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Journal of the Royal Society Interface logoLink to Journal of the Royal Society Interface
. 2019 Jul 10;16(156):20190048. doi: 10.1098/rsif.2019.0048

Nectar, humidity, honey bees (Apis mellifera) and varroa in summer: a theoretical thermofluid analysis of the fate of water vapour from honey ripening and its implications on the control of Varroa destructor

Derek Mitchell 1,
PMCID: PMC6685017  PMID: 31288647

Abstract

This theoretical thermofluid analysis investigates the relationships between honey production rate, nectar concentration and the parameters of entrance size, nest thermal conductance, brood nest humidity and the temperatures needed for nectar to honey conversion. It quantifies and shows that nest humidity is positively related to the amount, and water content of the nectar being desiccated into honey and negatively with respect to nest thermal conductance and entrance size. It is highly likely that honeybees, in temperate climates and in their natural home, with much smaller thermal conductance and entrance, can achieve higher humidities more easily and more frequently than in man-made hives. As a consequence, it is possible that Varroa destructor, a parasite implicated in the spread of pathogenic viruses and colony collapse, which loses fecundity at absolute humidities of 4.3 kPa (approx. 30 gm−3) and above, is impacted by the more frequent occurrence of higher humidities in these low conductance, small entrance nests. This study provides the theoretical basis for new avenues of research into the control of varroa, via the modification of beekeeping practices to help maintain higher hive humidities.

Keywords: evaporation, nectar, efficiency, humidity, climate, thermofluid

1. Introduction

The phenotype, the physical reflection of the gene, cannot be limited to purely the biological aspects of the organism itself because it directly causes change to the environment around it [1], in accordance with the laws of thermodynamics and mass and energy conservation. For most organisms, the realm of their influence extends only a very small distance from the biological tissue of the animal. However for those in which this goes beyond the usual, and their reach into the environment is significant, then it is termed an ‘extended phenotype’. The classic case cited is of beavers flooding areas with their dams [2]. For honeybee colonies, perhaps because of the relationship with man, the extended nature of this super organism's [3] phenotype has been overlooked and viewed as a simple shelter and container of honey and brood. In contrast to the beaver's dam, which constrains a single visible fluid, some of the fluids involved in a honeybee colony's nest: air, water vapour, water liquid and carbon dioxide are invisible to human eyes. These fluids are not passively restrained, but actively moved and changed in temperature and physical state within this extended phenotype. In addition, heat flux through the nest walls and entrance [4]; condensation and evaporation of water; and desiccation of nectar into honey, literally sugar refining, some of which is metabolized/‘burnt’ [5]. Thermofluids is defined as the study of fluid flows, heat transfer including phase changes and the combustion of fluids [6]. Therefore, a comprehensive analytical study of a honeybee's extended phenotype must include analysis based on thermofluids and apply its relevant tools. That these are more commonly used to analyse sugar refineries, buildings or nuclear power plants should not be seen as a barrier [1].

Research into honeybees is almost exclusively executed in man-made hives, and with only two exceptions [4,7], without any measurement of the hives physical characteristics. Unsurprisingly, there is very little quantitative research or analysis [4,8] into their thermofluid properties. It is from this low level that this analysis endeavours to understand the interplay of some of the thermofluid processes.

It is important to note that in this document, the unqualified term, humidity, will be only used to refer to the absolute humidity expressed as the vapour pressure in kilopascals or as a tuple of the saturation ratio χ, and the absolute temperature T denoted as {χ, T}. Thus, the humidity of 80% saturation at 34°C is shown as 4.3 kPa and/or {0.8, 307.2 K} from equation (3.1). The saturation ratio (relative humidity (RH)), will be clearly denoted if used. The dew point temperature is the temperature TD, for that humidity, where the air is at complete saturation i.e. {1.0, TD}. Thus, because {0.8, 307.2 K} equals 4.3 kPa which equals {1.0, 303.2 K}, then one can say the dew point temperature of {0.8, 307.2 K} is 303.2 K.

Honey, a high sugar concentration (greater than 0.8) fluid, is made by honeybees from flower nectar, a lower sugar concentration liquid (0.1–0.5), collected from numerous flowers sometimes at a considerable distance from the nest (up to 9 km) [9]. This nectar is passed by the forager honeybee to another [10] honeybee (unloader/storer), which then starts the desiccation process by selectively heating and aerating the nectar with their mouth parts while placing it in a honeycomb cell. This partially desiccated nectar is then exposed to low humidity air [11], while the hive population engages in vigorous forced air movement within the nest by fanning their wings [10,12,13]. This very energy intensive [8] process of nectar to honey conversion is placed above the brood nest in order to have less than 0.62 RH. After the desiccation process is completed, the cell may be capped with wax to prevent the reabsorption of water vapour. This RH value χHoney, when honey is in equilibrium with the vapour in the air, is termed the water activity of honey [11]. It has been shown to range from 0.5 to 0.7 and has a linear relationship with the water content of the honey (equation (1.1)) [14] (table 1 for term definitions and values).

χHoney=0.2686+1.756(1CHoney). 1.1

There are differences between subspecies as to when they begin the desiccation process, A. m. scutellata in dry hot climates, has been observed to reduce the water content by 50% in flight [23], whereas A. m. mellifera and A. m. ligustica in cooler climates do not [10].

Table 1.

Nomenclature.

term value description units
A factor of coefficient α—vapour fraction of water content of nectar made into honey
B0 factor of coefficient β0—vapour fraction of water content of nectar used as fuel for nectar evaporation
B1 factor of coefficient β1—vapour fraction of water from oxidation of nectar used as fuel for nectar evaporation
AEntrance cross-sectional area of entrance m2
CNectar concentration of nectar kg kg−1
CHoney 0.8 typical concentration of sugars in honey [5] kg kg−1
d0 0.2 diameter of tree cavity [15] m
d1 0.5 external diameter of tree [15] m
L˙meta 10 background colony metabolic rate [16] W kg−1
hTree 1.4 height of tree cavity [15] m
hHive 0.825 internal vertical dimension of hive with four shallows and one deep [17] m
LSucrose 15.1 latent heat of combustion of sucrose (lower heating value, water remains vapour) [18] MJ kg−1
LWater 2.43 latent heat of water vapourization at 305 K (32.8°C) [19] MJ kg−1
r 58 weight of metabolic water released per kilo of sucrose metabolized kg kg−1
TBrood 307.66 brood temperature [20] K
TD dew point temperature K
Ti temperature instance i K
TOut 295.66 temperature outside—for ZDUPSA average Pretoria spring summer (November–February) temperatures [21] K
uEnt air velocity through entrance ms−1
uEntMax 0.94 maximum entrance air velocity [22] due to fanning ms−1
WSucroseBase weight of sucrose in resultant honey kg
WColony 2 background colony population those not involved in foraging or evaporations approximately 20 000 honeybees [5] kg
WNectarDelivered weight of nectar delivered to nest kg
WNectarEvaporate weight of nectar required as fuel for the evaporation of nectar kg
W˙WaterEvaporate rate of water evaporated in honey ripening kg s−1
W˙NestNectar rate of nectar consumption from other processes than honey evaporation kg s−1
W˙HoneyBase rate of honey ripening in terms of resultant honey kg s−1
W˙VapourTotal rate of water vapour production from all sources inside the nest kg s−1
W˙^VapourTotal rate of water vapour removal by all methods inside the nest kg s−1
x0 0.440 internal horizontal dimension of hive [17] m
x1 0.478 external horizontal dimension of hive [17] m
α 1 proportion of evaporate water emitted as vapour while in the nest
β0 1 proportion of water content of nectar consumed emitted as vapour while in the nest
β1 1 proportion of sugar content of nectar consumed emitted as vapour while in the nest
ΓThermal TEE thermal efficiency of desiccation
ξ reciprocal concentration of honey subtract from reciprocal concentration of nectar
ρi density of water vapour in instance i kg m−3
ρInlet density of water vapour entering entrance kg m−3
ρExhaust density of water vapour exiting entrance kg m−3
ΛEvap thermal conductance of the nest enclosure e.g. hive, tree etc. for evaporation processes W K−1
ΛCon thermal conductance of the nest enclosure e.g. hive, tree etc. for condensation processes W K−1
λTree 0.2 thermal conductivity of tree wood [4] Wm−1 K−1
λHive 0.12 thermal conductivity of hive wood [4] Wm−1 K−1
χi relative humidity instance i
χBrood relative humidity inside the brood zone
χOut 0.6 outside relative humidity for ZDUPSA Pretoria summer spring relative humidity [21]
χHoney typical water activity of honey i.e. RH
θi water vapour pressure derived parameter Pa
γi RH derived dimensionless parameter
δi temperature-derived dimensionless parameter

In a nest with a single opening, all fluids from nectar desiccation and other processes must permeate through the walls or pass through the entrance. Water vapour and carbon dioxide can be removed by honeybees fanning at the entrance [5], achieving a maximum entrance air velocity of approximately 1 m s−1 [22,24]. While beekeepers often, in addition to a mesh floor, provision multiple entrances in summer totalling over 80 cm2 [17]; honeybee swarms prefer nests with single entrances of 12 cm2 or smaller [5]. However, water vapour converts back to a liquid by condensation, a process which needs the energy to be removed from the water vapour laden air. The principle of conservation of energy means that the rate of condensation is dependent on the lumped conductance of the nest walls, and the temperature difference between the dew point temperature of the humidity on the inside surface in the condensing zones and the outside air.

Values for the nest lumped conductance in a winter configuration have been experimentally measured [4] and represent a realistic estimate of the lower end of nest conductance. A realistic upper limit for nest conductance can be found analytically using standard shape factors [25].

The permeability of the honeybee applied propolis lining (plant resins) is of the order of 10–13 kg m−1 s−1 Pa−1 [26]. This results in a flow rate of the order of 2 mg s−1 at a water vapour pressure differential of 5 kPa and a thickness of 0.25 mm. This is insignificant compared to water removal rates up to 100 mg s−1 for condensation and advection.

Research into the humidity relations of A. mellifera, while less extensive than for temperature, has found that honeybee eggs require 5.1 kPa {0.9, 308.2 K} for development [27] and larvae require greater than 4.1 kPa {0.75, 307.7 K} [28]. The particularly high humidity for honeybee egg hatching should be taken in the context that the eggs are laid at the far end of the cells, a microclimate separated from the general nest environment [29,30]. However, fully grown larvae, which may then be infested with varroa, have conditions approaching that of the general nest environment.

Researchers have shown varroa fecundity falls significantly at humidities close to 4.3 kPa i.e. [31] 4.3 kPa {0.8 307.2 K}, [32] 4.2 kPa {0.75, 308.2 K}, [33] 4.3 kPa {0.7, 309.7 K}, [34] 4.2 kPa {0.872, 305.6 K}. Despite this, varroa has spread to honeybee colonies in a wide range of climates.

Condensate collection inside the hive or water disposal in the liquid phase by A. mellifera are not addressed in the literature. This absence has been noted by others [35].

The most recent and comprehensive studies into honeybee nest humidity have been undertaken by the Zoology department of the University of Pretoria in South Africa (ZDUPSA), and in a body of work related to humidity for A. m. scutellata have covered: the effects of external weather, winter clustering, differing nest types, hygropreference and honeybee fanning behaviour [20,23,3638]. This analysis, inspired by their work, seeks to provide the thermofluid theory to both explain and extend it while using their climate and fanning data for input, and their results for experimental validation where possible.

2. Approach

This analysis will use a steady state, simple zoned temperature model of the nest cavity with a single bottom entrance, all at the same constant humidity, but at different average temperatures and consequently different average relative humidities consisting of:

  • A honey/nectar zone below 0.6 RH at a temperature above 307.7 K [14,20].

  • A brood zone at 307.7 K (34.5°C) with a maximum humidity of 4.9 kPa {0.9, 307.7 K} [5,20].

  • A condensing zone at the dew point temperature, i.e. internal surface of the cavity.

In this model, which is a simplification of a complex system:

  • Water vapour enters the system from nectar evaporation, nectar consumption and through entrance inlet airflow by forced convection.

  • Water vapour leaves via condensation and entrance exhaust flow.

  • Heat energy is produced by metabolizing sugars.

  • Heat energy exits via conduction through the nest walls. The heat flows of the entrance gases are insignificant in comparison (approx. 10 mW versus approximately 100 W) [8] and ignored.

  • The pollen to insect protein process is considered as a constant rate metabolic energy overhead that consumes nectar, releasing water vapour from its water content and oxidation.

In reality, the honeybee nest is a set of complex interconnected processes as shown in figure 1, involving the fluids: nectar (orange), externally collected water (blue), condensate water (green) and gases (red). The latter are a mixture of air, water vapour and CO2. These are advected through the entrance and circulated between: a brood zone kept at a constant temperature, a nectar zone at elevated temperature for evaporation, and a lower temperature condensation zone.

Figure 1.

Figure 1.

Nest fluid transfer and phase change processes.

By using the standard thermofluid techniques of energy and mass balances across the system boundary to determine the ability of honeybees to dispose of the water vapour generated and therefore the resultant average humidity, this approach removes the necessity to analyse the internal detail while retaining validity.

To populate the model, the climatic and fanning behavioural data are from ZDUPSA [20] and the results, generated using MATLAB [39] are correlated to their findings [3638] (electronic supplementary material).

2.1. Water vapour production rate

For the purposes of this analysis, water vapour production consists of five components:

  • Water evaporated from nectar, at honey production rates of 5 mg s−1 (1 lb day−1) and may exceed 25 mg s−1 (5 lb day−1) [10,12].

  • Water content from the nectar used as fuel for nectar evaporation.

  • Metabolic water production from the nectar used as fuel for nectar evaporation.

  • Water content from the nectar used for other processes in the nest.

  • Metabolic water production from the nectar used for other processes in the nest.

The weight of water entering the vapour phase in the nest is defined in equation.

W˙VapourTotal=αW˙WaterEvaporate+[W˙NectarNest+W˙NectarEvaporate][β0(1CNectar)+β1CNectarr].

The coefficients α, β0, β1 define the proportion resulting in water vapour (vapour fraction) inside the nest from three classes of water source:

  • Water content of nectar that is ‘made’ into honey α.

  • Water content of the nectar consumed as metabolic fuel β0.

  • Water from the oxidation of the sugars from nectar consumed as fuel β1.

Similarly, 1 − α 1 − β0 and 1 − β1 are the proportions that are excreted or do not arrive at the nest.

If one considers only the delivered nectar concentration, as opposed to the collected nectar concentration, then differences between races of honeybee desiccating the nectar in flight can be ignored (A. m. mellifera and A. m. ligustica [40] versus A. m. scutellata [23]). Then according to the behaviours described one may determine α ≈ 1 [40]. From the winter behaviour of not defaecating for extended periods [5], one can deduce that β1 can be close to unity and, from their consumption of honey with an approximately 0.2 water content during winter, that β0 can be non-zero. More precise values, or the validity in the nectar gathering season, are unknown. The analysis can assess the significance of these coefficients and consequently their importance for further research. For other purposes, assumptions may have to be made about these coefficients.

The amount of water to evaporate and the fuel required for evaporation W˙WaterEvaporate,W˙NectarEvaporate are dependent on the rate of honey production, nectar concentration and the thermal efficiency of the nectar evaporating process TEE or ΓThermal, as shown in the expressions in previous work [8]. TEE is derived from the nest thermal conductance. However, depending on the nest configuration and the honeybee behaviours, the nest thermal conductances for evaporation and condensation may differ from each other, particularly in larger or higher aspect ratio nests that may give more space for stratification. Using the equation for the break-even energy margin from [8], an equation can be derived that gives maximum water vapour production at the minimum thermal efficiency for a specific nectar and honey concentration.

The rate of consumption of nectar for other metabolic processes W˙NectarNest is dependent on the honeybee colony mass and the metabolic rate, which is dependent on the nest internal temperature and hence the external temperature and the nest thermal conductance [4]. However, as a simplification, this rate of consumption will be assumed to be disjoint from the evaporation and condensation processes and a fixed value in this analysis, to concentrate on the effects of nectar condensation. Full integration into the analysis is left for future research.

2.2. Water removal rate

The total capacity for water removal is the sum of the water vapour that exits the entrance and that condensed inside the nest. The rate of condensation is defined by the latent heat lost through the nest walls as heat lost via entrance airflow is insignificant in comparison. The water vapour exhausted is characterized by the vapour density of the air and the total flow through the entrance. The maximum dew point temperature and hence exhaust water vapour density and exhaust water mass are defined by the following constraints:

  • 1. The brood area is not above 4.9 kPa {0.9, 307.7 K} [20]. This defines the limit of the vapour pressure and vapour density for the gas exhausted by fanning and the dew point for condensation.

  • 2. Honey can be ripened. This defines a vapour pressure that results in the maximum honey water activity (0.6) below a maximum achievable honeybee temperature of 318.2 K [41].

  • 3. The maximum fanning air velocity (0.924 ms−1 [22])

The fanning response to humidity is fitted, using a cubic polynomial (R2 0.9934), to the ZDUPSA normalized data with the presence of brood [20], as shown in figure 2, assuming the honeybees deliver air velocity proportional to this response up to their maximum.

Figure 2.

Figure 2.

Fanning response versus vapour pressure kPa using data from [20]. (Online version in colour.)

Fanning responses to carbon dioxide levels can be ignored as they cannot exceed 20% of water vapour partial pressure during nectar evaporation [8,42].

The climatic information, i.e. ambient temperature and humidity used in the analysis will be for the same location, i.e. Pretoria South Africa averages for spring and summer (November to February) of 295.7 K (22.5°C) and 0.595 RH [21].

Honeybee constructions and behaviours, as well as the nest walls, define a lumped conductance for the condensation process. Limits of conductance of the nest walls for both tree and man-made nests are derived from standard shape factors and techniques [25] using average dimensions from the literature [4,15]. For hives, the upper limit of one brood box and four shallows [17] will be used.

The energy balance of wall heat conduction and the heat produced by condensation produces an equation in terms of the dew point, which is then solved.

3. Analysis

3.1. Assumptions

The following assumptions in addition to those in §3 are made:

  • 1. System is in equilibrium, i.e. steady state.

  • 2. Entrance air velocity is proportional to fanning response and is independent of entrance size, i.e. sufficient fanning honeybees will be recruited.

  • 3. Water vapour losses or gains through permeation of the nest enclosure and its internal coating of propolis are insignificant.

  • 4. Water vapour pressure is the same throughout the nest or hive.

  • 5. There is only one entrance or vent and it is at the bottom of the nest or hive.

  • 6. The energy changes due to the thermal capacities of the fluids crossing the system boundaries are negligible compared to those involved in the state changes.

3.2. Basics

The partial pressure of water vapour is given in equation (3.1) after [43,44]

Pi=610.78χie[17.2694(Ti273.16/Ti35.86)], 3.1

and the vapour density from (3.2).

ρi=0.002166PiTi. 3.2

Let the following parameters be defined for instance i of temperature, RH and vapour pressure in (3.3), then equation (3.1) becomes (3.4) and at the dew point (3.5)

δi=Ti273.16Ti35.86γi=logχi17.2694θi=117.2694log(Pi610.78), 3.3
θi=γi+δi 3.4
andθD=δD. 3.5

If conditions change (RH, temperature) but the vapour pressure remains constant from instance j to i then

θj=θi=γj+δj=γi+δi. 3.6

Then (3.7), (3.8) and (3.9)

Pi=610.78e[17.2694θi], 3.7
Ti=273.1635.86δi1δi=273.1635.86(θjγi)1(θjγi) 3.8
andχi=e[17.2694γi]=e[17.2694(θjδi)]. 3.9

The upper limits of conductance for condensation in tree nests and man-made hives are derived from the conductance being the sum of the products of conductivities and shape factors of the components forming the cavities. For the tree nest equation,

ΛConλTree[2πhTreeln(d1/d0)+2πd0241(1/2)(d1d0)]. 3.10

For man-made hives with roof thickness identical to the walls,

ΛConλHive[2πhhive0.785ln(x1/x0)+2x02(1/2)(x1x0)]. 3.11

3.3. Water vapour generation

Taking from reference [8] the following:

The weight of evaporate

WWaterEvaporate=WSucroseBase(1CNectar1CHoney)=WSucroseBaseξ. 3.12

In terms of the rate of production of honey

W˙WaterEvaporate=CHoneyW˙HoneyBaseξ. 3.13

The weight of nectar metabolized

W˙NectarEvaporate=LWaterW˙SucroseBaseξCNectarLSucroseΓThermal=CHoneyLWaterW˙HoneyBaseξCNectarLSucroseΓThermal. 3.14

The volume of nest nectar consumed for other purposes is derived from the mass of the colony and the metabolic rate (3.15).

W˙NectarNest=L˙metaWColonyLSucroseCNectar. 3.15

By substitution of (3.14) and (3.15) into (2.1) gives.

W˙VapourTotal=αCHoneyW˙HoneyBaseξ+[L˙metaWColonyLSucroseCNectar+CHoneyLWaterW˙HoneyBaseξCNectarLSucroseΓThermal]×[β0(1CNectar)+β1CNectarr]. 3.16

Nectar collection and ripening are subject to the break-even constraint for the energy margin M for nectar collection from reference [8] which is maximized when the nectar source is close to the nest, hence

LSucroseLWaterξΓThermal. 3.17

Using (3.17), the water vapour rate for the value of TEE that breaks even in energy is given below in (3.18).

W˙VapourTotal=αCHoneyW˙HoneyBaseξ+[L˙metaWColonyLSucrose+CHoneyW˙HoneyBase][β0(1CNectar1)+β1r]. 3.18

For colony to be successful then the power consumed by background metabolism must be insignificant compared to the rate at which energy is stored by the colony i.e. inequality (3.19)

L˙metaWColonyCHoneyW˙HoneyBaseLSucrose. 3.19

Then (3.18) becomes (3.20), the maximum possible water production, similarly at TEE = 1 equation (3.21). Both equations are of the form (3.22).

W˙VapourTotalCHoneyW˙HoneyBase[αξ+β0(1CNectar1)+β1r], 3.20
W˙VapourTotalCHoneyW˙HoneyBase[αξ+LWaterξLSucrose(β0(1CNectar1)+β1r)] 3.21
andW˙VapourTotalCHoneyW˙HoneyBase(αA+β0B0+β1B1) 3.22

3.4. Water removal capacity

Assuming the condensing region to be of uniform temperature in equilibrium, the gas volume in the cavity as incompressible, and the amount of energy dissipated via the entrance by advection is negligible [8], then latent heat of condensation is dissipated by the nest walls, giving the energy balance shown in

W˙CondensateLWaterΛCon(TDTOut)where{TDTOut}. 3.23

The entrance velocity is described as the product of the maximum air velocity and cubic polynomial function with respect to RH at brood temperature 307.7 K. An RH at a known temperature is related to a dew point temperature T expressed as parameter δD by a function derived from equations (3.6), (3.7) and (3.8) to give

χ=e[17.2694(δDδBrood)]. 3.24

Substituting (3.24) into the polynomial gives

uEnt(TD)=uMax[a3e3[17.27(δDδBrood)]+a2e2[17.27(δDδBrood)]+a1e[17.27(δDδBrood)]+a0]. 3.25

The total water removal capacity equals the sum of advection and condensation hence

W˙^VapourTotal=ΛConLWater(TDTOut)+AEntuEnt(TD)2(ρExhaustρInlet). 3.26

Using equation (3.2) for the density of a vapour and (3.1) for the vapour pressure at the dew point TD gives

W˙^VapourTotal=ΛConLWater(TOutTD)+0.6615AEntuEnt(TD)(e[17.27θD]TDe[17.27θOut]TOut). 3.27

ΛCon and uEnt in equation (3.27) are expanded using (3.25), (3.10), (3.11) and (3.3) for the range of man-made hive and the tree nest cases and then solved for TD. With TD known, one can determine the brood zone RH using (3.24).

Brood zone air at humidity {χi, TBrood} is elevated to desiccating temperature, THoney, in the nectar/honey zone at the honey activity χHoney where {χi, TBrood} = {χHoney, THoney}, as shown in equation (3.28), which is derived from equation (3.8).

THoney=273.1635.86(γi+δBroodγHoney)1(γi+δBroodγHoney). 3.28

4. Results

The honeybee fanning information is derived from honeybee colonies in Pretoria South Africa. As a consequence, the climatic data used are from that location.

4.1. Water vapour production

The break-even point values of TEE, where maximum water vapour production occurs, vary with nectar concentration as plotted in figure 3 from equation (3.17). This maximum water production was plotted in figures 4 and 5 using equations (3.27) and (3.23). This is compared as a ratio to the minimum water production (TEE = 1.0) as shown in figure 6 using equation (3.16). The minimum water production is also shown in figure 7 Note: α β0 β1 are assumed to have a value of 1 in both figures 4 and 6.

Figure 3.

Figure 3.

TEE to nectar concentration at break-even point at zero nest to flower distance. (Online version in colour.)

Figure 4.

Figure 4.

Maximum water product at break-even TEE. (Online version in colour.)

Figure 5.

Figure 5.

Break-even water production contours mg s−1 versus nectar concentration and honey rate.

Figure 6.

Figure 6.

Ratio of minimum to maximum water product (Min: TEE = 1, Max: TEE = break-even). (Online version in colour.)

Figure 7.

Figure 7.

TEE = 1 water production contours mg s−1 versus nectar concentration and honey rate.

Water production is dependent on three coefficients α, β0, β1, which are multiplied by the terms A, B0 and B1 the relative magnitude of these terms are plotted in figure 8, for the case of TEE equal to one, and figure 9 where TEE is at the break-even value using equations (3.20), (3.22) and (3.21).

Figure 8.

Figure 8.

Water product factors at TEE = 1. (Online version in colour.)

Figure 9.

Figure 9.

Water product factors at TEE break-even. (Online version in colour.)

4.2. Water vapour removal capacity

The scenarios studied are divided into two nest types; a tree with a fixed height cavity and a man-made hive that can have a variable height. Each nest type is divided into four combinations of high and low lumped thermal conductance, small and large entrances. The entrance and nest dimensions are taken from sources [4,17]. Equations (3.10) and (3.11) provide conductances as shown in table 2.

Table 2.

Water removal capacity of nest limits of conductance and entrance area, at water vapour contents (a) 4.3 kPa and (b) 4.9 kPa.

water removal mg s−1
# nest description Aent cm2 ΛCon WK−1 1. (a) 2. (b)
A tree nest low conductance, small entrance 7.5 0.4 5.6 9.8
B tree nest low conductance, large entrance 15 0.4 9.8 17.9
C tree nest high conductance, small entrance 7.5 2 10.9 16.4
D tree nest high conductance, large entrance 15 2 15.1 24.5
E man-made hive, no shallows, small entrance 6.5 2.5 11.9 17.5
F man-made hive, no shallows large entrance 83 2.5 55.6 100.2
G man-made hive, four shallows small entrance 6.5 12 43.4 57.1
H man-made hive, four shallows large entrance 83 12 86.7 139.8

Using equation (3.27), one can then calculate the water vapour that can be removed by various combinations of entrance and condensation as shown in table 2 where A, B, C and D represent the limits of conductance and entrance area for a tree nest and E, F, G and H for man-made hives. The water removal capacity is tabulated at two levels of humidity 4.3 and 4.9 kPa. The spread of conductance and entrance area is shown in figure 10 against the contours of water removal at 4.9 kPa. The brood zone humidity versus water removal capacity is plotted in the figures 11 and 12. The humidities of optimal egg survival; the upper limit of varroa breeding success; Miami USA; summer Pretoria SA and winter Pretoria SA are shown for comparison.

Figure 10.

Figure 10.

Tree and man-made nest limits plotted onto contours of water removal versus nest conductance and entrance area. (Online version in colour.)

Figure 11.

Figure 11.

Man-made hive brood zone humidity. (Online version in colour.)

Figure 12.

Figure 12.

Tree nest brood zone humidity. (Online version in colour.)

The nectar desiccating temperature of the nectar/honey zone was plotted as contours against the brood zone vapour pressure and the resultant honey water content [14] and the resultant honey water content. This was calculated using equations (3.28) and (1.1) and shown in figure 13. The vertical dashed line indicates a typical long-term storage water content of 0.2. The horizontal dashed line indicates 4.3 kPa, the upper limit of varroa breeding success.

Figure 13.

Figure 13.

Contours of nectar/honey zone nectar desiccating temperature versus water content, 1 − CHoney and brood zone vapour pressure. (Online version in colour.)

4.3. Experimental agreement

The analysis indicates lower water vapour removal capacity in tree nests. Thus, one may expect to find higher humidities observed compared to hives when nectar ripening activity is not intense. Unfortunately there are no studies available that give sufficient information to infer the rate of water vapour production; however, a ZDUPSA study [38] did conduct a simultaneous measurement of humidity in both trees and man-made hives. It is reasonable to assume similar rates of water vapour production and thus predict the humidity in one environment given the humidity of the other using the model with median conductances for both nests. The observed humidity in the trees in the study was approximately 3.8 kPa {0.7, 307.7 K} which results from approximately 7 mg s−1 of water production according to the model in figure 12. Then using this water production in a median hive, it is predicted that this would produce approximately 3.0 kPa as shown in figure 11. This agrees with the ZDUPSA experimental values in the range 3.0–3.3 kPa.

Further, the model determines that, if the nectar flow is zero or low and fanning is not taking place, the removal of water vapour is primarily by condensation. Then the humidity is constrained by the internal nest surface temperature at saturation from equation (3.23) i.e. dew point. In the high conductance hives, this will be within a few degrees of the outside air temperature i.e. {1.0, approx. TOut}. ZDUPSA conducted two humidity studies in winter [36,38] in average ambient temperatures of 288 K. The elevation of inside temperature above ambient for wooden hives in cool winter configuration is around approximately 5 K [4] and less in warmer ambient temperatures. The model predicts then that the nest humidity will be about {1, 288 + 5} equal to {1, 293 K} or 2.3 kPa. The average observed humidity in the ZDUPSA experiment was between 1.9 kPa {0.35, 307.7 K} and 2.5 kPa {0.45, 307.7 K}. Another similar, earlier study in the UK [45] showed the internal dew point 7° higher than the external winter ambient temperature, which again concurs with the model.

5. Discussion

This is a zoned steady-state analysis of the averages of micro climates within the zones, thus extrapolating what occurs during the daily cycle is open to errors owing to thermal diffusivity, commonly known as thermal inertia. Thus, internal humidity changes due to condensation will follow, but lag behind and are less severe than predicted from the external daily temperature changes depending on the construction, contents of the nest and amount of insolation. This lag and averaging out will be most pronounced in the high thermal capacity and low conductance of tree nests. Further, water production and removal are not completely synchronous, as average nest humidity increases following foraging activity and then decreases with time as nectar desiccation proceeds, often at night, after the cessation of foraging.

There is considerable further work in finding: data on thermal diffusivity and time-varying nectar gathering and desiccation rates, to populate a more accurate transient-based analysis; factors governing microclimates within the zones, to determine their limits. However, this analysis should be sufficient to act as an aid to interpreting the daily rise and fall of hive humidity.

5.1. Factors in water production

During nectar desiccation the overwhelming majority of the water vapour in the nest is a direct consequence of the nectar desiccation, the water vapour from the rest of the hives nectar consumption and metabolism becomes an insignificant factor, as can be seen in figures 5 and 7 from the values of contours that cross the zero honey rate-axis.

TEE has a profound effect on water production as can be seen in the degree of variation between maximum and minimum values shown in figure 6, where for typical concentration ranges (0.2–0.4) and honey ripening rates 5–15 mg s−1 the minimum to maximum ratio is 0.5–0.75. TEE also has a limiting effect on usable nectar concentration. If one looks at figure 3, for the value of TEE equal to 1, the corresponding nectar sugar concentration is 0.132 kg kg−1. This value provides an indication of the lowest level of nectar resource that is of long-term use to honeybees even in the most favourable conditions.

To understand the importance of the various sources of water within the nest, one needs to compare their relative magnitudes as shown in figures 8 and 9. These show the relative magnitudes of the terms (A, B0, B1) that are multiplied by the coefficients (α, β0, β1). When TEE is equal to one, figure 8, it reflects a scenario where the external temperature is close to that inside the nest, i.e. tropical. By contrast, figure 5 is a colder climate, high heat loss scenario at the break-even point, where the colony is at its most stressed. In the ‘tropical’ scenario one can see that B1 and B0 both remain smaller than A except at very weak concentrations. The ‘colder’ scenario, however, has a high relative value for B0 throughout the concentration range. This indicates the water content of nectar used as fuel to desiccate the honey is a significant contributor of water in the nest. The magnitude of B0 means the coefficient β0c, the vapour fraction of nectar fuel water content, is an important value for the science related to honeybees in colder climates. Unlike α, β0 can currently only be inferred and assumed.

5.2. Humid brood zone, dry nectar honey zone

Honeybees appear on first inspection to have conflicting requirements of a high-temperature humid brood zone and dry air needed for nectar desiccation. If one looks at figure 13, one can see that if the humid air from the brood zone is heated it can desiccate nectar to low moisture levels. If air containing 4.3 kPa of water is then heated to 312 K then it will desiccate nectar to produce honey with only 20% water. This water content is low enough to prevent microbial growth in the honey and the vapour pressure is high enough to hinder the breeding of varroa. This fulfills both the need to have a long-term food supply and to reduce the impact of this parasite.

In this model, these zones are separated; however, for honeybees, this may not be easy to achieve, particularly in low aspect ratio man-made hives, where thermal stratification is not strong and is often disturbed by beekeepers.

5.3. High humidity required, but low humidity found in man-made hives

There is a marked contrast in humidity between in vitro honeybee rearing 4.1 kPa [28] and man-made hives 2.2–3.3 kPa [36,45]. In the latter, the humidity is measured outside the micro climates in the cells maintained by the nurse honeybees. If A. mellifera optimally evolved for tree dwelling then maintaining this difference between the general humidity and the micro climates must therefore represent a stress condition. The difference arises from the condition that unless there are very high water production rates then internal humidity in high conductance, large entrance hives is tied down to {1, TOut} (dew point ∼ outside temperature) and when large top vent/entrances are added then it is tied to {χOut, TOut}

5.4. Hives good for varroa, tree nests good for honey bees

That high humidities particularly in cooler climates require low thermal conductance enclosures has been discussed in relation to varroa in other work [4] and is an accepted thermofluid phenomenon [46]. In addition, the possible impact of top vents or entrances, using recent thermofluid models [47], has also been discussed [48].

The common practice of man-made hives of thin-walled wooden construction with many shallows on top is shown in the high conductance scenarios (limits E, F, G and H) which result in much higher lumped thermal conductances than tree nests (limits A, B, C and D) of 2.5 to 12 WK−1 versus 0.4 to 2.0 WK−1. This and the very much larger entrances used in summer (limits F, H) tie the humidity close to {1, TOut} at low water production rates and increase the water production rate needed to reach 4.3 kPa, by a factor of five as can be seen in figures 11 and 12 (i.e. 50 mg s−1 versus 10 mg s−1).

Taking nectar concentration of 0.33, typical of oil seed rape, a common European honey producing crop, one can see from figures 5 and 7 that these water production rates imply honey production rates of 12–25 mg s−1 for a man-made hive and 1–3 mg s−1 for a tree nest. This means honeybees in man-made hives need to forage and desiccate honey at 10 times the rate to obtain the 4.3 kPa humidity sufficient to affect varroa fecundity. The foraging conditions needed for these honey production rates will occur less frequently than those required by the modest rates needed by tree nests.

Counterintuitively, a subtropical climate, such as Florida, is not sufficient. The common practice of using high conductance, top vented hives [49,50], ties internal humidity to the outside, which in a Florida summer averages at 2.8 kPa {0.72, 301 K} [51]. At low water production levels, in this climate and hives, but without top vents, the humidity will only accumulate to ca 3.8 kPa, allowing varroa to proliferate.

However, with a sustained average outside temperature of above 303.2 K, e.g. warm desert areas of southern Algeria, the analysis shows a high conductance hive, without top vents, can accumulate 4.3 kPa. This may account for the reported higher brood infestation in northern compared to southern Algeria [52] where, in the south, for large parts of the year, the average ambient temperature is above 303.2 K [53]; yet in the north, the average summer temperature is 298 K [21] with a corresponding hive humidity of 3.2 kPa.

In addition, better nectar sources and higher external temperatures, factors shown in this analysis to give higher nest humidity, have been positively correlated with reduced varroa infestation in an experimental research of Mediterranean apiaries [54].

Thus changes to beekeeping practice can improve the frequency of varroa disrupting high humidity for man-made hives: improved foraging, avoiding top vents, constructing hives from lower thermal conductivity materials, having fewer shallows on the hive by more frequent harvesting and matching entrance size to water removal demand by changing the entrance size in response to changing internal humidity or ripening activity.

6. Conclusion

The thermofluid physics in the production and removal of water vapour bound the behaviours of the honeybee colony. Within the constraints of its steady state, averaging approach and assumptions, this theoretical analysis explores those boundaries and has found:

  • Honeybees must produce and dispose of considerable quantities of water vapour in order to convert nectar into honey. Typically four to seven times the weight of honey.

  • Climate is a major factor especially when cooler climates are combined with high conductance hives. The fuel used in nectar desiccation then becomes the dominant source of water vapour in the nest.

  • The thermal conductance of the nest and the dimensions of the entrance have a major impact on nest humidity. This makes high humidity a much more likely and frequent occurrence in tree nests and the low humidity found in man-made nests a likely stressor.

  • Low humidities observed in some hives may be a direct result of their construction and thermal conductance.

  • Hive thermal conductance and entrance size can potentially change the impact of varroa on honeybee colonies.

  • Top vents can tie inside to outside humidity, which even in subtropical climates is substantially below the ideal for larval growth and the reduction of varroa fecundity. Therefore, they may increase the levels of honeybee stress and the likelihood of varroa infestation.

Finally, this study shows, through changing hive design and beekeeping practices, how to achieve the absolute humidity level of 4.3 kPa (approx. 30 gm−3), which makes varroa fecundity fall.

Supplementary Material

delta.m

Supplementary Material

Author responses to decision letter comments
rsif20190048supp2.pdf (69.1KB, pdf)

Supplementary Material

fanning.m
rsif20190048supp3.m (1.5KB, m)

Supplementary Material

fWwater.m

Supplementary Material

fWwaterconstrained.m

Supplementary Material

fxi.m

Supplementary Material

gama.m

Supplementary Material

nectartempWK.m
rsif20190048supp8.m (1.6KB, m)

Supplementary Material

nestData.m
rsif20190048supp9.m (1.1KB, m)

Supplementary Material

parameters.m

Supplementary Material

Pretfit.m

Supplementary Material

PretoriaData.m

Supplementary Material

readme.txt
rsif20190048supp13.txt (1.3KB, txt)

Supplementary Material

scenario_P3.m

Supplementary Material

theta.m

Supplementary Material

totalwatergen3.m

Supplementary Material

vChi.m

Supplementary Material

vChiGamma.m

Supplementary Material

vPressure.m

Supplementary Material

vRho.m

Supplementary Material

vTempDelta.m

Supplementary Material

vTemperature.m

Supplementary Material

watergenfactors.m

Supplementary Material

condensateTDu.m

Acknowledgements

The authors thank C. E. Mitchell, for proofreading and Prof. Harvey Thompson, Prof. Keith Walters for feedback on the draft.

Data accessibility

This article has no additional data.

Competing interests

The author has no competing interests.

Funding

The author is not funded by any organization.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials

delta.m
Author responses to decision letter comments
rsif20190048supp2.pdf (69.1KB, pdf)
fanning.m
rsif20190048supp3.m (1.5KB, m)
fWwater.m
fWwaterconstrained.m
fxi.m
gama.m
nectartempWK.m
rsif20190048supp8.m (1.6KB, m)
nestData.m
rsif20190048supp9.m (1.1KB, m)
parameters.m
Pretfit.m
PretoriaData.m
readme.txt
rsif20190048supp13.txt (1.3KB, txt)
scenario_P3.m
theta.m
totalwatergen3.m
vChi.m
vChiGamma.m
vPressure.m
vRho.m
vTempDelta.m
vTemperature.m
watergenfactors.m
condensateTDu.m

Data Availability Statement

This article has no additional data.


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