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1.
Bacteriophages (phages) are the most abundant biological entities on the planet and are important as the greatest genomic reservoirs in both marine and terrestrial environments. In this study, we analysed T4-type phage communities in an upland black soil by monitoring g23 clones in DNA extracted from seasonal soil samples with no fertilizer, chemical fertilizers, chemical fertilizers plus manure, and natural restoration treatments. PCR products with degenerate primers MZIA1bis and MZIA6 were subjected to denaturing gradient gel electrophoresis. In total, 46 clones with different g23 sequences were obtained. Phylogenetic analyses indicated that T4-type phage communities in the upland black soil were distinctly different from those in marine environments and in an Antarctic lake, which strongly suggested that T4-type phage communities in soil differed from those in aquatic environments. Among 46 clones, 18 clones formed clusters with the clones from rice field soils, 14 clones formed three new clusters, and 13 clones were left as ungrouped, which indicated that T4-type phage communities in the upland black soil were relatively similar to those in rice field soils but that specific communities also inhabit in the upland black soil exclusively.  相似文献   

2.
Many studies have shown the ecological importance of viruses as the greatest genomic reservoirs on the planet. As bacteriophages (phages) comprise the majority of viruses in the environment, we surveyed the capsid genes (g23) of T4-type phages, Myoviridae, from DNA extracts of three paddy field soils located in northern, central and southern Japan using the degenerate primers MZIA1bis and MZIA6. Denaturing gradient gel electrophoresis (DGGE) was performed to separate PCR-amplified g23 products, and 56 DGGE bands were identified as g23 fragments. Only nine clones were grouped into T-evens, PseudoT-evens and ExoT-evens, and most of the other clones were classified into Paddy Groups I-VI. No significantly different distribution of g23 clones was observed among the paddy fields at the group level, indicating that phage communities estimated from the g23 composition were common on the nationwide level. Comparison of g23 sequences showed that g23 genes in paddy fields were different from those in marine environments, and more divergence of g23 genes was estimated in the paddy fields compared to the marine environment. Two novel g23 clones with very short amino acid residues were detected, suggesting the existence of uncharacterized, novel groups of g23 genes in paddy field soils.  相似文献   

3.
Our previous study revealed the high diversity of the major capsid gene (g23) of T4-type phages that existed in the paddy field soils in Northeast China. In this study, the phylogeny and genetic diversity of the g23 gene in the paddy floodwater samples collected from five sampling sites at three sampling times during the rice (Oryza sativa L.) growth season in Northeast China are reported. In total, 104 different g23 clones were isolated, among which 50% of the clones exhibited the highest identities with the clones retrieved in paddy soils and upland black soils. The remaining clones had the highest identities with lake origins. Phylogenetic analysis revealed that 43% of the g23 clones grouped into three novel subgroups which included the clones unique to paddy floodwater, and no g23 sequences obtained in paddy floodwater fell into the paddy soil groups II, III, IV, V, VI, VII and NPC-A. UniFrac analysis of g23 clone assemblages demonstrated that T4-type phage communities in paddy floodwater were changed spatially and temporally, and the communities were different from those in paddy soils. Further comparison of the g23 clone assemblages from different environments demonstrated that T4-type phages were biogeographically distributed, and the distribution was both affected by geographical separation and ecological processes across the biomes.  相似文献   

4.
The present study compared the capsid gene ( g23 ) of T4-type bacteriophages (phages) in Mn nodules with those in the plow layer soil and subsoils of two Japanese paddy fields by applying the primers MZIA1bis and MZIA6 to DNA extracts from the nodules and soils. The deduced amino acid sequences of the g23 genes in the Mn nodules were similar to those in the plow layer soil and in the subsoils. This result indicated that similar T4-type phage communities developed at these sites and that the diversity of T4-type phage communities was wide enough to cover those in the plow layer soil and in the subsoils. The majority of g23 clones formed several clusters with the clones and phages obtained from far-apart paddy fields, and the sequences of two clones were completely identical to a phage and a clone from other paddy fields at the nucleotide or amino acid level, indicating horizontal transfer of g23 genes between those paddy fields. A clone with a long nucleotide residue (686 bp) and a distribution remote from the other clones in the phylogenetic tree indicated that there were many uncharacterized, novel g23 genes in the paddy fields.  相似文献   

5.
Our previous study indicated that the diversity of the major capsid gene (g23) of T4-type bacteriophages (phages) of Novosphingobium and Sphingomonas strains isolated from the floodwater of a Japanese paddy field is comparable to those of the clones obtained from other Japanese paddy fields. For more strict comparison of the diversity, this study examined g23 sequences between Novosphingobium and Sphingomonas phages and phage communities in the identical floodwater of a Japanese paddy field. The clones were obtained by applying g23-specific primers to DNA extracted from the floodwaters. Many 23 clones in the floodwater were grouped into the same clusters of Paddy Groups I-VI with g23 genes of Novosphingobium/Sphingomonas phages with some clones belonging to an additional cluster. In addition, the remaining clones belonged to the clusters of marine clones and T4-type enterophages. These findings indicate that the g23 genes in the floodwater are more diversified than those of Novosphingobium/Sphingomonas phages including g23 genes closely related to the genes of enterophages and marine origins.  相似文献   

6.
We surveyed the capsid genes (g23) of T4-type bacteriophages in DNA extracted from fifteen rice field soils in Northeast China using primers MZIA1bis and MZIA6. Denaturing gradient gel electrophoresis (DGGE) was performed to separate PCR-amplified g23 products. In total, 53 DGGE bands were identified as g23 clones, nine of which belonged to a novel, Northeast China-specific group. In addition, four and six clones formed two novel groups with previously ungrouped clones obtained from Japanese rice fields. The majority of the remaining clones fell into Paddy Groups I and V, none of the clones belonged to Paddy Groups II, III, IV, and VI, indicating that phylogenetic distribution of g23 genes in rice fields in Northeast China was different from that in Japanese rice fields.  相似文献   

7.
Although microbial communities in soil are well known to change with soil depth, the changes in viral communities with soil depth have not been documented. This study examined the soil depth profiles of T4-type phage communities in two Japanese rice fields from g23 clones in soil DNA extracts to a depth of 1 m. T4-type phage communities changed with soil depth, and the communities were grouped into two groups: the communities of the surface soil layers, where rice roots developed densely, and those of the subsoil layers. Although coarse- and fine-textured soils were stratified in the subsoil layers in both profiles, denaturing gradient gel electrophoresis band patterns and phylogenetic affiliation of g23 were highly similar to each other among the subsoil layers in both fields, indicating that soil texture did not affect T4-type phage communities in these fields. In addition, some clones had g23 sequences identical to those retrieved from rice fields in Northeast China, indicating that closely related viruses and their hosts distribute across the sea between rice fields in Japan and Northeast China.  相似文献   

8.
Viruses exist everywhere on the planet. Recent development in viral genomics confirmed that genomic information is preserved among viral subsets and can be used for phylogenetic classification of viruses and for evaluation of viral diversity in the environment. The capsid gene of T4-type bacteriophages, g23, is the most widely applied gene for evaluating the diversity of the T4-type bacteriophage family. In this study, we applied denaturing gradient gel electrophoresis to PCR products of DNA with g23-specific primers that were extracted from a Japanese paddy field under long-term fertilizer trial and obtained 39 different g23 clones at the DNA level. They showed identities of 27–99% with the clones within the NCBI database at the amino acid level. They were quite distinctive from those obtained in marine environments and most of them formed six phylogenetically novel groups in the T4-type bacteriophage family with the clones obtained from another paddy field. The existence of six novel groups was confirmed from molecular analysis of all the amino acid sequences between the primers, of the amino acid sequences excluding hypervariable region, and of those of conserved regions. These findings indicate that T4-type bacteriophage communities in paddy fields consist of previously uncharacterized members phylogenetically distant from those in marine environments. The type of fertilizers and the stage during rice cultivation were not the major factors in determining T4-type bacteriophage communities in the paddy field.  相似文献   

9.
Abstract

The present study examined T4-type phage communities in rice straw (RS) under the composting process by analyzing the composition of the major capsid gene (g23) of T4-type bacteriophages. The g23 clones were obtained from RS throughout the composting process from RS materials to composting RS in the curing stage (for 124?days). Most of the g23 clones were phylogenetically closely related to those in rice field soils and rice field floodwaters, and Paddy Groups II and III appeared to characterize the g23 genes in the composting RS. The diversity of g23 genes in the composting RS was highest in the RS material (day 0 after the onset of composting) and in the early thermophilic stage (day 7), and decreased markedly in the middle and curing stages. This change was in contrast to that of the bacterial community, which showed higher diversity in the middle and curing stages. There was no specific clone that characterized any stage during the composting process. These findings indicate that the phage community is not the major controlling agent in determining eubacterial succession and that the thermophilic stage in the composting process efficiently annihilated T4-type phages in the composting pile.  相似文献   

10.
Denitrification is an important part of the nitrogen cycle in the environment, and diverse bacteria, archaea, and fungi are known to have denitrifying ability. Rice paddy field soils have been known to have strong denitrifying activity, but the microbes responsible for denitrification in rice paddy field soils are not well known. Present study analyzed the diversity and quantity of the nitrite reductase genes (nirS and nirK) in a rice paddy field soil, sampled four times in one rice-growing season. Clone library analyses suggested that the denitrifier community composition varied over sampling time. Although many clones were distantly related to the known NirS or NirK, some clones were related to the NirS from Burkholderiales and Rhodocyclales bacteria, and some were related to the NirK from Rhizobiales bacteria. These denitrifiers may play an important role in denitrification in the rice paddy field soil. The quantitative PCR results showed that nirK was more abundant than nirS in all soil samples, but the nirK/nirS ratio decreased after water logging. These results suggest that both diversity and quantity changed over time in the rice paddy field soil, in response to the soil condition.  相似文献   

11.
The present study examined T4-type phage communities in rice straw (RS) under the composting process by analyzing the composition of the major capsid gene ( g23 ) of T4-type bacteriophages. The g23 clones were obtained from RS throughout the composting process from RS materials to composting RS in the curing stage (for 124 days). Most of the g23 clones were phylogenetically closely related to those in rice field soils and rice field floodwaters, and Paddy Groups II and III appeared to characterize the g23 genes in the composting RS. The diversity of g23 genes in the composting RS was highest in the RS material (day 0 after the onset of composting) and in the early thermophilic stage (day 7), and decreased markedly in the middle and curing stages. This change was in contrast to that of the bacterial community, which showed higher diversity in the middle and curing stages. There was no specific clone that characterized any stage during the composting process. These findings indicate that the phage community is not the major controlling agent in determining eubacterial succession and that the thermophilic stage in the composting process efficiently annihilated T4-type phages in the composting pile.  相似文献   

12.
The conversion factor, kK, for estimation of microbial biomass potassium (K) by the chloroform-fumigation extraction method was determined for some arable soils: upland field soils under different fertilization conditions, an upland field soil under a greenhouse condition, and a paddy field soil under a flooded condition. The kK value varied with land utilization (paddy or upland) or fertilization (chemical or organic fertilizer). Value of kK was different between paddy field soil (0.28–0.38) and upland field soil (0.41–0.73). This study indicates that the value could be useful for the estimation of microbial biomass K in soil by the chloroform-fumigation extraction method and further investigation of the amounts of biomass K in different types of soils under conditions with varied field managements will be necessary.  相似文献   

13.
The community structure of methanogenic archaea is relatively stable,i.e.,it is sustained at a high abundance with minimal changes in composition,in paddy field soils irrespective of submergence and drainage.In contrast,the abundance in non-methanogenic oxic soils is much lower than that in paddy field soils.This study aimed to describe methanogenic archaeal community development following the long-term submergence of non-methanogenic oxic upland field soils in pot and field experiments.In the pot experiment,a soil sample obtained from an upland field was incubated under submerged conditions for 275 d.Soil samples periodically collected were subjected to culture-dependent most probable number(MPN)enumeration,polymerase chain reaction-denaturing gradient gel electrophoresis(PCR-DGGE)analysis of archaeal 16 S r RNA gene,and quantitative PCR analysis of the methyl-coenzyme M reductase alpha subunit gene(mcr A)of methanogenic archaea.The abundance of methanogenic archaea increased from 102 to 103 cells g-1 dry soil and 104 to 107 copies of mcr A gene g-1 dry soil after submergence.Although no methanogenic archaeon was detected prior to incubation by the DGGE analysis,members from Methanocellales,Methanosarcinaceae,and Methanosaetaceae proliferated in the soils,and the community structure was relatively stable once established.In the field experiment,the number of viable methanogenic archaea in a rice paddy field converted from meadow(reclaimed paddy field)was monitored by MPN enumeration over five annual cycles of field operations.Viability was also determined simultaneously in a paddy field where the plow layer soil from a farmer’s paddy field was dressed onto the meadow(dressed paddy field)and an upland crop field converted from the meadow(reclaimed upland field).The number of viable methanogenic archaea in the reclaimed paddy field was below the detection limit before the first cultivation of rice and in the reclaimed upland field.Then,the number gradually increased over five years and finally reached 103–104 cells g-1 dry soil,which was comparable to that in the dressed paddy field.These findings showed that the low abundance of autochthonous methanogenic archaea in the non-methanogenic oxic upland field soils steadily proliferated,and the community structure was developed following repeated and long-term submergence.These results suggest that habitats suitable for methanogenic archaea were established in soil following repeated and long-term submergence.  相似文献   

14.
The paddy field is being recognised as a biodiversity hotspot fostering a variety of organisms. However, there are few studies on the ecology of paddy field nematodes. We characterised nematode communities in rice paddy fields by comparing them with upland fields of rice or soybean. We examined nematode communities of the top (0-15 mm) and second (15-50 mm) soil layers before flooding (March or April), during flooding (June or July) and during the draining period (October) 2007-2009. We found that the nematode community in the paddy was different than that in the upland fields during all periods. Rhabdolaimus, Tobrilus, Mesodorylaims and Monhysteridae characterised the top of the paddy and Hirschmanniella characterised the second layer of the paddy. Total nematode density was generally lower in the paddy than in the upland field. However, the density in the paddy top layer increased with time from the flooding period to the draining period, during which time it was about the same as (or even greater than) the peak density in the upland fields. The density in the second layer of the paddy remained lower than that in the top layer of the paddy throughout the time course. Community diversity values were generally greater in the paddy top layer than in the paddy second layer across the six sampling periods, but periodic differences between the paddy and upland fields or between soil layers were not significant. During the flooding period, the F/(F + B) (13-37) and Enrichment Index (17-38) values were lower in the paddy than in the upland fields (32-47, 37-74, respectively) to reflect that bacteria dominate over fungi with slow decomposition due to anaerobic conditions in the flooded paddy field. In addition, particularly in the top layer, the Maturity (2.0-2.4) and Structure Index (23-72) values were greater in the paddy than in the upland fields (1.7-2.1, 9-15, respectively), indicating a well-developed ecosystem under water. These unique nematode communities persisted during the draining period, but there was a rapid increase in opportunistic bacterivores, which increased the EI values. We suggest that bactivorous nematodes in the families Cephalobidae and Chronogasteridae, herbivores in the genus Hirschmanniella, and fungivores in the genus Filenchus may be specific to paddy field soil rather than to pond and lake sediments.  相似文献   

15.
Forested mineral soil wetlands (FMSW) store large stocks of soil organic carbon (SOC), but little is known on: (i) whether the quality of SOC stored in these soils (proportion of active versus more resistant SOC compounds) differs from SOC in upland soils; (ii) how the quality of SOC in FMSW varies with mean annual temperature (MAT); and (iii) whether SOC decomposition rates in these environments respond to warming and drying more strongly than those observed in upland soils. To address this substantial knowledge gap, we identified nine FMSW and fifteen paired upland forest sites across three bioregions in North America (sub-alpine in Colorado; north-temperate in Minnesota; and south-temperate in South Carolina) to test the following three hypotheses. First, FMSW store a higher proportion of active SOC compared with upland systems because long anaerobic periods favor the accumulation of labile substrates. Second, in FMSW, SOC quality decreases from cold to warm bioregions because high quality detritus accumulates preferentially at cool sites where decomposition is slow. Finally, decomposition of SOC in FMSW will respond more strongly to warming under aerobic conditions than SOC from upland forest soils because of higher accumulation of active SOC in FMSW. To test these hypotheses, we incubated FMSW and upland forest soils at two constant temperatures (10 and 30 °C) for 525-d under aerobic conditions and constant moisture. In contrast to our first hypothesis, we observed similarly rapid depletion of active SOC compounds at initial stages of incubation across FMSW and upland sites, and across the 525-d incubations we observed overall lower SOC decomposition rates in our FMSW soils. In line with our second hypothesis, and across FMWS and upland soils, we found greater SOC loss in the sub-alpine bioregion than both temperate regions. In contrast to our last hypothesis, we found no difference in the temperature sensitivity (Q10) of SOC decomposition in FMSW and upland forest soils. Critically, total SOC loss (g SOC per g soil) was larger in FMSW because of the large amount of SOC stored in these ecosystems, indicating that despite a lack of difference between FMSW and upland responses, the total release of C from FMSW that could result from global warming may be large.  相似文献   

16.
Soil purple phototrophic bacterial (PPB) communities and their responses to elevated atmospheric carbon dioxide (CO2) concentration and nitrogen (N) fertilizer were investigated under a rotation of paddy rice (Oryza sativa L.) and winter wheat (Triticum aestivum L. cv. Yangmai 14) cultivation in a FACE (free‐air CO2 enrichment) system. Community structures and abundances of PPB were determined by denaturing gradient gel electrophoresis (DGGE) and real‐time quantitative PCR respectively, targeting the pufM gene, which encodes a protein in the light reaction centre of PPB. Soil PPB communities were more diverse and larger under rice than under wheat cultivation, which may be attributed to the flooding of the paddy field and soil moisture changes. Elevated atmospheric CO2 concentration significantly increased the abundance and biodiversity of PPB in soils under rice cultivation, while N fertilizer application rate had less effect on the abundance and diversity. Phylogenetic analysis showed that two common dominant DGGE bands belonged to Bradyrhizobium‐ and Rhodopseudomonas palustris‐like PPB in both rice and wheat soils. The results demonstrated a significant shift in soil PPB communities during the rice‐wheat rotation, and a strong positive response of PPB communities to an elevated atmospheric CO2 concentration. Our results also indicated that a diverse and abundant soil PPB community could occur in upland crop fields as well as in aquatic environments and paddy‐rice fields. These findings extend our understanding of the ecological significance of PPB in terrestrial soil environments and their responses to future climate change.  相似文献   

17.
为了研究紫茎泽兰(Ageratina adenophora)入侵对土壤菌根真菌(mycorrhizal fungi, MF)群落的影响,采用嵌套PCR 技术分析了外来植物紫茎泽兰入侵生境内土著植物群落、土著植物与紫茎泽兰混生群落、紫茎泽兰单优群落中, 侵染紫茎泽兰及土著植物的MF 群落结构, 及紫茎泽兰与土著植物根围土壤中MF 群落结构。结果表明, 紫茎泽兰不同入侵进程MF 群落结构存在差异, 其中, 从土著植物群落的植物根内检测到内养球囊霉(Glomus intraradices)型克隆; 从土著植物与紫茎泽兰混生群落的紫茎泽兰根内也检测到内养球囊霉型克隆, 而在土著植物根内检测到1 个球囊霉属(Glomus sp 2)型克隆; 从紫茎泽兰单优群落的紫茎泽兰根内未检测到MF, 但从其根围土壤中检测到2 个球囊霉属(Glomus sp 1 和Glomus sp 2)型克隆。在土著植物与紫茎泽兰混生群落中, 从紫茎泽兰根围土壤中检测到4 个克隆型, 分别为毛舌菌阔孢(Trichoglossum hirsutum)、皂味口磨(Tricholoma saponaceum)、亚盖趋本菌(Xylobolus subpileatus)和翘鳞肉齿菌(Sarcodon imbricatus), 从土著植物根围土壤中也检测到4 个克隆型, 分别为小皮伞(Camarophyllopsis hymenocephala)、肉色香蘑(Lepista irina)、皂味口磨及亚侧耳(Panellus serotinus)型克隆; 在土著植物群落中, 从根围土壤只检测到皂味口磨型克隆。紫茎泽兰入侵改变了土著MF 群落结构, 其中在土著植物占据的土壤中以外生菌根真菌为主, 而外来植物紫茎泽兰则更多地积累了丛枝菌根真菌。文中讨论了紫茎泽兰改变入侵地土壤菌根菌群落及其可能对紫茎泽兰入侵的反馈。  相似文献   

18.
Elucidating the biodiversity of CO2-assimilating bacterial communities under different land uses is critical for establishing an integrated view of the carbon sequestration in agricultural systems. We therefore determined the abundance and diversity of CO2 assimilating bacteria using terminal restriction fragment length polymorphism and quantitative PCR of the cbbL gene (which encodes ribulose-1,5-biphosphate carboxylase/oxygenase). These analyses used agricultural soils collected from a long-term experiment (Pantang Agroecosystem) in subtropical China. Soils under three typical land uses, i.e., rice–rice (RR), upland crop (UC), and paddy rice–upland crop rotation (PU), were selected. The abundance of bacterial cbbL (0.04 to 1.25?×?108 copies g?1 soil) and 16S rDNA genes (0.05–3.00?×?1010 copies g?1 soil) were determined in these soils. They generally followed the trend RR?>?PU?>?UC. The cbbL-containing bacterial communities were dominated by facultative autotrophic bacteria such as Mycobacterium sp., Rhodopseudomonas palustris, Bradyrhizobium japonicum, Ralstonia eutropha, and Alcaligenes eutrophus. Additionally, the cbbL-containing bacterial community composition in RR soil differed from that in upland crop and paddy rice–upland crop rotations soils. Soil organic matter was the most highly statistically significant factor which positively influenced the size of the cbbL-containing population. The RR management produced the greatest abundance and diversity of cbbL-containing bacteria. These results offer new insights into the importance of microbial autotrophic CO2 fixation in soil C cycling.  相似文献   

19.
围海造田是沿海地区拓展土地面积的主要途径。土壤氮矿化参数是揭示围海造田土壤肥力演变和土壤氮供应的重要指标,但是我国沿海造田土壤的相关研究少有报道。本研究以杭州湾南岸海积平原上慈溪市1000年和520年筑塘造田区为对象,选择4个代表性采样点,每个点从低洼稻田采集1个表层混合水稻土,在其相邻高地采集1个表层混合旱地土壤,共8个样品。采用间隙淋洗法研究了土壤样品氮矿化动力学特征。结果如下: 119 d培养试验证实水稻土和旱地土壤有机氮矿化动力学符合一级反应动力学方程Nt=N0(1-e-kt); 水稻土有机氮矿化势（N0）为82.7～161.9 mg/kg（平均114 mg/kg）,占有机氮的7.3%,旱地土壤N0为63.9～104.4 mg/kg（平均83.4 mg/kg）,占有机氮的7.3%; 水稻土有机氮矿化速率（k）为0.033～0.114/d（平均0.064/d）,旱地土壤k为0.007～0.023/d（平均0.020/d）。土壤综合供氮指标（N0k）,水稻土为3.8418.46 mg/(kgd)［平均8.0 mg/(kgd)］,旱地土壤为0.54～2.66 mg/(kgd)［平均1.6 mg/(kgd)］。水稻土总氮含量为1.4～2.0 g/kg （平均1.6 g/kg）,旱地为0.87～2.0 g/kg（平均1.3 g/kg）。可见,水稻土氮库、供氮潜力和速率均大于相邻旱地土壤。因此,从土壤氮肥力来讲,相对于旱地,围海形成的水稻田更具有可持续利用性。  相似文献   

20.
【目的】土壤易分解碳库(labile organic carbon,Lab-C)和耐分解碳库(recalcitrant organic carbon,Rec-C)是土壤有机质的重要组分,其组分大小与比例可反映土壤有机碳的周转与固存特性。因此,研究长期不同施肥制度下土壤易分解碳库与耐分解碳库的大小与比例,对土壤养分管理及肥力培育具有重要的意义。【方法】利用我国东部23年长期不同施肥制度下的黑土、潮土、红壤和32年水稻土共四类土壤的典型土样为代表,以不施肥(CK)、施化肥(NPK)、化肥配施秸秆(NPKS)和化肥配施有机肥(NPKM)4个处理土壤,采用颗粒密度相结合的方法,将土壤有机碳分为易分解碳和耐分解碳2个组分,分析了其不同组分碳含量及比例的变化特征。【结果】土壤经该方法分组后,四种土壤的平均质量回收率和碳回收率均超过95%,是一种测定土壤易分解碳和耐分解碳的可行方法。旱作土壤(黑土、潮土和红壤)易分解碳的平均含量为1.91 g/kg低于水田的2.42 g/kg,而易分解碳占总有机碳的平均比例为15.4%,高于水田的9.9%。NPKM处理下,黑土、潮土和红壤易分解碳含量显著高于NPKS、NPK及CK处理(P0.05),较NPK处理增加的比例分别为98.4%、43.7%和71.2%,同时提高了易分解碳占总有机碳的比例,但无显著差异性;NPK和NPKS处理下黑土与潮土易分解碳的含量较不施肥无显著变化,而红壤易分解碳含量较不施肥显著降低(P0.05),降低的比例分别为33.1%和29.6%;水稻土4个处理间易分解碳的含量及其占全碳的比例无显著差异性。四类土壤耐分解碳的含量与总有机碳含量的变化一致,均表现为NPKMNPKSNPKCK。NPKM处理下,四种土壤耐分解碳含量显著增加(P0.05),黑土、潮土、红壤和水稻土较NPK处理增加的比例分别为68.8%、42.7%、17.6%和17.2%,同时耐分解碳占全碳的比例降低;NPKS处理下黑土、潮土和水稻土耐分解碳的含量较NPK处理也增加,对应增加的比例分别为10.9%、15.1%和18.0%。同时,易分解碳和耐分解碳的含量与土壤总有机碳含量之间有极显著的正相关关系。【结论】旱作土壤易分解碳含量比水田土壤更易受不同施肥处理的影响,有机无机配施(NPKM与NPKS)可提高旱作与水田土壤易分解碳与耐分解碳的含量,同时相对提高了易分解碳占全碳的比例,且NPKM处理的效果优于NPKS处理,更优于化肥处理。  相似文献   

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