on the recessed faces for 0°, 30°, 60°, 105°, 135° & 180° wind attack angles are presented in this paper.
4. Mean Velocity Characteristics
In nature, as explained earlier in Para 1 that exponential velocity field along height within the ABL zone exists, it is difficult to define velocity load along building height. However, certain equations have been developed for the gradient velocity field in ABL. The power law equation, as described below, is widely used in wind engineering experiments for representing ABL flow.
Where, = Reference wind speed in m/s
= Reference height taken as 10 m.
= Time averaged longitudinal velocity at height Z above ground.
is the terrain roughness coefficient.
Though this equation is analytically not correct for the bottom 10 m of ABL it provides velocity of wind at higher altitudes well.