为研究氮添加影响森林土壤有机磷矿化的微生物调控机制,分析了10年的野外氮添加(100 kg N^(-2) ha^(-2)year^(-1))对沙地樟子松人工林土壤微生物中编码酸性磷酸单酯酶、碱性磷酸单酯酶和植酸酶的功能基因(phoC、phoD和appA)丰度及相关...为研究氮添加影响森林土壤有机磷矿化的微生物调控机制,分析了10年的野外氮添加(100 kg N^(-2) ha^(-2)year^(-1))对沙地樟子松人工林土壤微生物中编码酸性磷酸单酯酶、碱性磷酸单酯酶和植酸酶的功能基因(phoC、phoD和appA)丰度及相关酶活性和土壤理化性质的影响。结果表明,氮添加使樟子松人工林土壤中酸性和碱性磷酸单酯酶活性分别下降了18.09%和55.29%,植酸酶活性下降了41.88%。氮添加使土壤微生物中各基因拷贝数分别下降40.97%(16S-rRNA)、78.38%(phoD)、67.92%(phoC)、74.37%(appA)。各基因拷贝数占总细菌基因拷贝数的比例显著下降了61%(phoD)、44%(phoC)、55%(appA)。土壤微生物量碳、微生物量磷含量与酸性磷酸单脂酶、碱性磷酸单脂酶、植酸酶活性及16S rRNA、phoD、phoC、appA基因丰度显著正相关。土壤铵态氮含量与酸性磷酸单脂酶、碱性磷酸单脂酶活性及16S rRNA、phoC、appA基因丰度显著负相关。酸性磷酸单酯酶活性与其基因丰度显著正相关,其他两种酶活性与其基因丰度无显著相关性。以上结果表明,氮添加不仅降低了土壤解磷微生物丰度,还降低了解磷细菌在总细菌中的比例,从而大大降低了磷酸酶活性,抑制了有机磷的矿化。展开更多
Soil samples were collected from both bare and vegetated mine railings to study the changes in bacterial communities and soil chemical properties of copper mine tailings due to reed （Phragmites communis） colonizatio...Soil samples were collected from both bare and vegetated mine railings to study the changes in bacterial communities and soil chemical properties of copper mine tailings due to reed （Phragmites communis） colonization. The structures of bacterial communities were investigated using culture-independent 16S rRNA gene sequencing method. The bacterial diversity in the bare mine tailing was lower than that of the vegetated mine tailing. The former was dominated by sulfur metabolizing bacteria, whereas the latter was by nitrogen fixing bacteria. The bare mine tailing was acidic （pH = 3.78）, whereas the vegetated mine tailing was near neutral （pH ： 7.28）. The contents of organic matter, total nitrogen, and ammonium acetate-extractable potassium in vegetated mine tailings were significantly higher than those in the bare mine railings （P 〈 0.01）, whereas available phosphorus and electrical conductivity were significantly lower than those in the bare mine tailings （P 〈 0.01）. The results demonstrated that 16S rRNA gene sequencing could be successfully used to study the bacterial diversity in mine tailings. The colonization of the mine tailings by reed significantly changed the bacterial community and the chemical properties of tailings. The complex interactions between bacteria and plants deserve further investigation.展开更多
Carbon of humus acids(HSAC) and dissolved organic carbon(DOC) are the most active forms of soil organic carbon(SOC) and play an important role in global carbon recycling. We investigated the concentrations of HSAC,wat...Carbon of humus acids(HSAC) and dissolved organic carbon(DOC) are the most active forms of soil organic carbon(SOC) and play an important role in global carbon recycling. We investigated the concentrations of HSAC,water-soluble organic carbon(WSOC),hot water-extractable organic carbon(HWOC) and SOC in soils under different vegetation types of four copper mine tailings sites with differing vegetation succession time periods in Tongling,China. The concentrations of HSAC,WSOC,HWOC and SOC increased with vegetation succession. WSOC concentration increased with the accumulation of SOC in the tailings,and a linearly positive correlation existed between the concentrations of HSAC and SOC in the tailings. However,the percentages of HSAC and DOC in the SOC decreased during vegetation succession. The rate of SOC accumulation was higher when the succession time was longer than 20 years,whereas the speeds of soil organic matter(SOM) decomposition and humification were slow,and the concentrations of HSAC and DOC increased slowly in the tailings. The percentage of carbon of humic acid(HAC) in HSAC increased with vegetation succession,and the values of humification index(HI),HAC/carbon of fulvic acid,also increased with the accumulation of HSAC and SOC in soils of the tailings sites. However,the HI value in the each of the tailings was less than 0.50. The humification rate of SOM was lower than the accumulation rate of SOM,and the level of soil fertility was still very low in the tailings even after 40 years of natural restoration.展开更多
基金the National Natural Science Foundation of China (Nos.39830310 and 30070134)the NationalKey Basic Research Support Foundation (NKBRSF) of China (No.2002CB111504).
文摘Soil samples were collected from both bare and vegetated mine railings to study the changes in bacterial communities and soil chemical properties of copper mine tailings due to reed （Phragmites communis） colonization. The structures of bacterial communities were investigated using culture-independent 16S rRNA gene sequencing method. The bacterial diversity in the bare mine tailing was lower than that of the vegetated mine tailing. The former was dominated by sulfur metabolizing bacteria, whereas the latter was by nitrogen fixing bacteria. The bare mine tailing was acidic （pH = 3.78）, whereas the vegetated mine tailing was near neutral （pH ： 7.28）. The contents of organic matter, total nitrogen, and ammonium acetate-extractable potassium in vegetated mine tailings were significantly higher than those in the bare mine railings （P 〈 0.01）, whereas available phosphorus and electrical conductivity were significantly lower than those in the bare mine tailings （P 〈 0.01）. The results demonstrated that 16S rRNA gene sequencing could be successfully used to study the bacterial diversity in mine tailings. The colonization of the mine tailings by reed significantly changed the bacterial community and the chemical properties of tailings. The complex interactions between bacteria and plants deserve further investigation.
基金Supported by the National High Technology Research and Development Program(863 Program)of China(No.2006AA06Z359)the National Environmental Protection Public Welfare Science and Technology Research Program of China(No.201009041)the Special Foundation for Young Scientists of Anhui Province,China(No.2010SQRL150)
文摘Carbon of humus acids(HSAC) and dissolved organic carbon(DOC) are the most active forms of soil organic carbon(SOC) and play an important role in global carbon recycling. We investigated the concentrations of HSAC,water-soluble organic carbon(WSOC),hot water-extractable organic carbon(HWOC) and SOC in soils under different vegetation types of four copper mine tailings sites with differing vegetation succession time periods in Tongling,China. The concentrations of HSAC,WSOC,HWOC and SOC increased with vegetation succession. WSOC concentration increased with the accumulation of SOC in the tailings,and a linearly positive correlation existed between the concentrations of HSAC and SOC in the tailings. However,the percentages of HSAC and DOC in the SOC decreased during vegetation succession. The rate of SOC accumulation was higher when the succession time was longer than 20 years,whereas the speeds of soil organic matter(SOM) decomposition and humification were slow,and the concentrations of HSAC and DOC increased slowly in the tailings. The percentage of carbon of humic acid(HAC) in HSAC increased with vegetation succession,and the values of humification index(HI),HAC/carbon of fulvic acid,also increased with the accumulation of HSAC and SOC in soils of the tailings sites. However,the HI value in the each of the tailings was less than 0.50. The humification rate of SOM was lower than the accumulation rate of SOM,and the level of soil fertility was still very low in the tailings even after 40 years of natural restoration.
