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岷江干旱河谷-山地森林交错带根层土壤碳活性与储量特征 被引量:2
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作者 刘彬 鞠佳伶 +4 位作者 罗承德 刘牧 张健 白景文 雷波 《水土保持学报》 CSCD 北大核心 2012年第2期121-126,共6页
根层土受植物地下部分生命活动、代谢影响最直接和最强烈,其碳活性与储量特征对土壤质量改变乃至全球气候变化具有极高的灵敏性。以岷江干旱河谷-山地森林交错带及邻近生态系统为研究对象,研究根层土壤易氧化碳、微生物量碳等碳活性以... 根层土受植物地下部分生命活动、代谢影响最直接和最强烈,其碳活性与储量特征对土壤质量改变乃至全球气候变化具有极高的灵敏性。以岷江干旱河谷-山地森林交错带及邻近生态系统为研究对象,研究根层土壤易氧化碳、微生物量碳等碳活性以及碳密度、碳储量特征,可为该区的生态系统管理提供重要科学依据。结果表明,不同生态类型根层土的土壤碳密度为(0.14±0.007)~(101.16±0.301)kgC/m2,碳储量为(30.2±1.51)~(21850.6±65.02)kg。相对于干旱河谷,交错带根层土壤易氧化碳、微生物量碳等碳活性更强,为沿交错带逐步向下改善土壤环境抑制干旱河谷区上延提供了较好的碳素环境。尽管交错带天然林植被面积较小,但其土壤碳密度和土壤有机碳丰度指数因物种优势和所在山地垂直带谱中所处的相对有利位置,显著高于干旱河谷。在交错带内部,以高山栎为优势种的根层土具有更强的储碳能力,是包括退耕还林地在内的自然或人工植被调控生态工程建设中重要造林树种和恢复模式。 展开更多
关键词 岷江干旱河谷-山地森林交错带 根层土 碳活性 碳密度 碳储量
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Phosphorus fertilizer induced changes in the soil available P,the P nutrition and the growth of Pinus radiata seedlings grown in association with understory 被引量:1
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作者 Achmad Arivin Rivaie Russ Williams Tillman 《Journal of Forestry Research》 SCIE CAS CSCD 2010年第2期129-136,I0003,共9页
A study was carried out to investigate changes in the soil plant-available P,the P nutrition and the growth of Pinus radiata seedlings grown in association with understory,broom(Cytisus scoparius L.) or ryegrass(Lo... A study was carried out to investigate changes in the soil plant-available P,the P nutrition and the growth of Pinus radiata seedlings grown in association with understory,broom(Cytisus scoparius L.) or ryegrass(Lolium multiflorum) on Orthic Allophanic Soil,following the application of three rates of triple superphosphate(TSP)(0,50,and 100 mg·kg^-1P) under a glasshouse condition.The application of P fertilizer enhanced P availability in the rhizospheric of radiata seedlings and the bulk soils in a P-deficient site.P availability in the rhizospheric soils of ryegrass and broom,grown in association with radiata,were also increased by the presence of radiata roots.P concentrations in new shoot needles,old shoot needles,stem and roots of radiata pine increased with increase rates of TSP application,but the effects of ryegrass and broom on P nutrition of radiata seedlings depended on the soil P status.In the absence of P fertilizer addition(control treatment),P concentrations in new shoot needles,old shoot needles,stem,and roots of radiata grown in association with broom were higher than those with ryegrass,whereas,when P fertilizer was added(50 and 100 mg·kg^-1) the P concentration was lower.This is probably related to the growth of broom that may have removed much of the plant-available P in the soil as indicated by the consistently lower Bray-2 P concentration in the rhizosphere soil of radiata in association with broom than that in the rhizosphere soil of radiata in association with grass at the two high P rates.Furthermore,in the high P fertile soil(application rate of 100 mg·kg^-1),the dry matter yield of radiata was lower when it was grown with broom than with ryegrass.This result suggests that in moderate to high P fertile soils,P.radiata seedlings grow better with ryegrass than with broom,because broom grows vigorously in high P fertile soil and competes with P.radiata for P and perhaps for other nutrients as well. 展开更多
关键词 phosphorus fertilizer Pinus radiata UNDERSTORY RHIZOSPHERE soil available P P nutrition plant growth
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Influence of Ice on Soil Elemental Characterization via Portable X-Ray Fluorescence Spectrometry 被引量:4
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作者 D.C.WEINDORF N.BAKR +6 位作者 Y.ZHU A.MCWHIRT C.L.PING G.MICHAELSON C.NELSON K.SHOOK S.NUSS 《Pedosphere》 SCIE CAS CSCD 2014年第1期1-12,共12页
Field portable X-ray fluorescence (PXRF) spectrometry has become an increasingly popular technique for in-situ elemental characterization of soils. The technique is fast, portable, and accurate, requiring minimal sa... Field portable X-ray fluorescence (PXRF) spectrometry has become an increasingly popular technique for in-situ elemental characterization of soils. The technique is fast, portable, and accurate, requiring minimal sample preparation and no consumables. However, soil moisture 〉 20% has been known to cause fluorescence denudation and error in elemental reporting and few studies have evaluated the presence of soil moisture in solid form as ice. Gelisols (USDA Soil Taxonomy), permafrost-affected soils, cover a large amount of the land surface in the northern and southern hemispheres. Thus, the applicability of PXRF in those areas requires further investigation. PXRF was used to scan the elemental composition (Ba, Ca, Cr, Fe, K, Mn, Pb, Rb, Sr, Ti, Zn, and Zr) of 13 pedons in central and northern Alaska, USA. Four types of scans were completed: 1) in-situ frozen soil, 2) re-frozen soil in the laboratory, 3) melted soil/water mixture in the laboratory, and 4) moisture-corrected soil. All were then compared to oven dry soil scans. Results showed that the majority of PXRF readings from in-situ, re-frozen, and melted samples were significantly underestimated, compared to the readings on oven dry samples, owing to the interference expected by moisture. However, when the moisture contents were divided into 〉 40% and 〈 40〈 groups, the PXRF readings under different scanning conditions performed better in the group with 〈 40% moisture contents. Most elements of the scans on the melted samples with 〈 40% moisture contents acceptably compared to those of the dry samples, with R2 values ranging from 0.446 (Mn) to 0.930 (St). However, underestimation of the melted samples was still quite apparent. Moisture-corrected sample PXRF readings provided the best correlation to those of the dry, ground samples as indicated by higher R2 values, lower root mean square errors (RMSEs), and slopes closer to 1 in linear regression equations. However, the in-situ (frozen) sample scans did not differ appreciably from the melted sample scans in their correlations to dry sample scans in terms of R2 values (0.81 vs. 0.88), RMSEs (1.06 vs. 0.85), and slopes (0.88 vs. 0.92). Notably, all of those relationships improved for the group with moisture contents 〈 40%. 展开更多
关键词 Gelisols MOISTURE PERMAFROST proximal sensing regression
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