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81.
Water, Air, & Soil Pollution - The layered double hydroxides (LDHs) with a hydrotalcite-like structure are believed to possess great potentials as environmental remediation materials including... 相似文献
82.
Zhihong Xu Sally Ward Chengrong Chen Tim Blumfield Nina Prasolova Juxiu Liu 《Journal of Soils and Sediments》2008,8(2):99-105
Background, Aims, and Scope An improved understanding of important soil carbon (C) and nutrient pools as well as microbial activities in forest ecosystems
is required for developing effective forest management regimes underpinning forest productivity and sustainability. Forest
types and management practices can have significant impacts on soil C and nutrient pools as well as biological properties
in forest ecosystems. Soil C and nutrient pools were assessed for adjacent natural forest (NF), first rotation (1R) (50-year-old),
and second rotation (2R) (1-year-old) hoop pine (Araucaria cunninghamii Ait. ex D. Don) plantations in southeast Queensland of subtropical Australia.
Materials and Methods Five transects spaced 3 m apart with 9 sampling points along each transect were selected (9.6 m × 12.0 m each site), with
45 soil cores (7.5 cm in diameter) collected and separated into 0–10 and 10–20 cm depths. These soils were analysed for total
C, total nitrogen (N), C (δ13C) and N (δ15N) isotope composition. The 0–10 cm soils were analysed for pH, CEC, exchangeable cations, total P and total K, and assayed
for microbial biomass C and N, respiration, metabolic quotient, potential mineralizable N (PMN), gross N mineralization (M) and immobilization (I).
Results Total C and N in 0–10 cm soils were higher under NF and 1R plantation than under 2R plantation, while they were highest in
10–20 cm soils under NF, followed by the 1R and then 2R plantation. δ13C was lower under NF than under the plantations, while δ15N was higher under NF than under the plantations. Total P was the highest under NF, followed by the 1R and then 2R plantation,
while total K was higher under the 2R plantation. No significant differences were detected for pH, CEC, exchangeable cations,
microbial C and N, respiration and metabolic quotient among the 3 sites. PMN and M were higher under NF, while I was the highest under the 2R plantation, followed by the NF and then 1R plantation.
Discussion Soil total C and N in 0–10 cm depth were significantly lower under 2R hoop pine plantation than those under NF and 1R hoop
pine plantation. There were significant reductions in soil total C and N from NF to 1R and from 1R to 2R hoop pine plantations
in 10–20 cm depth. This highlights potential N deficiency in the 2R hoop pine plantations, and application of N fertilizers
may be required to improve the productivity of 2R hoop pine plantations.
There were no significant differences in other soil chemical and physical properties in 0–10 cm depth among the 3 sites under
NF, 1R and 2R hoop pine plantations, except for soil total P and K.
Soil microbial biomass C, CO2 respiration and metabolic quotient did not differ among the 3 sites assessed, perhaps mainly due to these biological variables
being too sensitive to variations in soil chemical and physical properties and thereby being associated with a larger variability
in the soil biological properties. However, soil potential mineralizable N, gross N mineralization and immobilization were
rather sensitive to the conversion of NF to hoop pine plantation and forest management practices.
Conclusions Total C and N in the top 20 cm soil were highest under NF, followed by 1R and then 2R hoop pine plantations, indicating that
N deficiency may become a growth-limiting factor in the 2R hoop pine plantations and subsequent rotations of hoop pine plantation.
The sample size for soil δ13C seems to be much smaller than those for soil total C and N as well as δ15N. The significant reductions in soil total P from NF to 1R and then from 1R to 2R hoop pine plantations highlight that P
deficiency might become another growth-limiting factor in the second and subsequent rotations of hoop pine plantations. Soil
microbial properties may be associated with large spatial variations due to these biological properties being too sensitive
to the variations in soil chemical and physical properties in these forest ecosystems.
Recommendations and Perspectives Soil potential mineralizable N, gross N mineralization and immobilization were useful indices of soil N availability in response
to forest types and management practices. The sampling size for soil δ13C was much smaller than the other soil chemical and biological properties due to the different patterns of spatial variation
in these soil properties. 相似文献
83.
两种真姬菇摇瓶发酵产生菌丝体及 胞外多糖研究 总被引:1,自引:0,他引:1
采用摇瓶培养法对2种真姬菇的发酵工艺进行研究,结果表明:真姬菇Ⅰ、Ⅱ发酵生产菌丝体及胞外多糖的碳源是葡萄糖,氮源是酵母膏;液体发酵培养基是葡萄糖3%、酵母膏 0.4%、vitB1 10mg/100ml、KH2PO4 0.1%、MgSO4 0.1%,pH值为6.0;液体发酵的优化条件是初始pH 6.0~7.0,振荡速度110~130r/min,培养温度25~28℃,装液量150ml/250ml。2种真姬菇菌丝体及胞外多糖产量较高,真姬菇Ⅰ菌丝体干重、胞外多糖产量分别是 3.92、8.83 mg /ml;真姬菇ⅠⅠ菌丝体干重、胞外多糖产量分别是3.25、7.69 mg /ml,即真姬菇Ⅰ摇瓶发酵菌丝体干重、胞外多糖产量高于真姬菇Ⅱ。 相似文献
84.
85.
86.
不同施肥水稻土可溶性有机氮组分差异及影响因素 总被引:3,自引:1,他引:3
可溶性有机氮(Soluble Organic Nitrogen,SON)在研究土壤供氮能力方面至关重要,而目前关于水田生态系统SON组成及其影响因素尚不清楚。运用红外光谱和氨基酸自动分析仪研究了长期(33年)不同施肥处理对水稻土SON含量、组分的影响及其主控因子。结果表明:单施化肥、化肥+牛粪、化肥+稻草处理土壤SON较不施肥处理提高23.49%、58.70%和106.30%,游离氨基酸氮提高32.27%、84.42%和95.21%,可溶性蛋白氮提高20.83%、70.00%和95.83%;不同施肥处理土壤游离氨基酸组成均以中性氨基酸占优势;土壤可溶性氮官能团组成均具有酰胺类化合物的红外特征吸收峰;RDA结果表明,土壤SON含量和组成差异明显,CK和NPK处理主要受土壤容重影响,而NPKM和NPKS则主要受有机质、全氮、微生物量氮、蛋白酶和谷氨酰胺酶影响。因此,SON含量和组分变化与施肥处理密切相关,长期添加有机肥能够显著增加土壤SON及其组分的含量,提高土壤供氮潜力。 相似文献
87.
Soil soluble organic nitrogen and active microbial characteristics under adjacent coniferous and broadleaf plantation forests 总被引:1,自引:0,他引:1
Shihe Xing Chengrong Chen Biqing Zhou Hui Zhang Zhongmin Nang Zihong Xu 《Journal of Soils and Sediments》2010,10(4):748-757
Purpose
Soil soluble organic nitrogen (SON) is considered as a sensitive indicator of soil nitrogen (N) status and plays an important role in N cycling in forest ecosystems. Most work on forest soil SON to date has been conducted in temperate areas. The information about soil SON pools and dynamics in tropical and subtropical areas is limited. The aim of this study was to investigate the effects of different forest types on soil SON availability and associated microbial properties. 相似文献88.
Linking soil bacterial diversity to ecosystem multifunctionality using backward-elimination boosted trees analysis 总被引:1,自引:0,他引:1
Background, aim, and scope
There is increasing evidence of linkages between biodiversity and ecosystem functions. Recent interests on this topic have expanded from an individual-function perspective to a multifunction perspective. This study aims to explore the soil bacterial diversity–multifunctionality relationship. 相似文献89.
Yuzhe Wang Lianwei Zhang Hong Yang Guijun Yan Zhihong Xu Chengrong Chen Dongke Zhang 《Journal of Soils and Sediments》2016,16(3):801-810
Purpose
Biochar has been suggested as a soil conditioner to improve soil fertility and crop productivity while simultaneously mitigate global climate change by storing carbon in the soil. This study investigated the effect of pine (Pinus radiata) biochar application on soil water availability, nitrogen (N) and carbon (C) pools and growth of C3 and C4 plants.Materials and methods
In a glasshouse pot trial, a pine biochar (untreated) and nutrient-enriched pine biochar were applied to a market garden soil with C3 (Spinacia oleracea L.) and C4 (Amaranthus paniculatus L.) plants at rates of 0, 1.0, 2.0, and 4.0 % (w/w). Plant biomass, soil pH, moisture content, water holding capacity (WHC), hot water extractable organic C (HWEOC), and total N (HWETN), total C and N, and their isotope compositions (δ 13C and δ 15N) of soils and plants were measured at the end of the experimentation.Results and discussion
The soil moisture content increased while plant biomass decreased with increasing untreated biochar application rates. The addition of nutrient-enriched biochar significantly improved plant biomass in comparison to the untreated biochar addition at most application rates. Biochar application also increased the levels of labile organic C and N pools as indicated by HWEOC and HWETN.Conclusions
The results suggested that the addition of pine biochar significantly improved soil water availability but not plant growth. The application of nutrient-enriched pine biochar demonstrated that the growth of C3 and C4 plants was governed by biochar nutrient availability rather than its water holding capacity under the pot trial condition.90.
Soil soluble organic nitrogen (SON) can play an important role in soil nitrogen (N) cycling in forest ecosystems. This study examined the effect of land-use change from a native forest (NF) to a first rotation (1R) and subsequent second rotation (2R) hoop pine (Araucaria cunninghamii) plantation on soil SON pools. The impact of residue management on SON pools was also investigated in the 2R forest, where SON was measured in tree rows (2R-T) and windrows (2R-W). Various extraction techniques were used to measure SON pool size in the 0-10, 10-20 and 20-30 cm layers of soil. The results showed that land-use change had a significant impact on soil SON pools. In the 0-10 cm layer, 3.2-8.7, 14-23, 20-28, 60-160 and 127-340 mg SON kg−1 were extracted by water, 0.5 M K2SO4, 2 M KCl, hot water and hot 2 M KCl, respectively. The size of the SON pools and the potential production of SON (PPSON) were generally highest in the NF soil and lowest in the 2R-T soil, and in all forest types decreased with soil depth. The larger SON pools in the NF soil coincided with lower soil, litter and root C:N ratios, suggesting that the difference in the size of SON pools between the NF and 1R soil may be related to differences in the quality of organic matter input under the different forest ecosystems. Differences in the size of SON pools between the 1R soil and the 2R soils and between the 2R-T soil and the 2R-W soil may be related to the quantity of organic matter input and time since disturbance. Significant relationships were found between the SON extracted by 0.5 M K2SO4 (SONps) and 2 M KCl (SONKCl), and also among the SON extracted by hot 2 M KCl (SONhKCl), hot water (SONhw) and water (SONw), suggesting that the organic N released by these groups of extracts may be at least partly from similar pools. 相似文献