An Evaluation of Revegetation Success on Bauxite Residue

The current study was undertaken to evaluate the success of a revegetation program on three sites within the Bauxite Residue Disposal Area at the Aughinish Alumina Ltd. refinery. This was achieved by determining botanical diversity, substrate conditions, and plant uptake. Two sites revegetated in 1999, with and without the use of gypsum, were assessed and compared to a site revegetated in 1997. Compared to an initial 6 species used in seeding, a total of 47 species were recorded growing on the three sites with greatest diversity on the 1997 site. There was limited variation in the residue properties of the three treatments indicating that diversity was most influenced by succession and not substrate conditions. Limited available manganese was found in all treatments and significantly lower exchangeable magnesium in the gypsum-amended treatment. Exchangeable sodium, aluminum, and pH in the substrate were not at levels of concern. Appreciable nitrogen, phosphorus, and potassium were found as a result of a fertilizing program. Dominant species in the 1999 treatments, Holcus lanatus and Trifolium pratense , were analyzed for elemental composition. Compared to previous studies, foliar nitrogen, phosphorus, potassium, and calcium were adequate and sodium levels were low. Manganese and magnesium levels were low, and availability should be assessed as part of the monitoring program. Furthermore, the effect of a fertilizing regime on plant uptake and substrate conditions needs to be assessed.     

Effect of soil water stress on soil respiration and its temperature sensitivity in an 18-year-old temperate Douglas-fir stand

We analyzed 17 months (August 2005 to December 2006) of continuous measurements of soil CO₂ efflux or soil respiration (R_S) in an 18‐year‐old west‐coast temperate Douglas‐fir stand that experienced somewhat greater than normal summertime water deficit. For soil water content at the 4 cm depth (θ) > 0.11 m³ m^?3 (corresponding to a soil water matric potential of ?2 MPa), R_S was positively correlated to soil temperature at the 2 cm depth (T_S). Below this value of θ, however, R_S was largely decoupled from T_S, and evapotranspiration, ecosystem respiration and gross primary productivity (GPP) began to decrease, dropping to about half of their maximum values when θ reached 0.07 m³ m^?3. Soil water deficit substantially reduced R_S sensitivity to temperature resulting in a Q₁₀ significantly < 2. The absolute temperature sensitivity of R_S (i.e. dR_S/dT_S) increased with θ up to 0.15 m³ m^?3, above which it slowly declined. The value of dR_S/dT_S was nearly 0 for θ < 0.08 m³ m^?3, thereby confirming that R_S was largely unaffected by temperature under soil water stress conditions. Despite the possible effects of seasonality of photosynthesis, root activity and litterfall on R_S, the observed decrease in its temperature sensitivity at low θ was consistent with the reduction in substrate availability due to a decrease in (a) microbial mobility, and diffusion of substrates and extracellular enzymes, and (b) the fraction of substrate that can react at high T_S, which is associated with low θ. We found that an exponential (van't Hoff type) model with Q₁₀ and R₁₀ dependent on only θ explained 92% of the variance in half‐hourly values of R_S, including the period with soil water stress conditions. We hypothesize that relating Q₁₀ and R₁₀ to θ not only accounted for the effects of T_S on R_S and its temperature sensitivity but also accounted for the seasonality of biotic (photosynthesis, root activity, and litterfall) and abiotic (soil moisture and temperature) controls and their interactions.     

接种丛枝菌根真菌对云南石漠化土壤呼吸的影响

为探明"丛枝菌根（Arbuscular mycorrhiza，AM）真菌-植物-土壤"耦合作用对石漠化土壤呼吸季节动态的影响，采用LI-6400-09土壤呼吸室和便携式光合作用测量系统，对圆柏（Sabina chinensis）接种摩西斗管囊霉（Funneliformis mosseae，FM）、根内根孢囊霉（Rhizophagus intraradices，RI）2种AM菌种处理下土壤呼吸季节动态进行野外连续定位观测，并探究AM真菌接种处理下石漠化土壤呼吸速率与植物生长、土壤理化性质之间的关系。结果表明：（1）相较于对照，接种AM真菌对石漠化生境土壤呼吸季节动态产生了显著影响（P<0.01）。AM真菌处理具有较高的土壤呼吸季节变化幅度，即根内根孢囊霉处理土壤呼吸速率（1.55-9.10 μmol m^-2 s^-1）显著高于摩西斗管囊霉（1.62-8.29 μmol m^-2 s^-1）和对照（1.23-4.46 μmol m^-2 s^-1）；（2） AM真菌接种处理下土壤温湿度变化对土壤呼吸的影响显著大于对照，即土壤温度与水分对土壤呼吸的平均解释量大小顺序为：RI （44.84%；52.35%）>FM （17.18%；41.65%）>CK （2.66%；16.55%）；（3）2种菌种处理下土壤呼吸速率均与土壤有机质、硝态氮、全氮、速效钾、树高、胸径及根系生物量呈显著或极显著正相关（P<0.01或0.05），而与pH呈极显著负相关（P<0.01），但对照处理土壤呼吸速率除与pH呈显著负相关（P<0.05）外，与其它土壤理化指标相关性不显著；（4）土壤温度和水分、硝态氮、铵态氮、有机质、易氧化有机碳、速效钾、全氮及全磷对土壤呼吸变化的贡献最大，而胸径、树高、有效磷、微生物生物量、根系生物量及pH的影响次之。因此，"AM真菌-寄主植物-土壤"相互作用对石漠化生境土壤呼吸季节动态的影响，主要取决于不同AM真菌接种处理对土壤微气候（如含水量）、碳素（有机质、易氧化有机碳）、无机氮库（铵态氮、硝态氮）、根系生物量及磷钾养分可利用性的调控。     

Warming increases soil carbon input in a Sibiraea angustata-dominated alpine shrub ecosystem

Plant-derived carbon (C) inputs via foliar litter, root litter and root exudates are key drivers of soil organic C stocks. However, the responses of these three input pathways to climate warming have rarely been studied in alpine shrublands. By employing a 3-year warming experiment (increased by 1.3 °C), we investigated the effects of warming on the relative C contributions from foliar litter, root litter and root exudates from Sibiraea angustata, a dominant shrub species in an alpine shrubland on the eastern Qinghai-Tibetan Plateau. The soil organic C inputs from foliar litter, root litter and root exudates were 77.45, 90.58 and 26.94 g C m⁻², respectively. Warming only slightly increased the soil organic C inputs from foliar litter and root litter by 8.04 and 11.13 g C m⁻², but significantly increased the root exudate C input by 15.40 g C m⁻². Warming significantly increased the relative C contributions of root exudates to total C inputs by 4.6% but slightly decreased those of foliar litter and root litter by 2.5% and 2.1%, respectively. Our results highlight that climate warming may stimulate plant-derived C inputs into soils mainly through root exudates rather than litter in alpine shrublands on the Qinghai-Tibetan Plateau.     

Rice G protein γ subunit qPE9-1 modulates root elongation for phosphorus uptake by involving 14-3-3 protein OsGF14b and plasma membrane H+-ATPase

Heterotrimeric G protein is involved in plant growth and development, while the role of rice (Oryza sativa) G protein γ subunit qPE9-1 in response to low-phosphorus (LP) conditions remains unclear. The gene expression of qPE9-1 was significantly induced in rice roots under LP conditions. Rice varieties carrying the qPE9-1 allele showed a stronger primary root response to LP than the varieties carrying the qpe9-1 allele (mutant of the qPE9-1 allele). Transgenic rice plants with the qPE9-1 allele had longer primary roots and higher P concentrations than those with the qpe9-1 allele under LP conditions. The plasma membrane (PM) H⁺-ATPase was important for the qPE9-1-mediated response to LP. Furthermore, OsGF14b, a 14-3-3 protein that acts as a key component in activating PM H⁺-ATPase for root elongation, is also involved in the qPE9-1 mediation. Moreover, the overexpression of OsGF14b in WYJ8 (carrying the qpe9-1 allele) partially increased primary root length under LP conditions. Experiments using R18 peptide (a 14-3-3 protein inhibitor) showed that qPE9-1 is important for primary root elongation and H⁺ efflux under LP conditions by involving the 14-3-3 protein. In addition, rhizosheath weight, total P content, and the rhizosheath soil Olsen-P concentration of qPE9-1 lines were higher than those of qpe9-1 lines under soil drying and LP conditions. These results suggest that the G protein γ subunit qPE9-1 in rice plants modulates root elongation for phosphorus uptake by involving the 14-3-3 protein OsGF14b and PM H⁺-ATPase, which is required for rice P use.