*The organic nitrogen concentration is a calculated value that is the difference between the concentration of TKN and Dissolved ammonia. The portion of ammonia nitrogen increased during storage by 13.5% (from 59.3% to 72.8%) in the open EMS and by 6.5% (from 72.6% to 79.1%) in the covered EMS, respectively. Concurrently, the organic nitrogen concentrations decreased by 1114 mg/L N in the open EMS and by 288 mg/L N in the covered EMS compared with their respective influents. The mineralization rate on organic nitrogen was 23.7% in the open EMS and 7.8% in the covered EMS. It is noteworthy that ammonia nitrogen was up to 72.6% of TKN in the influent in the covered EMS. This high ammonia ratio suggests that extensive hydrolysis had occurred before the manure entered the EMS. Since the more easily biodegradable organic nitrogen had been mineralised, the bacteria attack the hard decomposable part of organic nitrogen. As a result, a lower mineralization rate on the organic nitrogen was achieved in the covered EMS. The TKN concentration in the open EMS reduced by 37.5% compared to that in its influent. This reduction is primarily the result of sedimentation of volatile solids (containing organic nitrogen) and volatilization of ammonia. The ammonia concentration dropped by 23.4% in the open EMS comparing to its influents. The quantity of nitrogen loss by means of volatilization is hard to measure. However, the value should be greater than 23.4% because a portion of organic nitrogen was converted to ammonia nitrogen during the period of storage. The TKN concentration in the covered EMS was only 6.6% less than that of the influent to the covered EMS. It appeared that the reduction in TKN caused by settling was no more than 6.6% as there was ammonia loss in the biogas released to the atmosphere (4.2). The ammonia concentration increased slightly by 1.7% in the covered EMS. This represented the difference between the ammonia produced in organic matter decomposition and ammonia lost with biogas bubbles release. Comparing the changes in TKN and ammonia nitrogen in the open EMS and the covered EMS systems, the results indicate that the covered EMS can reduce nitrogen loss by approximately 82% and maintain approximately 93% of the nitrogen levels in the influent during the storage period. The nitrogen conservation effect of the Negative Air Pressure Cover System is obvious. Table 4-2 shows the changes in phosphorus concentration in the two EMS systems between influent and treated manure. In all four cases dissolved P accounts for approximately 70% or more of the total P. It should be considered highly available for plants. Phosphorus concentrations significantly dropped in both the open and covered EMS systems during the storage period. Only 28.3% of the Total-P levels in the influent were found to remain in the treated manure in the open EMS, and only 42.3% of the Total-P levels in the influent were found to remain in the treated manure in the covered EMS. Similarly, only 26.5% of the dissolved P levels in the influent were found to remain in the treated manure in the open EMS, and only 58.4% of the dissolved P levels in the influent were found to remain in the treated manure in the closed EMS. These reductions in phosphorus do not necessarily mean phosphorus is lost from the EMS. Theoretically, P should be 100% conserved during anaerobic digestion (Field et al., 1985) and any apparent losses are a result of phosphorus transfer from the liquids to the solids within the EMS. In a covered lagoon digester study, Safley and Westerman (1992a) found that the P concentrations in the effluent were 20 to 30% less than those in the influent. They explained this reduction as probable solids accumulating in the lagoon. The Hydraulic Retention Time used in their study was 67 days. In our study, the average manure storage period in the EMSs was more than 100 day. More P accumulation in the solids is not therefore unanticipated. Total-P in the settled solids accounts for more than 90% of the total in the EMS, even though the liquid occupies the greater portion of an EMS, (Bicudo et al., 1999). Field et al. (1985) pointed out that unstirred digestions of animal manures may have an important fraction of the manure P in the digester due to the settling of manure solids. 4-2 Summary of phosphorus in the open and the covered EMS
The fates of nitrogen and phosphorus in manure slurry are different in an anaerobic EMS system. Nitrogen, primarily, is subjected to the conversion from organic to inorganic form. Nitrogen exists mainly in the liquid portion of an EMS. More than 60% NH3-N and 70% of TKN are found contained in liquid portions of an EMS (Campbell et al. 1997). Phosphorus, on the other hand, moves by means of incorporating orthophosphate, polyphosphate, and organically bound phosphorus into bacteria cells and that settle down to the EMS bottom. Biogas Production Potential In this study, no biogas samples were collected. The discussion of the potential for biogas production will focus on the possibility of methane production by analysis of the volatile fatty acids (VFA) data collected in both EMS. The literature of recent years relating to anaerobic digestion of animal manure contains numerous observations suggesting volatile fatty acid relationships have direct correlation with digester performance and methane production. Acetic acid is known to be the immediate precursor of approximately 70% of all methane formed during digestion. Similarly, propionic acid is the immediate precursor to approximately 70% of acetic acid. These two acids play important roles in indication of successful methane production. Acetic acid concentrations lower than 800 mg/L and the ratio of propionic to acetic (P/A) lower than 1.4 are two indicators for successful methane production (Hill et al., 1987). Table 4-3a and 4-3b illustrate the VFA in both the open and the covered EMS respectively. Acetic acid was the predominant form of VFA appearing in both EMS, suggesting that the carbonaceous organic matter in the swine manure had been decomposed or hydrolysed. The substrate is ready for methanogens to produce methane. Table 4-3a VFA in the Open EMS
Table 4-3b VFA in the Covered EMS
Having methane production potential does not mean that methane will be successfully produced. In an analysis of the acetic acid concentration in the covered EMS (Table 4-3b), it can be seen that the acetic acid level remained high from February to June. High acetic acid levels usually mean methanogens have failed to convert acetic acid to methane and carbon dioxide. During above mentioned period, there was no significant methane production. The acetic acid concentration started to drop down between May and June. This reduction in acetic acid probably resulted from the formation of methane (Eq. 2-1). The following months acetic acid data verified the hypothesis. By July and August, the acetic acid concentration levels were very low in the covered EMS, which is an indicator of successful methane production. The observations of biogas production on the covered EMS support this conclusion. No bubbles of a significant size were observed under the cover from February to May. Large bubbles appeared in late May under the covers and very large bubbles were observed from June to August. No further observations were possible since the primary cell was emptied on August 31 and the secondary cell was emptied on September 1. The number, size and frequency of gas bubbles were not recorded in detail. The dimension of the bubbles formed in the secondary cell in a day is approximately 15 m in diameter and 2 m in height. The volume of bubbles is estimated as 35 to 60 m3. The pressure in the bubbles is higher than barometric pressure because of the accumulation of precipitation on the surface of the cover. When the bubbles moved to the sides of the cell, the blower was able to discharge the gas into the atmosphere. It took the blower 10 to 20 minutes at flow-rates of 50 to 150 L/s to release the gases contained in the bubble. Based on the number and size of bubble as well as the frequency of bubble formation, the biogas production is estimated to be 100 to 300 m3/day in the covered EMS (two cells) in the summer months. The number and size of bubble were usually larger in the secondary cell than that in the primary cell. Acetic acid concentration levels in the open EMS also decreased over the course of the study (Table-4-3a, Figure 4-1). Figure 4-1 shows that the decrease in acetic acid started between June and July, which is one month later than that occurred in the covered EMS. Similarly, acetic acid concentration dropped to below 800 mg/L in August, which also happened one month later than that did in the covered EMS. These facts indicate that biogas production occurred later in the open EMS than in the covered EMS. The most probable reason for later methane production in the open EMS than in the covered EMS is that the temperatures in the open EMS were lower than those in the covered EMS. A comparison of the average temperatures in the open and covered EMS between May and August shows the covered EMS was approximately 4-5oC warmer than the open EMS during that period (Figure 4-1). Temperature differences at the bottom of the two EMS were even bigger (Figure 4-3). The temperatures at the bottom of an EMS are significant since most of the biomass, including methanogens, are situated at the bottom. An analysis of propionic concentrations in both EMS shows that the ratio of propionic acid to acetic acid (P/A) remained low in both the EMSs. The maximum P/A in the covered EMS was 0.79, which occurred in June. The maximum P/A in the open EMS was 0.85, which occurred in July. P/A ratios lower than 1.4 indicates that proton-reducing acetogens are more active or, at lest, not less active than acetate-utilizing methanogens in the EMS (Eq. 4-1, 2-1, and 2-2). It appears that reduced methanogens activity is the cause of failure in biogas production in spring and winter. |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Samples |
pH value in the Samples |
||||||||||
Feb. |
Mar. |
April |
May |
June |
July |
Aug. |
mean |
max |
min |
SD |
|
| Influent to open EMS | 7.48 |
6.93 |
7.50 |
6.81 |
6.57 |
6.43 |
6.10 |
6.83 |
7.50 |
6.10 |
0.54 |
| In open EMS |
7.69 |
7.82 |
7.45 |
7.27 |
7.51 |
7.77 |
7.46 |
7.57 |
7.82 |
7.27 |
0.21 |
| Influent to covered EMS | 7.18 |
7.34 |
7.72 |
7.23 |
7.33 |
7.38 |
7.49 |
7.38 |
7.72 |
7.18 |
0.20 |
| In covered EMS | 7.55 |
7.65 |
7.52 |
7.35 |
7.59 |
7.90 |
7.66 |
7.60 |
7.90 |
7.35 |
0.19 |
The alkalinity in both the covered EMS and the open EMS are almost totally bicarbonate alkalinity (BA). The carbonate and hydroxide alkalinity kept below 20 mg/L and 10 mg/L, respectively, in both the open and covered EMS during the entire study period. The ratio of bicarbonate alkalinity (BA) to total alkalinity (TA) is a good indication of the occurrence of digestion. The BA/TA values for the EMS liquid are above 0.85 indicating good biological health (Pos et al., 1985). In fact the BA/TA value for the EMS liquid indicates that the EMS may be underfed biologically (Safley & Westerman, 1989).
Figure 4-2 illustrates that pH levels were fairly constant in both the open and covered EMS during the entire study period. The VFA produced in the acidogenesis phase during anaerobic digestion is neutralised by the alkalinity in the manure.
The temperatures in both open and covered EMS were recorded during the period that manure sampling occurred. EMS temperatures were measured at different depths. At the commencement of sampling of this study in late February, the surface of both the covered and open EMS was frozen and the surfaces of both EMS melted in mid-March.
Figure 4-3 indicates that EMS temperatures varied widely throughout the entire study period. The covered EMS temperature is consistently higher than the open EMS temperature over the entire study period with the exception of April, when the reverse is true. The temperature variation over time shows that the temperatures, from February to April, were low (below 10 oC). These low temperatures are not conducive to anaerobic digestion (biogas production). During that period, no significant biogas can be expected. From May to August, the temperatures in the open and the covered EMS stood above 12oC. Methane production of 0.2 L/g VS destroyed may be expected in the both EMSs in May according to Safley & Westerman (1992a). In this study, however, no significant biogas production occurred in May. Other factors in addition to low temperature are therefore responsible for gas production.

Figure 4-2 VFA, Alkalinity and pH in The Lagoon with and without a Cover

Figure 4-3 Temperature variation in EMSs with depth and with time
1. Temperature at a certain depth in the covered EMS is higher than tha in the open EMS.
2. Temperatures started to rise from March and reach the top value in July, in both EMS.
3. It seems that the average temperatures in the EMS are above 10ºC from May to September,
which minimum temperature for biogas production.
From February to May little difference in temperature occurred between the covered EMS and the open EMS. From May to August, the average temperature in the covered EMS is 4 to 5oC higher than those in the open EMS.
The EMS temperature is a function of depth. Surface temperatures are lower than temperatures taken at depth in the winter, and surface temperatures are higher than temperatures taken at depth in the summer. The variation in temperatures with depth is greater in the open EMS than in the covered EMS (Figure 4-3). The temperature differences during summer months between the surface and at the depth of 5 ft were approximately 5oC in the covered EMS and 10oC in the open EMS. This would suggest that deep (deeper than 7 feet) uncovered EMS are not suitable for use as an anaerobic digester because the temperatures at the bottom (around 10oC) are below temperatures at which anaerobic digestion can occur efficiently.
Organic matter decomposition
Table 4-5a and Table 4-5b illustrate the properties of the organic matter in the EMS
influents in the EMSs. Relatively large standard deviations (SD) are found for all organic
parameters.
Table 4-5a Organic matter in the open EMS influent and in the open EMS
Parameters |
Influent (raw manure) |
In EMS (stored manure) |
removal |
||||||||
Mean |
Max |
Min |
SD |
Mean |
Max |
Min |
SD |
Mean |
|||
| TCOD (mg/L) | 55000 |
110000 | 21000 |
30425 |
14786 |
23000 |
5900 |
6458 |
73.1% |
||
| Soluble COD (mg/L) | 16271 |
24000 |
5900 |
6103 |
7714 |
14000 |
3000 |
3622 |
52.6% |
||
| VS (mg/L) | 32000 |
88000 |
7000 |
28601 |
5129 |
8400 |
2300 |
2486 |
84.0% |
||
| VFA (mg/L as acetate) | 7111 |
9912 |
5708 |
1445 |
4947 |
13218 |
360 |
4208 |
30.4% |
||
Table 4-5b Organic matter in the covered EMS influent and in the covered EMS
Parameters |
Influent (raw manure) |
In EMS (stored manure) |
removal |
||||||||
Mean |
Max |
Min |
SD |
Mean |
Max |
Min |
SD |
Mean |
|||
| TCOD (mg/L) | 38143 |
57000 | 16000 |
13813 |
19790 |
32000 |
6500 |
8660 |
48.1% |
||
| Soluble COD (mg/L) | 8800 |
17000 |
2700 |
4943 |
9078 |
14000 |
2940 |
4471 |
-3.2% |
||
| VS (mg/L) | 27543 |
67000 |
4800 |
21675 |
6836 |
13000 |
1840 |
3647 |
75.2% |
||
| VFA (mg/L as acetate) | 4836 |
7438 |
1374 |
2203 |
4416 |
9439 |
896 |
2736 |
8.7% |
||
Total Chemical Oxygen Demand (TCOD) is used as the measurement of organic concentration in swine slurry and is related to biogas production and cell synthesis. Soluble COD (SCOD) represents the soluble parts of TCOD. The difference between TCOD and SCOD is insoluble or solid COD. Since micro-organisms can only use dissolved and some colloidal organic matter, insoluble COD is seldom discussed in research papers. Insoluble COD can be converted into soluble COD by hydrolytic enzymes. As a result of hydrolysis, SCOD increases, solid COD decreases, TCOD, however, does not change. In a stepwise process, acidogenesis and methanogenesis bacteria decompose the hydrolysis products to inorganic matter, mainly methane and carbon dioxide (known as gas COD, Yang & Moengangongo 1987), or synthesize the hydrolysis products to a cell component that is a kind of insoluble COD.
Volatile Solids (VS) are another measure of organic matter and contribute to TCOD. VS can be classified as Volatile Suspended Solids (VSS) and Volatile Filtrable Solids (VFS). Most of VSS can be removed by sedimentation. As VSS are settled, a portion of solid COD is removed from the liquid.
Volatile Fatty Acids are a component of SCOD, and their removal is mainly by means of methanogenesis biological removal) or volatilization (physical removal).
From the above discussion, it is found that organic matter removal is the comprehensive effect of physical (sedimentation & volatilization) and biological (methanogenesis) processes taking place in an anaerobic digester. Yang & Moengangongo (1987) reported that in a controlled anaerobic digestion, physical removal efficiency (57%) played a dominant part in the overall removal mechanism as compared to the biological removal efficiency (20%). The physical and biological removal efficiencies in lagoons or EMSs is not available in the literature.
Comparing the concentrations of TCOD, SCOD, VS and VFA in the open EMS to its influent concentrations gives an indication of the degree of treatment accomplished by the EMS. The reductions in TCOD, SCOD, VS, and VFA in the open EMS were 73%, 53%, 84% and 30% respectively. The corresponding reductions in the covered EMS were 48%, -3%,75% and 9%, respectively.
There was a large difference in TCOD removal between the two EMSs that mainly resulted from the difference in SCOD removal (reduced by 53% in the open EMS; increased by 3% in covered EMS). As mentioned above, SCOD removal can be accomplished by either biological degradation that is closely related to methane yield, or by volatilization of VFA. From the Table 4-3, it is evident that methanogenesis probably took place in one month (August) in the open EMS. Biological removal was therefore very limited. The probable explanation is that the 53% reduction in SCOD resulted primarily from the volatilization of VFA (that reduced by 30% during the same period). In the covered EMS, VFA volatilization was almost eliminated (minimal release to the atmosphere happened while biogas bubbles were discharged). Consequently, limited physical removal of VFA occurred. The 9% VFA removal resulted mainly from methanogenesis. It can therefore be concluded that the open EMS volatilizes VFA and that this is probably a primary source of odour from open EMS.
The previous discussion was a simplified analysis. The actual change in organic matter during storage is more complicated because some settled organic solids could be hydrolyzed to oligomers or monomers and be metabolized to volatile acids added to dissolved organic matter. If this dissolved organic matter is not physically removed (volatilization) or biologically removed (methanogenesis), it will accumulate in an EMS and result in low removal of TCOD and VS, and an increase in SCOD and VFA. This is what appears to have happened during the first five months (February to June) of this study in the covered EMS. The VFA biological removal (9%) in the covered EMS took place during summer (July to August).
No significant stabilisation (methanogenesis) of organic matter took place in the winter in either the covered EMS or the open EMS. Biogas production (an indication of stabilisation) was observed in the covered EMS from late May to the end of this study in late August. The notable stabilisation of organic matter (VFA decrease) started a month later in the open EMS in June and lasted to the end of the study in early September.
The low stabilisation rate of organic matter in the winter and spring, that occurred in both the covered EMS and the open EMS, was as a result of:
The quality of manure was similar regardless of whether it was stored in the open EMS or in the covered EMS: organic matter was partially decomposed; nitrogen existed mainly in liquid portion; and phosphorus exists mainly in sediments. However, a covered EMS has some advantages over an open EMS.
The covered EMS can retain significantly more nutrient by preventing ammonia from releasing into the atmosphere. The nitrogen loss from the open EMS is approximately 37.5%. Nitrogen loss from the covered EMS is 6.6%. The EMS covered with a Negative Air Pressure Cover System is able to reduce nitrogen loss by 82% compared to the open EMS.
Nitrogen in the EMS is primarily in the form of NH3-N that is ready for the rapid conversion to NO3N after manure application. This is of benefit to the initial crop intake following application. The portion of TKN that is NH3-N is 79.1% in the covered EMS and 73.4% in the open EMS respectively.
Significant biogas production accompanied by a reduction in acetate acid was observed after June in the covered EMS. The biogas production is estimated to be 100 300 m3/day. Based on the acetic acid analysis, biogas production probably started in July in the open EMS, a month later than in the covered EMS. No significant biogas production was observed during winter and spring in the covered EMS.
A higher organic matter removal (73% TCOD) was obtained in the open EMS than in the covered EMS (48% TCOD). The higher removal in the open EMS seemed to be related to VFA emission (physical removal). The volatilization of these VFAs from the open EMS is a major contribution to odour.
The effectiveness of the negative pressure system in retaining heat was observed. The average temperature was 5oC higher in the covered EMS than that in the open EMS during the period from June to September. The higher temperature in the covered EMS resulted in one month earlier biogas production in it than in the open EMS.
The temperatures in the EMSs varies with depth. If an EMS is deeper than 7 feet, the temperature at its bottom will hardly reach 10oC, which hinders the activity of methanogens.
Low initial biomass in the EMSs is a contributing reason for the low stabilization rate achieved in the early storage period. To increase biomass population, some sediments should be kept in EMS at the time the EMS is emptied.
Suggestions for Future Study
This study has demonstrated that significant potential to harvest biogas may exist in a
covered storage. Some adaptations of the storage management might yield significant useful
energy. For example, in the study a biogas yield of 200 m3/day over the period
of April 15 to August 30 would produce 650 gigajoules of energy, with a value of $3500 at
current natural gas prices.
Specific activities which may enhance the knowledge and understanding of potential
opportunities includes the following:
Acknowledgements
In December of 1999, DGH Engineering Ltd. received a research grant from Manitoba Livestock Manure Management Initiative to evaluate changes in the composition of manure during its storage in covered earthen manure storage basins. The primary purposes of the study were twofold: to determine the impact of covers on the conservation of nutrients in stored manure; and to evaluate the role of covers in the stabilisation of organic matter in manure. This study was conducted at two locations, the van Aert Family Farm near St. Clement, Manitoba and the Preun Family Farm near St. Andrews, Manitoba.
From the study, it has been found that nitrogen losses can be reduced by as much as 82% through the use of a cover, and that although the extent of stabilisation of organic matter in manure is comparable for both covered and uncovered earthen manure storages during the winter and spring, covered earthen manure storages experience stabilisation of organic matter, as evidenced by reductions in VFA concentrations, at an earlier point in time in the summer than uncovered earthen manure storages.
DGH Engineering Ltd. would like to express its gratitude to the Manitoba Livestock Manure Management Initiative and the Agri-Food Research and Development Initiative for their assistance, co-operation and advice provided during the course of this study. Additionally, DGH Engineering Ltd. would like to thank both the van Aert Family and the Preun Family for allowing use of and access to earthen manure storages located on their properties and for their ongoing co-operation and assistance throughout the study.
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