陳 亮,劉 鋒,*,肖潤林,吳金水,*

1 中國科學(xué)院亞熱帶農(nóng)業(yè)生態(tài)研究所,亞熱帶農(nóng)業(yè)生態(tài)過程重點實驗室, 長沙 410125 2 中國科學(xué)院亞熱帶農(nóng)業(yè)生態(tài)研究所,長沙農(nóng)業(yè)環(huán)境監(jiān)測研究站, 長沙 410125

人工濕地氮去除關(guān)鍵功能微生物生態(tài)學(xué)研究進展

陳 亮1,2,劉 鋒1,2,*,肖潤林1,2,吳金水1,2,*

1 中國科學(xué)院亞熱帶農(nóng)業(yè)生態(tài)研究所,亞熱帶農(nóng)業(yè)生態(tài)過程重點實驗室, 長沙 410125 2 中國科學(xué)院亞熱帶農(nóng)業(yè)生態(tài)研究所,長沙農(nóng)業(yè)環(huán)境監(jiān)測研究站, 長沙 410125

人工濕地是一種能有效處理水體氮素污染的生態(tài)技術(shù),其中微生物是驅(qū)動人工濕地系統(tǒng)中氮素去除的重要引擎。近20年來,隨著分子生物學(xué)技術(shù)的廣泛應(yīng)用,有關(guān)人工濕地氮去除功能微生物生態(tài)學(xué)方面研究取得了一些重要進展。以硝化-反硝化作用和厭氧氨氧化作用這兩種重要的人工濕地微生物脫氮途徑為主,針對氨氧化細菌/古菌、厭氧氨氧化菌和反硝化菌等關(guān)鍵脫氮功能微生物的研究,重點歸納總結(jié)了目前有關(guān)這幾類關(guān)鍵功能菌群在人工濕地中的豐度、活性、多樣性、分布特征與影響因素,及其對廢水中氮去除的作用,并在此基礎(chǔ)上對今后的重點研究工作提出了展望。面向未來人工濕地氮去除關(guān)鍵功能微生物的研究應(yīng)側(cè)重其在污水凈化和溫室氣體減排等方面的生態(tài)功能研究,同時加強其代謝過程與機制以及不同功能菌群間的關(guān)聯(lián)研究。

人工濕地；氨氧化細菌/古菌；厭氧氨氧化菌；反硝化菌

隨著社會經(jīng)濟和農(nóng)業(yè)生產(chǎn)的發(fā)展,大量外源氮素進入自然水體中造成了嚴重的河流湖泊等水環(huán)境富營養(yǎng)化問題。當(dāng)前,人工濕地已成為有效削減水體中外源氮素的重要技術(shù)手段,在處理非點源污染帶來的氮負荷更是如此。人工濕地是由基質(zhì)(原位土壤或人工填料)、生長在其上的水生植物和附著與懸浮在二者上的微生物所組成的生態(tài)系統(tǒng)。根據(jù)污水在系統(tǒng)中流動方式的差異,人工濕地污水處理系統(tǒng)通?？煞譃楸砻媪?surface flow constructed wetlands, SFCW)和潛流(subsurface flow constructed wetlands, SSFCW)兩種類型,后者又分為水平流(horizontal subsurface flow constructed wetlands, HSSFCW)和垂直流(vertical subsurface flow constructed wetlands, VSSFCW)兩種進水方式；與傳統(tǒng)污水處理工藝相比,人工濕地具有氮去除效果好、耐沖擊負荷能力強、運行管理費用低和生態(tài)環(huán)境友好等優(yōu)點[1]。

圖1 人工濕地氮去除關(guān)鍵微生物過程及相應(yīng)功能基因 Fig.1 The key microbial N-removal pathways and their related functional genes in constructed wetland

1 氨氧化細菌或古菌(AOB/AOA)

氨氧化是硝化作用的第一個反應(yīng)步驟,也是限速步驟,是人工濕地氮去除過程的重要環(huán)節(jié)。典型的氨氧化過程通常認為是一個主要由變形菌門(Proteobacteria)中的一小部分細菌類群所進行的專性好氧的化能自養(yǎng)過程,這類細菌被稱為氨氧化細菌(AOB)。然而近年來越來越多的證據(jù)顯示,在自然界原核生物組成中占重要比例的中溫泉古菌(non-thermophilic Crenarchaeota)(后單獨劃分為奇古菌門(Thaumarchaeota))也具有氨氧化能力,這類古菌被稱作氨氧化古菌(AOA)[6]。這兩類具有氨氧化作用的微生物普遍存在于海洋沉積物、湖泊底泥和陸地土壤等不同的生境中。在典型的微生物群落中,AOB所占的比例通常<0.1%,且主要集中在亞硝化球菌屬(Nitrosococcus)、亞硝化單胞菌屬(Nitrosomonas)和亞硝化螺菌屬(Nitrosospira)這3個屬[7]。相比之下,AOA無論在數(shù)量和多樣性上普遍都要高于AOB,已知的主要種屬有Nitrosopumilus、Nitrosophaera、Nitrosocaldus、Nitrosotalea等,但目前尚未確定是否所有的奇古菌均具有氨氧化能力[8]。

氨氧化微生物作為驅(qū)動人工濕地氮轉(zhuǎn)化的一類重要功能微生物得到了研究者的廣泛關(guān)注(表1)。氨氧化菌群落在人工濕地中的不同區(qū)域分布不同,植物根系是微生物最活躍的區(qū)域,根區(qū)為微生物提供了結(jié)構(gòu)不同的附著表面并形成了根系分泌物和輸氧濃度梯度,通常AOB數(shù)量和種類在氧含量較高的基質(zhì)表層和植物根區(qū)相對較多[12]。如靖元孝等[13]研究的風(fēng)車草(Cyperusalternifolius)人工濕地系統(tǒng)中,根區(qū)的硝化微生物數(shù)量和硝化強度遠高于非根區(qū)。此外,AOB的群落結(jié)構(gòu)在人工濕地系統(tǒng)中通常比較穩(wěn)定,Roberts等[14]利用FISH技術(shù)對潛流濕地系統(tǒng)生物膜中氨氧化細菌Nitrosomonas的原位分析發(fā)現(xiàn)氨氧化菌從生物膜形成的初期就已經(jīng)存在,在5個月的實驗期間其占總細菌種群的比例約1%,但在提高氨氮濃度的一段時間里,Nitrosomonas很快增加到總細菌種群的7%。Ibekwe等[15]采用變性梯度凝膠技術(shù)(DGGE)研究處理奶牛場廢水的人工濕地中AOB組成變化情況,發(fā)現(xiàn)AOB種類在系統(tǒng)中以Nitrosospira為主且在試驗期間沒有發(fā)生優(yōu)勢種群變化。在人工濕地系統(tǒng)中,AOB主要以Nitrosomonas和Nitrosospira這兩種屬居多,且前者比后者具有更低的基質(zhì)親和力和更高的活性,因此Nitrosospira通常發(fā)現(xiàn)存在于低氨氮環(huán)境中且更能忍受外界物理化學(xué)環(huán)境條件的變化,而高氨氮濃度環(huán)境下更易導(dǎo)致Nitrosomonas成為占主導(dǎo)地位的唯一優(yōu)勢種[16- 18]。許多不同的環(huán)境因素包括溫度、pH和鹽度,以及氨氮和有機碳負荷等都會影響氨氧化微生物的多樣性及組成。Dong等[9]對處理養(yǎng)豬廢水的“濕地-塘-濕地”組合人工表面流濕地系統(tǒng)中潛在硝化速率和AOB群落進行了研究,研究發(fā)現(xiàn)AOB數(shù)量和硝化速率與濕地中氨氮濃度均呈顯著正相關(guān)關(guān)系。Sims等[19]對一污水處理廠出水的表面流人工濕地中AOA和AOB進行了為期兩年的季節(jié)性采樣分析,q-PCR結(jié)果顯示人工濕地底泥和水中的AOA豐度在冬夏季都普遍高于AOB,進一步采用末端限制性片段長度多態(tài)性分析(T-RFLP)發(fā)現(xiàn)在冬季AOB普遍具有較低的峰強,表明其對溫度的敏感度要高于AOA,研究還發(fā)現(xiàn)人工濕地的硝化作用強度只與AOB豐度呈顯著相關(guān),表明該濕地中硝化作用主要是由AOB驅(qū)動的。人工濕地不同種類的植物以及其它微生物也會對氨氧化菌群結(jié)構(gòu)造成影響。黃娟等[20]對低溫域(0—15℃)下黃菖蒲、菖蒲和香蒲人工濕地系統(tǒng)中硝化強度和AOB/AOA數(shù)量的研究表明不同植物根際氨氧化過程的主要功能微生物具有一定差異,AOA和AOB對于濕地土壤氮轉(zhuǎn)化均具有不可忽視的作用,并與植物本體、土壤硝化過程微環(huán)境之間有一定的耦合關(guān)系。Schramm等[21]研究證實氨氧化菌和異養(yǎng)微生物間存在競爭,隨著生物膜成熟異養(yǎng)微生物的增加會降低氨氧化菌的種群數(shù)量。這些研究表明人工濕地系統(tǒng)中普遍存在氨氧化微生物,且其豐度、群落結(jié)構(gòu)和代謝活性受溫度、pH、溶解氧、氧化還原電位、氨氮濃度、植物等外界環(huán)境因素的影響。

2 反硝化細菌

微生物的反硝化作用是將氮素以N2O或N2形式從人工濕地中最終去除的過程。反硝化菌為兼性厭氧菌,多為化學(xué)異養(yǎng)型菌,在對氮轉(zhuǎn)化的過程中只獲得能量,并以有機物為電子供體和細胞生長碳源。具有反硝化能力的微生物種類較多,土壤中重要的反硝化細菌包括芽孢桿菌屬(Bacillus)、假單胞菌屬(Pseudomonas)、微球菌(Micrococcus)；水體中主要的反硝化菌有假單胞菌屬(Pseudomonas)、產(chǎn)氣單胞菌屬(Aeromonas)和弧菌屬(Vibrio)；其它反硝化菌有氣桿菌屬(Aerobacter)、產(chǎn)堿桿菌屬(Alcalogenes)、短桿菌(Brevibacterium)、黃桿菌屬(Flavobactrium)等[29]。

表1 人工濕地系統(tǒng)中氨氧化微生物(AOA/AOB)的國內(nèi)外研究概括

反硝化作用的4個過程分別由硝酸還原酶(Nar)、亞硝酸還原酶(Nir)、氧化氮還原酶(Nor)和氧化亞氮還原酶(Nitrous oxide reductase, Nos)進行催化,相應(yīng)編碼基因分別為nar、nir、nor、nos[30]。目前針對環(huán)境樣品研究者較多選擇nirK/nirS和nosZ作為分子標記基因來研究反硝化菌群落多樣性和豐度情況。反硝化菌活性的測定普遍采取的是乙炔抑制法[31-32]。該方法利用乙炔能夠抑制N2O還原成N2的原理,向采得的樣品柱通入一定量乙炔氣,培養(yǎng)一段時間后,從中抽取一定量氣體,用氣相色譜分析N2O的濃度,據(jù)此計算反硝化速率。

對人工濕地系統(tǒng)中反硝化菌群落的研究普遍發(fā)現(xiàn)具有較高的豐度和多樣性。Ruiz-Rueda等[33]在處理市政廢水的表面流濕地中發(fā)現(xiàn)存在豐富的反硝化功能基因nirS。Chon等[34]采用定量PCR技術(shù)檢測處理污水處理廠出水的人工濕地中反硝化功能基因(narG、nirS和nosZ)豐度都在106—109copies/g間,并呈現(xiàn)季節(jié)性差異。Kjellin等[35]通過DGGE研究nosZ功能基因多樣性發(fā)現(xiàn)越靠近人工濕地進水口反硝化菌群落越簡單,且延長水力停留時間會導(dǎo)致表面流濕地底泥中反硝化菌的群落結(jié)構(gòu)更復(fù)雜,說明底泥中碳氮濃度會對反硝化菌群具有重要影響,濃度越高菌群結(jié)構(gòu)越簡單優(yōu)勢種更明顯。Song等[32]認為要使?jié)竦刂芯哂凶畲蟮姆聪趸俾时仨毤嬗凶罴训沫h(huán)境條件和代謝活性,該研究利用T-RFLP技術(shù)監(jiān)測了一個新建人工濕地中反硝化群落的年際變化情況,結(jié)果發(fā)現(xiàn)第二年濕地中反硝化菌的群落結(jié)構(gòu)更簡單且穩(wěn)定,活性也比第一年強,相關(guān)分析表明反硝化作用主要受濕地環(huán)境中溫度,pH和有機碳(DOC)濃度的影響很大。一般來說氧的存在會抑制反硝化酶,但有的人工濕地中存在能夠在有氧條件下進行反硝化的微生物[11],這種好氧反硝化菌含有不受氧氣抑制的周質(zhì)硝酸鹽還原酶(Nap)。溫度變化對反硝化菌有強烈影響,在溫度低于5℃時反硝化速度很慢,并且在溫度低進行的反硝化通常不徹底會產(chǎn)生N2O和NO。通常增加人工濕地中DOC含量會提高反硝化速率,但Burchell等[36]研究表明冬季低溫(7.5℃)情況下反硝化速率對增加有機質(zhì)并沒有響應(yīng)。反硝化的最佳pH值為6—8,低于5時反硝化菌的活性受到很大抑制。植物對人工濕地反硝化菌群的影響主要是通過根際分泌有機碳,許多研究證實有植物比無植物情況下對NO3-N的去除效率更高,且反硝化功能基因、速率大小會因植物種類不同而不同[33,37-39]。

3 厭氧氨氧化細菌

表2 人工濕地系統(tǒng)中厭氧氨氧化菌的國內(nèi)外研究概括

4 關(guān)鍵功能微生物對人工濕地中氮去除的效應(yīng)

微生物是人工濕地氮去除能力的重要評價指標,最常見的研究方法是用微生物數(shù)量和活性作為評價污染物去除率的參考指標,探討微生物群落的組成和分布,從而了解人工濕地處理廢水時微生物在其中的作用過程。目前明確闡述關(guān)鍵功能微生物類群在人工濕地氮去除作用與機制的研究還較少,如某些氮轉(zhuǎn)化功能微生物對溫室氣體的釋放具有一定的調(diào)節(jié)作用,而如何應(yīng)用它們控制溫室氣體的排放還有待深入研究。

5 展望

綜上所述,現(xiàn)代分子生物學(xué)技術(shù)的發(fā)展為人工濕地微生物生態(tài)研究開啟了新紀元,有關(guān)氮轉(zhuǎn)化功能菌群在復(fù)雜的人工濕地系統(tǒng)中的存在、多樣性組成及活性等得到了廣泛研究,這對于我們深刻理解人工濕地氮去除的復(fù)雜過程具有重要推動作用。如何提高廢水中氮的處理效率依然是未來人工濕地技術(shù)需解決的重要問題之一,而氮轉(zhuǎn)化相關(guān)功能微生物的研究可謂重點。面向未來的人工濕地功能微生物與氮去除研究,應(yīng)以新技術(shù)新方法為手段,重點開展以下幾個方面的研究。

(1)進一步探索與挖掘新型氮轉(zhuǎn)化功能微生物在人工濕地中的群落分布與生態(tài)功能。厭氧氨氧化菌、氨氧化古菌和一步硝化菌的發(fā)現(xiàn)更新了人們已有的對氮循環(huán)的認識,而新型氮轉(zhuǎn)化功能種群在人工濕地系統(tǒng)中的研究報道還非常少,許多問題有待更多研究。例如厭氧氨氧化菌在不同類型和尺度的人工濕地系統(tǒng)以及不同時空變化下的普遍性和活性強度如何還不清楚,如何進一步發(fā)揮其在某些特殊廢水處理中的應(yīng)用潛力也需更多研究。盡管氨氧化古菌在一些人工濕地系統(tǒng)中能夠檢測到很高豐度和多樣性,但大多研究表明氨氧化作用主要是由氨氧化細菌主導(dǎo),對于這類含amoA基因的氨氧化古菌在系統(tǒng)中大量存在和分布具有的生理功能或生態(tài)學(xué)意義尚不清楚。因此,進一步采用先進分子生物學(xué)技術(shù)(如高通量測序技術(shù)等)并結(jié)合各種原位分析手段(如基于DNA分析的穩(wěn)定同位素探測技術(shù)(DNA-SIP)等)明確這兩類氨氧化菌群在人工濕地氮轉(zhuǎn)化過程中的作用和其它潛在的生態(tài)功能是未來研究的一個重點。

(2)加強人工濕地中氮去除關(guān)鍵微生物的代謝過程與機制的研究。在很多情況下,相關(guān)的監(jiān)測及通量(如進出水中氮濃度變化、氨揮發(fā)、N2O釋放等)和反應(yīng)速率(如硝化、反硝化速率、厭氧氨氧化速率等)與氮轉(zhuǎn)化功能微生物的群落多樣性信息并沒有建立直接關(guān)聯(lián),而環(huán)境因素對其功能作用的表達又具有重要影響,因此加強對這些關(guān)鍵微生物的作用過程及影響因素的認識是發(fā)展調(diào)控人工濕地氮去除有效方法的重要前提。

(3)不同氮去除關(guān)鍵微生物菌群間的關(guān)聯(lián)研究。當(dāng)前研究多只針對某一類功能微生物菌群及過程獨立開展,同一系統(tǒng)中硝化、反硝化和厭氧氨氧化等菌群間的關(guān)系以及它們各自驅(qū)動的氮轉(zhuǎn)化過程是如何交替發(fā)生的尚不清楚。因此在特定人工濕地系統(tǒng)中研究不同氮轉(zhuǎn)化功能菌群間的耦合關(guān)系,以及這種耦合關(guān)系下對廢水中氮去除的貢獻作用,通過關(guān)聯(lián)微生物豐度和功能活性與各形態(tài)氮轉(zhuǎn)化通量,構(gòu)建相關(guān)氮去除模型,為最終調(diào)控人工濕地微生物過程提高氮去除率提供科學(xué)依據(jù)。

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ResearchadvancesinmicrobialecologyforN-removalinconstructedwetlands

CHEN Liang1,2, LIU Feng1,2,*, XIAO Runlin1,2, WU Jinshui1,2,*

1KeyLaboratoryofAgro-ecologicalProcessesinSubtropicalRegion,InstituteofSubtropicalAgriculture,ChineseAcademyofSciences,Changsha410125,China2ChangshaResearchStationforAgricultural&EnvironmentalMonitoring,InstituteofSubtropicalAgriculture,ChineseAcademyofSciences,Changsha410125,China

A constructed wetland (CW) is an effective technology for the treatment of nitrogen (N) pollution in water bodies, with microorganisms being important engines driving N-removal. Over the past two decades, with the development of culture-independent molecular techniques, break-through progress has occurred in microbial ecology for N-removal in CWs. Nitrification-denitrification and anammox processes have been recognized as the two main microbial pathways for N-removal in CWs. In the present study, we reviewed the available literature regarding research progress in N-removal communities including archaeal and bacterial ammonia oxidizers, anammox bacteria, and denitrifying bacteria in CWs. Case studies on bacterial abundance, activities, diversity, distribution, influence factors, and contribution to N-removal are summarized, and future perspectives for this research field are presented. Future microbial ecology studies of N-removal in CWs should focus on the role of microorganisms in purification of sewage and emission reduction in greenhouse gases, and improve research on their N-metabolic processes, mechanisms, and interactions.

constructed wetland; ammonia oxidizing bacteria/archaea; anammox bacteria; denitrifying bacteria

中國博士后基金項目(2014M560648; 2015T80878)；國家自然科學(xué)基金項目(41601272)

2016- 06- 15; < class="emphasis_bold">網(wǎng)絡(luò)出版日期

日期:2017- 04- 25

*通訊作者Corresponding author.E-mail: liufeng@isa.ac.cn; jswu@isa.ac.cn

10.5846/stxb201606151159

陳亮,劉鋒,肖潤林,吳金水.人工濕地氮去除關(guān)鍵功能微生物生態(tài)學(xué)研究進展.生態(tài)學(xué)報,2017,37(18):6265- 6274.

Chen L, Liu F, Xiao R L, Wu J S.Research advances in microbial ecology for N-removal in constructed wetlands.Acta Ecologica Sinica,2017,37(18):6265- 6274.