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Article

Cattle Manure Fermented with Biochar and Humic Substances Improve the Crop Biomass, Microbiological Properties and Nutrient Status of Soil

1
Department of Agrochemistry, Soil Science, Microbiology and Plant Nutrition, Faculty of AgriSciences, Mendel University in Brno, 61300 Brno, Czech Republic
2
Institute of Chemistry and Technology of Environmental Protection, Faculty of Chemistry, Brno University of Technology, Purkynova 118, 61200 Brno, Czech Republic
3
Institute for Environmental Studies, Faculty of Science, Charles University in Prague, Benatska 2, 12800 Praha, Czech Republic
4
Institute of Environmental Engineering, Warsaw University of Life Sciences, 159 Nowoursynowska, 02-776 Warsaw, Poland
5
Agricultural Research, Ltd., 66441 Troubsko, Czech Republic
6
Department of Geology and Soil Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemedelska 3, 61300 Brno, Czech Republic
*
Authors to whom correspondence should be addressed.
Agronomy 2022, 12(2), 368; https://doi.org/10.3390/agronomy12020368
Submission received: 30 December 2021 / Revised: 24 January 2022 / Accepted: 28 January 2022 / Published: 31 January 2022

Abstract

:
Co-composting of raw manure with other organic sources has recently gained the attention of the scientific community. In the present study, raw manure and manures enriched with humic substances (Humac) or biochar were co-composted to improve their physico-chemical properties. We conducted an experiment including variants consisting of soil amended with manure (M), manure + Humac (M + H), manure + biochar (M + B), and unamended (control). Soil physico-chemical, biological, and plant properties were assessed altogether. All matured manures differed from each other physico-chemically (nutrient content) and in microbial composition, and hence their effects on the observed parameters. Compared to control, the soil respiration and enzyme activities related to N and P mineralization were enhanced due to the amendment of either manure or enriched manures. The M + H treatment resulted in higher pH of the manures as compared to other treatments, whereas the M + B and M treatments revealed the highest Corg contents of the final product, which was negatively correlated with HA:FA. In the same manner, M + H and M + B were the most prominent treatments, causing higher variations in basal soil respiration. The same treatments resulted in the highest percent increase values of soil enzymes related to C, N, and P, which further show the potential of manure modification as a viable option to boost soil fertility and health.

1. Introduction

Decreased soil fertility and degradation of croplands are the key challenges faced by farmers in recent eras. Organic matter is a universal indicator of soil quality and is considered an important component of healthy soils [1]. Its loss or decrease can result in reduced soil fertility or complete degradation of agricultural soils [2]. One way to enhance soil fertility is the use of high-quality manure as the primary source of organic matter and nutrients. Manure application to soil has a positive effect on crop yields, soil chemical and physical properties, and soil microbial activities, resulting in the accelerated recycling of nutrients [3,4,5], with the exception of suboptimal nitrogen: the phosphorus ratio [6]. The quality and composition of cattle manure may vary depending upon the production technology, type of bedding [7] and the used litter, and animal feeding management (type of diet) or animal category (cow, horse, pig, etc.). The resulting product is always characterized by a high content of organic matter and nutrients.
Recent studies have focused on the benefits arising from the enrichment or co-application of manure with biochar or humic substances [8,9]. Biochar is a charred organic material used to enhance soil fertility and to sequester carbon [10]. Biochar production from residual crops biomass offers an opportunity for both using the agricultural co-products more efficiently and reducing the number of agricultural wastes (e.g., rice husks, wheat straw) [11]. The application of biochar can improve various biological [12] and chemical [10] properties of soils. For example, biochar may stimulate microbial activity in low fertile soils [13] and positively affect the organic matter transformation in soil, resulting in higher available nutrients [14]. Moreover, the addition of biochar reduced nutrient loss during the manure fermentation process [15], as well as improved the chemical parameters and the content of humic substances. The biochar amendment changed the thermodynamics and heat generation during the manure fermentation process [16]. Biochar added to manure increased the manure functional diversity [17], albeit the biochar itself provides numerous benefits to soil, the application of sole biochar did not always result in a positive effect on the soil properties and crop yield. Therefore, its modification by co-composting or mixing it with manure, human feces, food waste, or agricultural residues is recommended [18].
Humic acids (HAs) are ubiquitous organic compounds that can be found in soils, peats, sediments, and low-rank coals. Their positive effect on soil fertility is well known. This impact of HA is ascribed to its ability to solubilize and transport nutrients, bind the contaminants, stimulate plant growth [19], and improve various soil chemical and physical parameters [20,21].
The positive effects of the combined manure–HAs or manure–biochar soil applications have been reported in several studies. Co-applied manure and HA benefit the soil through increasing soil microbial biomass carbon [22], soil aggregation, cation exchange capacity, total carbon, and nitrogen [23]. Biochar addition to manure results in improved humification during the fermentation process [24], and biochar added to the cattle feed provided feces which after fermentation formed biochar enriched- manure having higher availability of N and P when amended to soil [25]. Biochar combined with manure also increased plant biomass yield under water-limited conditions [26,27,28], which suggests the advantage of using combined manure and biochar under currently increasing global water scarcity in agro-ecosystems.
In the present study, we intended to investigate the impact of manure combined with biochar or humic acids on the properties of the produced amendments and evaluate its possible benefits to soil and plants. Manure fermented alone or with biochar or with commercially available humic substances—Humac—was tested for its effect on both the soil physico-chemical and biological properties when applied in the pot experiment with barley (Hordeum vulgare L.). The novelty of our approach lies especially in the use of combined manure—humic substances material for fermentation and as a soil amendment, which, to our knowledge, has not been studied before. We hypothesized that the amendments (manure plus biochar and manure plus humic substances) would: (I) act synergistically and improve both manure and soil properties in comparison to the solely fermented manure; (II) added materials (biochar, Humac) would lead to significant enrichment of manure with nutrients.

2. Materials and Methods

2.1. Fermentation Experiment

The fermentation experiment was carried out using three variants according to mixed materials: (i) manure only (control), (ii) manure mixed with humic substances, i.e., Humac (H), and (iii) manure mixed with biochar (B). The amounts of materials (in kg) used in the variant preparation equaled the soil application doses (t·ha−1) for the plant experiment are defined in Table 1.
All mixtures were prepared in triplicates. Fresh manure was procured from cattle breed farm and biochar produced from agricultural waste (cellulose fibers and cereal husks) at 600 °C (Sonnenerde GmbH, Riedlingsdorf, Austria) as obtained from a commercial manufacturer. According to the manufacturer, the properties of the biochar were as follows (content expressed in dry matter): C 86.6%, N 3.0 g·kg−1, O 10.0 g·kg−1, H 14.2 g·kg−1, Ca 35 g·kg−1; Ash550°C 11.7%, salts 0.42%, pH(CaCl2) 8.5, BET 288.5 m2·g−1. Humac named (AGRO soil fertility stimulator), originally derived from leonardite-oxyhumolite, composed of (dry matter ≥ 85%; free HA ≥ 50%; C 38.4%, O 18.6%, N 3.1%, Na 1.5%, Ca 1.5%, Fe 1.6%, K 1.1%, Zn 64 mg·kg−1, B 77 mg·kg−1, Cu 19 mg·kg−1, Se 1.67 mg·kg−1, all in dry matter; pH 6.5 (Envi Produkt Ltd., Prague, Czech Republic).
In amended manure variants, the manure and additives (Humac or biochar) were thoroughly mixed by intensive mixing in the 50 L-barrels. The barrels were tightly covered, and fermentation process was carried out for 58 days at stable temperature 22.2–25.2 °C and relative humidity 60–78%. The flow of air was not controlled but was limited due to the covering. At the end of the fermentation process, samples were collected from each barrel and analyzed for dry matter (DM), pH (measured in CaCl2 suspension), organic carbon (Corg), total nitrogen (N), ammonium nitrogen (N-NH4, determined according to [29], phosphate (P), potassium (K), calcium (Ca), magnesium (Mg), boron (B), humic:fulvic acid ratio (HA:FA), ammonium-oxidizing bacteria (AOB), denitrifying microorganisms (nirS) (results in Section 3.1).

2.2. Sampling of Biosolids, Chemical and Microbiological Properties

Manure was dried to the constant weight at 60 °C and sieved through a 0.15-mm mesh prior to analyses. DM was estimated gravimetrically. The pH (in CaCl2 extract from fresh manure) was measured according to ISO 10390: 2005 [30]. Corg was measured by dry combustion method [31]. Phosphorous (P) was estimated by following the protocol of [32]. Nitrogen (N) composition of biochar was determined using LECO TruSpec analyzer (MI USA). Elemental composition was determined according to standardized method [33]. HA:FA ratio was determined from the contents measured according to [34]. Samples for determination of AOB and nirS by qPCR were freeze-dried and sieved through a 0.15-mm mesh. DNA was extracted from 0.2 g of freeze-dried sample using the E.Z.N.A.® Soil DNA Kit (Omega Bio-tek, Norcross, GA, USA). The SYBR-Green platform was used on a CFX96 Real-Time PCR detection system (Bio-Rad Laboratories, Hercules, CA, USA). AOB were quantified according to the protocol of Rotthauwe et al. [35], nirS (nitrate reductase gene copies) were quantified according to the method developed by Kandeler et al. [36].

2.3. Pot Experiment and Design

The pot experiment with barley (Hordeum vulgare L.) as a test crop was performed. The 5-L pots—top diameter 22 cm, base diameter 17 cm, height 18 cm—were used. First, the pots were filled up with 5 kg of a soil-sand mixture (1:1), where fine quartz sand (0.1–1.0 mm) was mixed with sieved (2.0 mm) topsoil collected from the rural area near the town Troubsko (Czech Republic–49°10′28″ N 16°29′32″ E). The soil was silty clay loam (according to USDA Textural Soil Classification), Haplic luvisol (according to the WRB Soil Classification—FAO [37], its properties are shown in (Table 2). Selected pots were further amended with fermented manure or enriched manures with Humac or biochar.
The following treatments were used (i) the unamended soil (soil control), and three variants of soil amended with (ii) fermented manure (control, M), (iii) manure enriched with Humac (M + H), and (iv) manure enriched with biochar (M + B). The amendment dose was 165 g·pot−1 (with equaled 50-tonne biosolid·ha−1). Each variant (except for the soil control) was amended with a mixed manure variant () and prepared in four replicates. Each pot was watered with distilled water to 65% WHC (which was maintained throughout the experiment), and 16 barley seeds were sown in each pot. After 2 weeks, the number of plants in the pots was reduced to 13. The experiment was carried out for 12 weeks in a growth chamber (CLF Plant Climatics GmbH, Germany) under controlled conditions (day/night): temperature (20/12 °C), relative air humidity (45/70%), photoperiod (12/12 h), light intensity of 370 µmoL·m−2·s−1.

2.4. Soil Sampling, Physico-Chemical, and Enzymatic Analyses

At the end of the experiment, the above-ground plant biomass was harvested at the ground level, dried at 60 °C to constant weight, and reported as dry AGB. The substrate from each pot was homogenized by sieving it through 2 mm mesh under sterile conditions and sampled for further analysis. Air dried soil samples were analyzed for physico-chemical properties, i.e., pH [30], total soil C (TC) [31], total soil N (TN) [38]. Freeze-dried samples were used for the analyses of enzymatic activities: β-glucosidase (GLU), arylsulfatase (ARS), phosphatase (Phos), urease (Ure), N-acetyl-β-d-glucosaminidase (NAG) [39]. The samples stored at 4 °C were used for determination of dehydrogenase activity (DHA) following Casida et al. (1964) [40], soil basal respiration (BR) and substrate-induced respiration (SIR)—d-glucose (Glc-SIR), citric acid (Cit-SIR), d-trehalose (Tre-SIR), N-acetyl-β-d-glucosamine (NAG-SIR), l-alanine (Ala-SIR), l-lysine (Lys-SIR), or l-arginine (Arg-SIR) [41].

2.5. Statistical Analyses

Data obtained from the physico-chemical and biological measurements were statistically analyzed using the multivariate analysis of variance (MANOVA), principal component analysis (PCA), one-way analysis of variance (ANOVA), Tukey HSD post hoc test (at significance level p = 0.05), and Pearson correlation analysis (Program R, version 3.6.1).
The results of Pearson’s correlation analysis were interpreted as follows: 0.5 < r < 0.7 (moderate correlation) and 0.7 < r < 0.9 (high correlation) [42].

3. Results

3.1. Effect of Amendments on Manure Maturation

The results revealed that all three variants differed significantly from each other in terms of physical, chemical, and biological characteristics (Table 3).
The differences between the M + H variant and the other two variants (as depicted in Figure 3A) can be seen, e.g., the pH was higher for the M + H variant compared to the M + B variant and the M variant (Table 3). The pH correlated significantly positively with nirS (r = 0.82) and negatively with Corg and AOB (r = −0.82 and −0.81, respectively (Figure 2A). DM also significantly differed between the variants and patterned as follows: M < M + H < M + B (Table 3). The Corg was significantly lower in the M + H in comparison to M and M + B (Table 3). Corg significantly negatively correlated with HA:FA (r = −0.7) and nirS (r = −0.75) (Figure 2A). The total N was similar across the variants.
Similarly to N contents, the content of available P was comparable among the variants where the exact measured values decreased in the following order: M > M + H > M + B (Table 3). P content was moderately positively correlated with N-NH4 (r = 0.54). The N-NH4 content significantly decreased in both M + H and M + B variants as compared to the M variant. Both the K and Mg contents in M + B were significantly lower as compared to M and M + H. The PCA biplot and Pearson’s correlation analyses revealed that K and Mg (positively intercorrelated) significantly negatively correlated with calcium (Ca) and boron (B) (positively intercorrelated) (Figure 1 and Figure 2). Due to the higher Ca content in biochar, the resulting content of Ca in M + B was significantly increased as compared to the two other variants. The Ca content correlated moderately positively with total N (r = 0.69) and negatively with N-NH4 (r = −0.71) (Figure 2A). In our study, boron contents were similar across the variants. The HA:FA ratio was not affected by biochar addition while significantly increased in the M + H variant. The HA:FA correlated moderately positively with nirS (r = 0.73) and K (r = 0.66), and negatively with Corg (r = −0.7) and AOB (r = −0.87) (Figure 2A).
The AOB was significantly lower in M + H as compared to the other two variants, and the PCA biplot and Pearson’s correlation found an antagonism and negative correlation of AOB with nirS (r = −0.74) (Figure 2A and Figure 3A). The nirS values significantly differed among the treatments, where it was the highest for M + H and the lowest for the M variant.

3.2. Effect of Manure and Amendments on Soil Respiration

The results revealed a significant (p ≤ 0.05) increase in basal respiration (BR) in manure amended variants in comparison to control (Figure 1C). The combined addition of M + H and M + B had the most profound effect on the BR of soil. This positive role of the carbon-rich amendments on soil microbial activity was further supported by the observed moderate positive correlation between BR and the TC (r = 0.67) (Figure 2B). The moderate positive correlation between BR and sugars-induced SIR (Glc-SIR—r = 0.54, Tre-SIR—r = 0.6, NAG-SIR—r = 0.62) and amino acid-induced SIR (Lys-SIR—r = 0.6, Arg-SIR—r = 0.55) further corroborates the community-broad positive effect on microbial respiration arising from single (M) or combined applications (M + H or M + B) when compared to control (Figure 2B). However, there were differences between the results of the various SIR assays (i.e., Glc-SIR versus Ala-SIR and Arg-SIR) for the M, M + H, and M + B variants, which implies functionally diverse microbiomes in these treatments. The M + B variant showed the highest values in several SIR assays, including Glc-SIR, Tre-SIR, NAG-SIR, and Lys-SIR. (Figure 1D–J).

3.3. Effect of Manure and Amendments on Soil Nutrient Cycling and or Enzymatic Activities

Transformation of nutrients in the test soil was affected by the activities of the microbial biomass in the respective experimental variants, which could be documented by, e.g., the agonistic relationship and the moderate positive correlation between DHA and TC (r = 0.48) and between DHA and the TN content (r = 0.47) (Figure 2B). Further, a positive correlation between DHA and GLU (r = 0.45) and between DHA and Ure (r = 0.60) was observed (Figure 2B). DHA was found to be significantly increased due to amending the soil with manure (by 35, 63, and 53% on average for M, M + H, and M + B variants, respectively). The manure amendment in soil-stimulated mineralization of soil Corg is evidenced by the significantly higher DHA in all manure-treated soils as compared to control.
The variants amended with enriched manure (M + H and M + B) showed significantly higher GLU values by 31% and 12%, respectively, on average compared to control soil. The highest and significantly different (as compared to the control and M variant) value of GLU was measured in the M + H soil (Figure 1O). NAG value significantly higher than in control (and M variant) was reported for the M + B treatment by 13%, compared to control—(Figure 1N). The PCA biplot showed a clear convergence of GLU with Phos as well as NAG with Ure (Figure 3B).
The activity of Ure was higher in the manure-based variants by 61 and 48% for M + H and M + B, respectively, when compared to the control (Figure 1L). Apart from moderate positive correlation with DHA (r = 0.60), the Ure activity correlated also with NAG-SIR (r = 0.46), Ala-SIR (r = 0.50), and dry AGB (r = 0.53) (Figure 2B and Figure 3B).
Relative to control, the activity of Phos significantly increased only in the M + H variant (Figure 1M) and showed a significant correlation with Ure (r = 0.35) and with GLU (r = 0.41) (Figure 2B). On the contrary, ARS activity significantly decreased following the addition of all manures to the soil, especially of M, by 29% on average (Figure 1K). ARS activities in the M + H and M + B variants were comparable. The PCA biplot revealed antagonism between ARS activities and the results of the SIR assays (except Cit-SIR) (Figure 3B).

3.4. Effect of Manure and Amendments on Soil Physico-Chemical Properties and Plant Biomass

The pH values significantly differed between the tested variants. The control treatment and M + B showed significantly lower values than the soil in M + H treatment (Figure 1A). The pH values moderately positively correlated with dry AGB (r = 0.55), that increased (compared to the control) in soil when amended with manure (+62%, in average), M + B (+43%) and especially with M + H (+95%, Figure 1S). Dry AGB was further positively correlated with the soil TC and TN content (r = 0.52 and 0.30, respectively) in the test variants. The TC content (Figure 1P) was significantly higher compared to control (by 9%, 15%, and 17%) in all manure-based variants (M, M + H, and M + B, respectively). The PCA biplot indicated TC agonisms with BR and enzyme activities (i.e., DHA, NAG, Ure) (Figure 3B).
The soil TN content (Figure 1P) was significantly higher (by 13%, 21%, 18%) in all manure-based variants (M, M + H, M + B, respectively) as compared to control). Significantly positively correlated with TC (r = 0.79) and moderately negatively correlated with C:N (r = −0.61) (Figure 1R,S and Figure 2B). No significant difference was found in C:N among the variants; however, high average values of C:N in the control and M + B variants were in contrast to the low average values of AGB dry (Figure 1R,S).

4. Discussion

4.1. Effect of Amendments on Manure Maturation

Manure maturation is connected with the activity of various groups of microorganisms, especially bacteria, fungi, and actinomycetes. The intensity of these processes is determined by the access of air, ambient humidity, and temperature, which were kept the same in all cases in the present study. With access to air, the decomposition of organic substances proceeds much faster than in anaerobic conditions, and there are large losses of organic matter and especially nitrogen, which is rapidly lost as ammonia. With limited air access (mild anaerobiosis conducted in this work), organic matter is only partially degraded from manure, and more methane would have formed, which prevents the decomposition of organic matter into carbon dioxide, water, and ammonia [43].
As expected, the DM content of the enriched manure was influenced by Humac and Biochar enrichment, which was given by the vast difference between the DM of manure (~30.0%), Humac (≥85%, added in 1% w/w), and biochar (≥65%, added in 4% w/w). Despite our initial expectations, the alkaline nature of biochar (pH = 9.6) did not significantly impact the resulting pH of the M + B mixture compared to the M variant, which can be attributed to the type and amount of used biochar. On the contrary, Humac addition in M + H variant caused a significant increase in pH when compared to the unamended manure (M). The negative correlation of pH with Corg and AOB implied that microbial mineralization processes took place and affected the pH of the mixtures. We assume that the available Corg and N-NH4 in the M + B variant were aerobically (or partially anaerobically) oxidized, which putatively lead to Ca precipitation, similarly as it occurred in broiler litter due to urea hydrolysis as reported previously by Burt et al. [44]. Concurrently, increased ammonia oxidation might have decreased the pH and caused decreased N-NH4 content.
With biochar (86.6% C, dry weight) and Humac (38.4% C d. w.), a significant portion of fresh C was introduced to the manure, yet the Corg content in the matured M + H mixture was lower when compared to M and the M + B variants. We assume that Corg-rich amendments (M + H, M + B) facilitated decomposition and humification as reported previously [45]. A high amount of HAs was added to the M + H mixture as well. However, we presumed that humic acid-derived carbon underwent intensified mineralization due to the higher solubility of humic acid under increased pH as referred by [46] and concurrently increased vulnerability to auto-oxidation [47]. Another study by [48] reported that increased carbon oxidation (prevailing in M + B and M + H, in contrast to M) was coupled with higher denitrification because this may be caused by depletion in oxygen availability. Moreover, Paul and Beauchamp, and Dlamini et al. [49,50], also reported that water-soluble C, VFA, or particular carbon sources in manure might promote denitrification. The findings by Sarkhot et al. [51] suggested that biochar can stabilize the various forms of N in manure via various adsorption mechanisms. Agyarko-Mintah et al. [52], in another study, reported increased N retention during manure composting, while N-NH4 was decreased during the maturation phase. Yet, our data implied that the addition of biochar to manure did not affect the total N contents that were found to be similar across the various treatments at the end of the maturation experiment. Similarly, we did not observe significant changes in the P contents as a result of the addition of either Humac or biochar to manure before its maturation, and therefore we cannot corroborate the results of previous studies [53,54] suggesting that organic matter contributes to P stabilization.
The contents of K and Mg in the M + B variant were lower, whereas the content of Ca was higher when compared to the other variants (Table 3). These trends were fully in line with the composition of biochar that was less rich in K and Mg while richer in the Ca when compared to manure (Table 3).
The addition of Humac, as a material rich in humic acids (≥50%), resulted in a higher HA:FA ratio when compared to other variants. Additionally, we assume that fulvic acid formation was further promoted in the M + H variant via increased degradation (mineralization) of the organic matter (as evidenced by the lowest Corg content). These findings were further supported by the observed antagonism of AOB and HA:FA as shown by PCA biplot (Figure 3A), which further corroborates the role of fulvic acids in anaerobic ammonium oxidation and carbon mineralization. Similarly, it was evidenced by Liu et al. [55], who found out that the addition of FA into denitrifying bacterial culture resulted in FA-accelerated metabolism of carbon source.
The highest pH and HA:FA ratio, promoting denitrification, and lower available N-NH4 (compared to the fermented manure) in the M + H variant (Table 3) were critical parameters for the lowest abundance of AOB in this treatment. On the other hand, the same critical traits (pH, HA:FA), which limited the numbers of AOB, anticipated the increased abundance of denitrifying microorganisms (determined as nirS) in the M + H as compared to the other two tested variants.

4.2. Effect of Manure and Amendments on Soil Respiration

In previous works, it has been reported that both the single application of manure and combined with biochar can stimulate soil respiration [56]. The addition of compost or manure enriched with humic acids also increased soil microbial biomass [23,45]. In contrast, the single application of Humac to soil resulted in decreased BR [57]. In our study, the application of all manure types significantly increased BR as compared to the control soil.
Despite the significant differences observed between the results of the SIR assays for the tested treatments, the overall schematic representation of the mutual relationships by PCA biplot (Figure 3B) showed clear agonisms (and convergence with BR) among all SIRs. The results of Pearson’s correlation analysis support this observation (Figure 2B).
All manure-amended variants revealed increased respiration, which corresponds to previous findings [58]. It can be deduced from the results of all determined SIRs that the amendment of biochar-enriched manure promoted microbial activity in the soil, as compared to the control (Figure 3D–J). Respiration measured upon the addition of saccharides (d-glucose, d-trehalose) showed significantly increased values in M + B and significantly decreased Tre-SIR in M + H as compared to the other two manure-amended variants. Presumably, lower Corg in M + H manure together with higher pH (Table 3) less efficiently stimulated the oxidation of primary C-sources. Some N-containing substrates (N-acetyl-β-d-glucosamine, L-lysine) led to significantly higher SIR in M + B variant when compared to the M, which implies that M + B more promoted the microbial nitrifying degraders of fungal biomass (NAG is the degradation derivate of chitin). These observations are in line with our previous findings on the increased fungal abundance and higher turnover of fungal biomass, which was reported for the M + B treated soil [59].
In contrast, the M + H treatment had a negative effect on SIR in comparison to the soil amended with M + B. As such, we could not confirm that the combined addition M + H was beneficial for soil as previously observed by [23]. The detailed evaluation of the soil basal and induced respiratory traits determined in our study revealed that the most beneficial impact on soil in terms of respiration arose from the application of manure amended with biochar, which was most likely achieved via the stimulation of fungal biomass and through the enrichment of soil with C and N, and enhanced C and N mineralization [57].

4.3. Effect of Manure and Amendments on Soil Nutrient Cycling and or Enzymatic Activities

The amendment of soil with manure (alone or in combination) apparently stimulated mineralization of soil Corg as evidenced by the significantly higher DHA in the M, M + H, and M + B variants when compared to the control (Figure 1B). The M + H variant showed the highest DHA, likely because it received the highest portion of the readily available Corg [23,60].
Moreover, the M + H variant was assumed to exert the most advanced cellulose decomposition among the manure types, which preceded increased GLU. We ascribed this from the highest HA:FA ratio as a degradation process evolution indicator in the M + H manure (Table 3). It was referred that GLU and cellulolytic microbiological functional groups were strongly correlated with the production of fulvic and humic acids [61].
We further revealed significantly increased (compared to the control) NAG in the M + B variant, which is in line with Zhang et al. [62] and implies higher fungal abundance and its turnover in soil. Moreover, NAG is an indicator of N mineralization and nitrification, together with Ure. The Ure activity was significantly enhanced in all manure amended variants. However, the M + H variant reached the highest value. These results suggest that M + H addition to soil increased available and microbial N, which is in line with previous findings [23,60].
On the other hand, ARS was significantly lower in all manure-based variants as compared to the control. Therefore, the addition of manure appeared to have a rather negative effect on ARS activity, similarly to the MSW (municipal sewage water) compost that negatively impacted the activity of ARS [63]. However, the enriched manures (M + H and M + B) showed significantly higher values of ARS than the M variant.
The soil phosphatase was significantly increased (as compared to the control) only in the M + H variant, implying a positive role of Humac on P mineralization by hydrolysis of organophosphates [64]. This is in line with another study reporting that the solubility of phosphates was positively related to the humic acid content in the compost [65].

4.4. Effect of Manure and Amendments on Physico-Chemical Properties of Soil and Plant Biomass

The soil pH is controlled and driven by a number of various processes and parameters, including the composition of the soil, minerals, and soil microbial properties. In our study, only the application of M + H significantly increased the soil pH (Figure 1A). On the other hand, TC contents in soil were significantly changed with the addition of C-rich materials (M, M + H, or M + B) when compared to the control soil. The highest value was reached in M + B variant. Moreover, the Pearson correlation analysis also revealed significant positive correlations (with r values of 0.48–0.57) between Glc-SIR, NAG-SIR, Arg-SIR, and the TC content. These findings corroborate the beneficial effects of manure-based amendments on the TC content that was higher in treated (M, M + H, M + B) variants in comparison to control (Figure 1Q), and M + B reached significantly higher values than M. The manure-induced microbial soil activity was putatively mediated by higher nutrient availability. We ascribed this presumption from the reported observation that soil respiration was principally determined by substrate supply (which contains nutrients) rather than by the pool size of microbial biomass carbon [66]. The authors of mentioned study referred as well to specific microbial respiratory activity positively correlated with substrate (and thus nutrient) availability.
The high correlation of TN with TC (r = 0.92) documented the general increase in the availability of macronutrients in the soil treated with manure. In addition, higher TN content in the M, M + H, and M + B treatments led to the increased plant biomass in these treatments when compared to unamended soil, which corresponds with the previously reported beneficial effects of manure and organic matter co-application on soil fertility and plant growth [23,60,67,68,69]. On the other hand, the soil TN content moderately negatively correlated with C:N (r = −0.61). Therefore, we presumed higher rate of both C and N sequestration, and moderate nitrification (low C:N ratio is assumed to cause rapid release of N into the soil in the form of inorganic N compounds such as nitrates) in the variants, which concurrently exerted the higher TC and dry AGB.

5. Conclusions

The results suggested that all matured (fermented and enriched) manures differed in their physico-chemical characteristics, microbial composition, and nutrient contents as compared to the control. In the pot experiment, the soil respiration increased due to soil amendment with either manure or enriched manures. The activities of enzymes related to N and P mineralization (urease, N-acetyl-β-d-glucosaminidase, phosphatase) were enhanced in M + H and M + B variants. However, some parameters, such as arylsulfatase, decreased due to added manures. Altogether, there were several indices of the beneficial effects of enriched manures, which also translated into apparently increased plant dry biomass, especially in the case of the M + H variant. Following our results, we may conclude that amending manure with biochar and humic acids before maturation may provide several benefits, induce positive changes in soil when applied, and ultimately support soil fertility and plant growth. However, in order to maximize the assumed synergic effects, the role of biochar and humic substances for the quality of manure and soil needs to be further studied.

Author Contributions

Conceptualization, T.H., J.H. and M.B.; methodology, T.H., J.H. and M.B.; software, T.H., T.B.; validation, M.B., T.H. and J.K.; formal analysis, O.L., T.B.; investigation, J.H., J.K., A.M. and M.B.; resources, O.L., M.R. and A.K.; data curation, T.H., M.R. and O.L.; writing—original draft preparation, T.H., L.B., J.H.; writing—review and editing, T.H., J.H., L.B., J.K., A.M. and M.B.; visualization, T.H. and A.K.; supervision, M.R., M.B.; project administration, M.B., A.K.; funding acquisition, M.B., A.K. All authors have read and agreed to the published version of the manuscript.

Funding

The work was supported by the project of the Technology Agency of the Czech Republic TH03030319, and by the Ministry of Education, Youth and Sports of the Czech Republic, grant number FCH-S-21-7398.

Data Availability Statement

The data presented in this study are available on request from the corresponding author.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Results of the pot experiment with four tested variants, i.e., soil (control), soil amended with manure (M), soil amended with manure and Humac (M + H), and soil amended with manure and biochar (M + B). The measured parameters were as follows: (A) soil reaction = pH [-], (B) dehydrogenase activity [µg TPF·g−1·h−1], (C) basal respiration [μg CO2·g−1·h−1], (D) d-glucose SIR [μg CO2·g−1·h−1], (E) citric acid SIR [μg CO2·g−1·h−1], (F) d-trehalose SIR, (G) N-acetyl- β -d-glucosamine SIR [μg CO2·g−1·h−1], (H) l-alanine SIR [μg CO2·g−1·h−1], (I) L-lysine SIR [μg CO2·g−1·h−1], (J) l-arginine SIR [μg CO2·g−1·h−1], (K) arylsulfatase [nmol·g−1·min−1], (L) urease [nmol·g−1·min−1], (M) phosphatase [nmol·g−1·min−1], (N) N-acetyl- β -d-glucosaminidase [nmol·g−1·min−1], (O) β-glucosidase [nmol·g−1·min−1], (P) total soil nitrogen [%], (Q) total soil carbon [%], (R) C:N ratio [-], (S) dry plant aboveground biomass [g]. Different letters indicate differences between the values at the statistical level of significance p ≤ 0.05.
Figure 1. Results of the pot experiment with four tested variants, i.e., soil (control), soil amended with manure (M), soil amended with manure and Humac (M + H), and soil amended with manure and biochar (M + B). The measured parameters were as follows: (A) soil reaction = pH [-], (B) dehydrogenase activity [µg TPF·g−1·h−1], (C) basal respiration [μg CO2·g−1·h−1], (D) d-glucose SIR [μg CO2·g−1·h−1], (E) citric acid SIR [μg CO2·g−1·h−1], (F) d-trehalose SIR, (G) N-acetyl- β -d-glucosamine SIR [μg CO2·g−1·h−1], (H) l-alanine SIR [μg CO2·g−1·h−1], (I) L-lysine SIR [μg CO2·g−1·h−1], (J) l-arginine SIR [μg CO2·g−1·h−1], (K) arylsulfatase [nmol·g−1·min−1], (L) urease [nmol·g−1·min−1], (M) phosphatase [nmol·g−1·min−1], (N) N-acetyl- β -d-glucosaminidase [nmol·g−1·min−1], (O) β-glucosidase [nmol·g−1·min−1], (P) total soil nitrogen [%], (Q) total soil carbon [%], (R) C:N ratio [-], (S) dry plant aboveground biomass [g]. Different letters indicate differences between the values at the statistical level of significance p ≤ 0.05.
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Figure 2. The Pearson’s correlation matrix of the maturated manure properties (A), soil, and plant properties (B). Explanation: . Significant at 0.10 level; * Significant at 0.05 level; ** Significant at 0.01 level; *** Significant at 0.001 level.
Figure 2. The Pearson’s correlation matrix of the maturated manure properties (A), soil, and plant properties (B). Explanation: . Significant at 0.10 level; * Significant at 0.05 level; ** Significant at 0.01 level; *** Significant at 0.001 level.
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Figure 3. The PCA biplot of the maturated manure properties (A), soil and plant properties (B). (A) M = fermented manure, M + H = manure + Humac, M + B = manure + biochar; (B) control = control soil, M = soil amended with fermented manure; M + H = soil amended with manure + Humac, M + B = soil amended with manure + biochar.
Figure 3. The PCA biplot of the maturated manure properties (A), soil and plant properties (B). (A) M = fermented manure, M + H = manure + Humac, M + B = manure + biochar; (B) control = control soil, M = soil amended with fermented manure; M + H = soil amended with manure + Humac, M + B = soil amended with manure + biochar.
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Table 1. Variants of the fermentation experiment.
Table 1. Variants of the fermentation experiment.
VariantManure
[t·ha−1]
Biochar
[t·ha−1]
Humac
[t·ha−1]
Manure
[kg·Barrel−1]
Biochar
[kg·Barrel−1]
Humac
[kg·Barrel−1]
Control50001000
Humac (H)5000.51000.1
Biochar (B)5020100.40
Table 2. Properties of soil used in the pot experiment.
Table 2. Properties of soil used in the pot experiment.
pHTN [%]TC [%]C:NNmin [mg·kg−1]N-NO3 [mg·kg−1]N-NH4 [mg·kg−1]
7.290.161.408.7762.8456.806.04
H [%]S [%]K [mg·kg−1]Ca [mg·kg−1]Mg [mg·kg−1]P [mg·kg−1]
0.580.01231325923697
TN = soil total nitrogen, TC = soil total carbon, C:N = soil total carbon/total nitrogen ratio, Nmin = mineral nitrogen, N-NO3 nitrate nitrogen, N-NH4 = ammonium nitrogen, H = soil hydrogen, S = soil sulphur, K = soil potassium, Ca = soil calcium, Mg = soil magnesium, P = soil phsphorus.
Table 3. Properties of the maturated manure variants (mean ± standard deviation, n = 3, * statistically significant difference at p ≤ 0.05).
Table 3. Properties of the maturated manure variants (mean ± standard deviation, n = 3, * statistically significant difference at p ≤ 0.05).
MM + HM + B
Mean ± SD *Mean ± SD *Mean ± SD *
DM [%]30.01 ± 0.02 c31.22 ± 0.02 b31.48 ± 0.02 a
pH [-]9.04 ± 0.01 b9.25 ± 0.01 a9.05 ± 0.01 b
Corg [%]13.50 ± 0.28 a12.45 ± 0.36 b13.01 ± 0.14 a
N [%]2.48 ± 0.05 a2.49 ± 0.05 a2.54 ± 0.03 a
N-NH4 [mg·kg−1]2.06 ± 0.02 a1.56 ± 0.04 b1.44 ± 0.08 c
P [%]4.22 ± 0.36 a3.58 ± 0.58 a3.45 ± 0.64 a
K [g·kg−1]84.36 ± 5.21 a87.57 ± 3.87 a67.03 ± 2.62 b
Mg [g·kg−1]9.61 ± 0.50 a9.30 ± 0.15 a7.34 ± 0.18 b
Ca [g·kg−1]20.93 ± 0.88 b22.68 ± 0.88 b32.95 ± 1.96 a
B [mg·kg−1]47.20 ± 1.11 a43.78 ± 2.49 a54.53 ± 9.35 a
HA:FA [-]0.79 ± 0.01 b1.20 ± 0.07 a0.69 ± 0.03 c
AOB [copies·g−1]2.11·108 ± 2.63·107 a1.01·108 ± 1.38·107 b2.09·108 ± 3.63·106 a
nirS [copies·g−1]1.07·109 ± 1.59·108 c1.87·109 ± 2.38·108 a1.40·109 ± 1.69·108 b
M; manure, M + H; manure + Humac, M + B; manure + biochar. SD = standard deviation. Letters indicate differences between the values at the statistical level of significance p ≤ 0.05.
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Holatko, J.; Bielska, L.; Hammerschmiedt, T.; Kucerik, J.; Mustafa, A.; Radziemska, M.; Kintl, A.; Baltazar, T.; Latal, O.; Brtnicky, M. Cattle Manure Fermented with Biochar and Humic Substances Improve the Crop Biomass, Microbiological Properties and Nutrient Status of Soil. Agronomy 2022, 12, 368. https://doi.org/10.3390/agronomy12020368

AMA Style

Holatko J, Bielska L, Hammerschmiedt T, Kucerik J, Mustafa A, Radziemska M, Kintl A, Baltazar T, Latal O, Brtnicky M. Cattle Manure Fermented with Biochar and Humic Substances Improve the Crop Biomass, Microbiological Properties and Nutrient Status of Soil. Agronomy. 2022; 12(2):368. https://doi.org/10.3390/agronomy12020368

Chicago/Turabian Style

Holatko, Jiri, Lucie Bielska, Tereza Hammerschmiedt, Jiri Kucerik, Adnan Mustafa, Maja Radziemska, Antonin Kintl, Tivadar Baltazar, Oldrich Latal, and Martin Brtnicky. 2022. "Cattle Manure Fermented with Biochar and Humic Substances Improve the Crop Biomass, Microbiological Properties and Nutrient Status of Soil" Agronomy 12, no. 2: 368. https://doi.org/10.3390/agronomy12020368

APA Style

Holatko, J., Bielska, L., Hammerschmiedt, T., Kucerik, J., Mustafa, A., Radziemska, M., Kintl, A., Baltazar, T., Latal, O., & Brtnicky, M. (2022). Cattle Manure Fermented with Biochar and Humic Substances Improve the Crop Biomass, Microbiological Properties and Nutrient Status of Soil. Agronomy, 12(2), 368. https://doi.org/10.3390/agronomy12020368

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