| Literature DB >> 25816149 |
René van den Brom1, Hendrik-Jan Roest2, Arnout de Bruin3, Daan Dercksen1, Inge Santman-Berends4, Wim van der Hoek3, Annemiek Dinkla2, Jelmer Vellema5, Piet Vellema1.
Abstract
In 2007, Q fever started to become a major public health problem in the Netherlands, with small ruminants as most probable source. In order to reduce environmental contamination, control measures for manure were implemented because of the assumption that manure was highly contaminated with Coxiella burnetii. The aims of this study were 1) to clarify the role of C. burnetii contaminated manure from dairy goat farms in the transmission of C. burnetii to humans, 2) to assess the impact of manure storage on temperature profiles in dunghills, and 3) to calculate the decimal reduction time of the Nine Mile RSA 493 reference strain of C. burnetii under experimental conditions in different matrices. For these purposes, records on distribution of manure from case and control herds were mapped and a potential relation to incidences of human Q fever was investigated. Additionally, temperatures in two dunghills were measured and related to heat resistance of C. burnetii. Results of negative binomial regression showed no significant association between the incidence of human Q fever cases and the source of manure. Temperature measurements in the core and shell of dunghills on two farms were above 40°C for at least ten consecutive days which would result in a strong reduction of C. burnetii over time. Our findings indicate that there is no relationship between incidence of human Q fever and land applied manure from dairy goat farms with an abortion wave caused by C. burnetii. Temperature measurements in dunghills on two farms with C. burnetii shedding dairy goat herds further support the very limited role of goat manure as a transmission route during the Dutch human Q fever outbreak. It is very likely that the composting process within a dunghill will result in a clear reduction in the number of viable C. burnetii.Entities:
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Year: 2015 PMID: 25816149 PMCID: PMC4376525 DOI: 10.1371/journal.pone.0121355
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Fig 1Schematic drawing of dunghill cross section (a). Schematic drawing of dunghill as simplified for setting up an energy balance (b).
In Fig. 1a, a schematic drawing of dunghill cross section, placed on a concrete floor is presented. Please note that in reality the shape of a dunghill is less smooth. Calculations were performed with a height of the dunghill of 2.5 m, a width of 5 m, and a length (into the paper) of 10 m. These dimensions approach those of the dunghill of farm A. The measurement locations for shell and core temperatures are indicated. r = radius [m], T = temperature [°C]. In Fig. 1b, the dunghill was modelled as a hollow cylinder of infinite length with an inner radius of 0.5 m and an outer radius of 2.5 m. Temperature prediction was only possible between both temperature measurement locations (Tcore and Tshell). r = radius [m], T = temperature [°C].
Fig 2Distribution of manure and incidences of human Q fever patients.
In Fig. 2a, twelve dairy goat farms with abortion waves caused by Coxiella burnetii in 2008 and/or 2009 (case farms; red dots), and 24 dairy goat farms without notified abortion waves caused by C. burnetii, bulk tank milk (BTM) PCR negative results between 2009 and 2014, and BTM ELISA negative results in 2008 from which records of manure distribution were available (controls; green dots), as well as incidences (number of cases per 100,000 residents) of human Q fever patients (the darker area, the more human Q fever patients) are presented. In Fig. 2b, distributions of manure from case farms outside a radius of ten km around case farms to four-digit postcode areas (dark colored) are presented. In Fig. 2c, distributions of manure from control farms outside a radius of ten km around case farms to four-digit (dark colored) are presented.
Fig 3Outside and dunghill temperatures during the experiment.
In Fig 3a, temperatures in the core (dark blue) and shell (red) of the dunghill on farm A are presented. In Fig 3b, temperatures in the core (dark blue) and shell (red) of the dunghill on farm B are presented. For both farms, the average (yellow), the minimum (turquoise) and the maximum (purple) outside air temperature in Eindhoven, the Netherlands (www.knmi.nl) during the experiments are shown. All temperatures are in degree Celsius.
Fig 4Estimated temperature profiles inside the dunghill at Farm A on 4th November 2009.
Cases for Qprod = 0 (only conduction, Equation 3) and for Qprod = 50 W/m3 and λ = 2 W/m∙K (conduction and heat production, Equation 2) are shown. The λ value of wet soil is taken [20], the value for Qprod was estimated based on heat transfer calculations using the outdoor air temperature on 4th November 2009.
Estimated temperature profiles in 18 segmented parts of dunghill A.
| Temperature [°C] | Longest consecutive period above a certain temperature [°C] | Reduction[%] | % of the volume of the dunghill (cumulative) | ||||||
|---|---|---|---|---|---|---|---|---|---|
| Half ring | <30 | 30–40 | 40–50 | ≥50 | T (days) | Max | Average | ||
| 1 | 0.16 | ||||||||
| 2 | 0.48 (0.64) | ||||||||
| 3 | 0.8 (1.44) | ||||||||
| 4 | 1.12 (2.56) | ||||||||
| 5 | 1.44 (4) | ||||||||
| 6 | 36 | 46 | 15 | 0 | >40(15) | 43 | 42 |
| 1.76 (5.76) |
| 7 | 26 | 47 | 24 | 0 | >40(17) | 44 | 43 |
| 2.08 (7.84) |
| 8 | 21 | 44 | 32 | 0 | >40(32) | 46 | 44 |
| 2.4 (10.24) |
| 9 | 17 | 42 | 38 | 0 | >40(38) | 47 | 45 |
| 2.72 (12.96) |
| 10 | 14 | 39 | 40 | 4 | >40(44) | 51 | 46 |
| 3.04 (16) |
| 11 | 10 | 39 | 40 | 8 | 53(3) | 53 | 53 | 100 | 3.36 (19.36) |
| 12 | 6 | 38 | 33 | 20 | ≥55(3) | 56 | 55 | 100 | 3.68 (23.04) |
| 13 | 5 | 36 | 31 | 25 | ≥56(4) | 58 | 57 | 100 | 4 (27.04) |
| 14 | 3 | 33 | 33 | 28 | ≥55(8) | 59 | 58 | 100 | 4.32 (31.36) |
| 15 | 1 | 35 | 30 | 31 | ≥57(7) | 61 | 59 | 100 | 4.64 (36) |
| 16 | 1 | 34 | 30 | 32 | ≥55(10) | 62 | 60 | 100 | 4.96 (40.96) |
| 17 | 1 | 31 | 31 | 34 | ≥55(11) | 64 | 60 | 100 | 5.28 (46.24) |
| 18 | 1 | 26 | 35 | 35 | ≥56(11) | 65 | 62 | 100 | 5.6 (51.84) |
| 19 | 1 | 24 | 34 | 38 | ≥58(11) | 67 | 63 | 100 | 5.92 (57.76) |
| 20 | 1 | 23 | 33 | 40 | ≥56(12) | 68 | 64 | 100 | 6.24 (64) |
| 21 | 1 | 23 | 32 | 41 | ≥57(12) | 69 | 65 | 100 | 6.56 (70.56) |
| 22 | 1 | 22 | 31 | 43 | ≥58(12) | 70 | 66 | 100 | 6.88 (77.44) |
| 23 | 1 | 20 | 31 | 45 | ≥59(12) | 71 | 67 | 100 | 7.2 (84.64) |
| 24 | 7.52 (92.16) | ||||||||
| 25 | 7.84 (100) | ||||||||
aTemperature profiles in the segmented parts 1, 2, 3, 4, 5, 24 and 25 fell outside the scope of the two measurement locations in the dunghill (see Fig. 5). These are therefore outside the range of validity of the temperature profile model.
bFor each segmented part, the number of days that the estimated temperature in the dunghill fell within a certain temperature interval during the 97 days of the experiment is presented.
cThe combination of the minimum daily temperature (T) with the longest consecutive time interval (days) that could achieve the maximum reduction percentage. In all cases, the highest temperature fell within this period. For the longest consecutive time period also the maximum and the average temperature are determined.
dEstimated reduction percentage of C. burnetii in the dunghill according to comparison with described decimal reduction time (DRT) in milk, as described by Enright et al. [21] and extrapolated using Equation 4.
eFor the segmented parts 6–10, the reduction percentage of C. burnetii could not be quantified based on the calculated temperature profiles. Reduction percentages in these segmented parts are less than 100% when compared to DRT of C. burnetii in milk [21]. Nevertheless, based on DRT in goat manure (see Table 3), survival of C. burnetii is just above 3 hours at a temperature of 40 degree Celsius. Therefore, total reduction of C. burnetii in the segmented parts 6–10 might also be possible.
fFor each segmented part, its contribution (%) to the total volume of the dunghill is presented. Also, the cumulative percentage is presented.
Fig 5Cross-section of the dunghill.
Cross-section of the dunghill with the different layers, for which estimated reduction percentage of C. burnetii according to comparison with described decimal reduction time (DRT) in milk, as described by Enright et al. [21] and extrapolated using Equation 4, are described.
Decimal reduction time (in seconds) of the Nine Mile reference strain of Coxiella burnetii at different temperatures in different matrices.
| DRT in seconds (minutes; hours (when the number of hours stayed above 0,1)) | |||||
|---|---|---|---|---|---|
| NM in PBS | NM in 1.8% ammonia | NM in 1.8% urea | NM in manure from deep litter stable | NM in milk (Enright et al., 1957) | |
| Temperature (t) (°C) | 10^(-0.1139t+8.7138) | 10^(-0.1355t+10.383) | 10^(-0.1222t+9.4457) | 10^(-0.0996t+8.0317) | 10^(-0.2253t+17,3307) |
| 40 | 14381 (240; 4) | 918333 (15306; 255) | 36116 (602; 10) | 11161 (186; 3.1) | 208305147 (3471752; 57863) |
| 50 | 1044 | 4055 (68; 1,1) | 2166 (36; 0,6) | 1126 (19; 0.3) | 1163322 (19389; 323) |
| 60 | 66,0 | 113,3 | 123,7 | 113,7 | 6497 (108; 1,8) |
| 65 | 30,0 | 102,2 | 40,0 | 36,1 | 486 (8; 0,1) |
| 70 | 3,3 | 3,8 | 4,6 | 11,5 | 36 |
| 72 | 4,3 | 5,2 | 6,3 | 7,3 | 13 |
DRT, decimal reduction time; NM, Nine Mile reference strain of C. burnetii; PBS, Phosphate Buffer Saline;
aExtrapolated DRT results;
bIntrapolated DRT result.
Coxiella burnetii PCR results in manure from two dairy goat farms.
| Farm | Manure location |
|
| Negative | Not determined |
|---|---|---|---|---|---|
| A | Dunghill | 1 | 8 | 9 | |
| Deep litter stable | 2 | 4 | |||
| B | Dunghill | 10 | 3 | 1 | 5 |
| Deep litter stable | 2 | 1 |
Number of C. burnetii positive samples categorized in manure location per farm. The category ‘Not determined’ reflects samples for which no signals were observed in the internal control, or C. burnetii targets.