The fractionation of iron-phosphorus compounds in sediments studied by Mössbauer spectroscopy

Iron compounds of phosphorus form a large part of the phosphorus bound in sediments. Mössbauer spectroscopy is a technique that enables us to study, directly, chemical forms of iron in solid samples. Mössbauer spectroscopy allowed us to check, directly, the selectivity of the extraction scheme for soil phosphorus proposed by Chang &; Jackson (1957), but only as far as the iron compounds are concerned. It appears that selectivity of the extraction method leaves much to be desired.

     

Excretion of total phosphorus,dissolved reactive phosphorus,ammonia, and urea by Lake MichiganMysis relicta

Rates of nutrient release byMysis relicta in Lake Michigan were measured on five nights at a 45-m station near Milwaukee, Wisconsin, U.S.A., in the summer of 1977. Nocturnal vertical migrations of the mysids were monitored with both echosounder tracings and vertical net tows. Estimates of the total areal dry mass of the mysids ranged from 600 to 1 820 mg m–2. Rates of release of dissolved reactive phosphorus, total phosphorus, ammonia, and urea were measured in dark incubations on shipboard. Excretion experiments were initiated immediately after mysids were collected from each of several vertical net hauls. The depths of maximum mysid densities corresponded approximately with a deep phytoplankton peak located in the vicinity of the thermocline. Semiquantitative demands for N and P by phytoplankton within this peak were obtained from¹⁴C estimates of primary production from a previous study, assuming a constant C:N:P ratio for the algae. These algal nutrient demands were compared to potential N and P release by the mysids to obtain a first approximation of the relative rates of nutrient supply and demand for the field phytoplankton populations. Our analysis indicates that mysids may directly supply about 1–10% of the daily N and P demands of the phytoplankton in the deep peak. However, indirect interactions betweenMysis relicta and other organisms, such as small zooplankton and fishes, could be major factors in nutrient recycling within the metalimnion and subthermocline region of Lake Michigan.Contribution No. 238, Center for Great Lakes Studies, University of Wisconsin-Milwaukee, Wisconsin.Contribution No. 238, Center for Great Lakes Studies, University of Wisconsin-Milwaukee, Wisconsin.     

The phosphorus economy of a hypertrophic seepage lake in Scania,south Sweden groundwater influence

The phosphorus dynamics and economy of Lake Bysjön, a hypertrophic seepage lake in Scania, southern Sweden, were investigated during 1973–1977. The mean dissolved inorganic phosphorus concentration (1973–1977) was 580 µg · l^–1. There were no correlations between dissolved inorganic P, total organic P, dissolved organic P, particulate P and phytoplankton biomass. Groundwater inflow and lake water outflow through the ground are the most important factors for maintaining a constant water volume. Groundwater seepage is also important for water quality. Groundwater inflow, together with planktonic activity, keeps the P concentration high in the lake water.     

Antibiotic-resistantArthrobacter sp. andPseudomonas sp. responses in the rhizosphere of blue grama after herbage removal

Summary Streptomycin-resistant Pseudomonas and Arthrobacter were isolated from semi-arid grassland soil and their relative responses in the rhizosphere of blue grama (Bouteloua gracilis) subjected to herbage removal were evaluated. Using plants grown in normal soil, the two bacteria showed differential responses to herbage removal, which were most marked in the rhizoplane, where the Pseudomonas showed a two-log unit increase over a 60 hour period, while Arthrobacter, in contrast, exhibited a one-log unit decrease in viable counts for at least 48 hours after defoliation, responses which are similar to those observed in root exudate medium experiments by earlier workers. These results suggest that the rhizoplane may be a critical environment for interaction of these two types of microorganisms, and that sequential responses of the root-associated soil microorganisms may occur after herbage removal from this important rangeland plant. These responses are most likely associated with increased exudate release following herbage removal, which has been best documented using blue grama grown under sterile conditions.     

Mineral element content in Ulva lactuca L. with reference to eutrophication in Hong Kong coastal waters

The amounts of tissue nitrogen, phosphorus, potassium, sodium, calcium and iron were estimated in the green alga Ulva lactuca L. collected from 9 rural and 14 urban littoral sites in the waters around Hong Kong Island during 1978 and 1979. The mean levels of tissue nitrogen and phosphorus were respectively 65% and 87% more in urban sites than in rural ones. Very significant correlation (r = 0.920) was found between the logarithmic concentration of seawater inorganic nitrogen and that of tissue nitrogen. The same applied to soluble reactive phosphorus in seawater and tissue phosphorus (r = 0.886). The levels of potassium, sodium and calcium in the alga were relatively uniform. However considerable variation in the level of iron was detected. The potential use of Ulva as an indicator species for eutrophication is discussed.     

Dissolved oxygen dependent phosphorus release from profundal sediments of Lake Constance (Obersee)

Phosphorus release rates from profundal sediments of Lake Constance (Obersee) have been determined in D.O., pH regulated sediment-water systems. Above 10% O₂ saturation (> 1.2 ppm D. O.) and with pH as in situ, no net release could be found. Sedimentations of diatom sludge (Asterionella formosa) and carbonate-phosphate coprecipitate (CaCO₃.CaHPO₄) increased the release to 0.5 mg × m^–2 × d^–1 which, however, will not be relevant to the P balance in Obersee. The annual phosphorus accumulation in profundal Obersee and Ueberlingersee is, therefore, observed as due to sinking of phosphorus-bound detritus during the stagnation period.The experimental work was carried out at the Limnological Institute of the University of Freiburg/Breisgau (West Germany) and has been supported by the Industrieverband Körperpflege und Waschmittel e.V. and the Gernan Research Council (DFG)The experimental work was carried out at the Limnological Institute of the University of Freiburg/Breisgau (West Germany) and has been supported by the Industrieverband Körperpflege und Waschmittel e.V. and the Gernan Research Council (DFG)     

不同磷水平对柱花草形态学指标的影响

在不同磷素水平培养条件下,探讨磷胁迫对柱花草形态指标及生物量的影响,评价柱花草对磷浓度的耐受性.该文以12个不同基因型柱花草品种为材料,设置7个磷肥梯度,分别为0.2、0.1、0.075、0.050、0.035、0.02 g·kg-1,以不施磷肥为对照,采用盆栽方法进行施肥试验,比较不同柱花草品种形态指标对不同磷浓度的...     

哈尼梯田湿地土壤不同形态磷的时空分布特征

磷是湿地和农业生态系统中的重要元素之一,其中土壤磷形态的迁移转化广受关注。以哈尼梯田湿地为例,分别在哈尼梯田湿地的水稻生长期、收获期和休闲期,采集湿地不同海拔（梯田区上部、中部和下部）和不同深度的土壤（0-20 cm,20-40 cm,40-60 cm,60-80 cm）进行磷形态分析,研究了哈尼梯田湿地土壤中不同形态磷的时空分布规律和影响因素。结果表明：（1）哈尼梯田湿地土壤中总磷（TP）含量均值为318.74 mg/kg,在水稻收获期含量最高,无机磷（IP）含量均值在水稻休闲期最高（85.95 mg/kg）,湿地土壤磷总体呈缺乏状态。（2）受外源磷输入影响,铁铝结合态磷（NaOH-P）占无机磷比重最大,且季节差异性显著（P<0.05）;而钙结合态磷（HCl-P）在各季节无显著差异（P>0.05）,这与湿地生态环境和地质背景有关。（3）哈尼梯田湿地对磷的迁移有截留作用,表现为各形态磷含量总体呈现在上部梯田湿地较高,并随海拔的降低而降低;不同形态磷含量在20-40 cm土层富集。（4）除HCl-P外,其余形态磷与土壤粒径在不同土层表现为负相关;不同土层TP和有机磷（OP）与pH值呈正相关;土壤总有机碳（TOC）与不同形态磷在收获期呈显著负相关（P<0.05）。研究表明了哈尼梯田湿地立体空间结构和人为活动能影响湿地生态系统中磷的分布与迁移循环,该结论可为梯田湿地的可持续发展提供参考。     

根系去除改变了毛竹林土壤酶活性对氮磷添加的响应

亚热带是我国氮和磷沉降的热点地区,森林生态系统碳（C）、氮（N）、磷（P）循环对N和P沉降的响应受到广泛关注。根系作为森林土壤碳和养分持续供给的重要来源,其输入变化在N和P沉降下通过影响土壤酶活性进而调控土壤碳和养分循环过程。以毛竹林为研究对象,选择硝酸铵和磷酸二氢钠分别进行N和P添加,共设置4个处理：对照、N添加、P添加和N+P添加,并结合壕沟处理,探究毛竹林土壤C、N、P循环相关酶活性对氮磷添加和根系去除的响应,并分析它们与土壤和细根化学性质之间的关系。结果表明：土壤C、N循环相关酶活性整体上对根系去除的响应比氮磷添加更敏感,这主要是因为根系去除显著降低土壤全氮和铵态氮含量,但短期氮磷添加并未显著改变调控土壤酶活性分异的土壤有机碳、全氮和铵态氮含量。与C、N循环相关酶活性不同,土壤P循环相关酶对根系去除和磷添加处理均呈现负响应,这可能是因为阻断根系P吸收和补充土壤P元素降低了微生物的P开采作用。但研究区土壤微生物仍受到P限制作用,这是因为在P缺乏毛竹林生态系统,根系比微生物具有更强的P吸收利用能力。研究结果强调了不同功能土壤酶活性对土壤养分添加和根系输入变化响应的敏感性差异,为预测低P毛竹林生态系统土壤C和养分循环提供依据。