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1.
半干旱沙区退耕还林对碳储量和分配格局的影响   总被引:7,自引:1,他引:6  
以农田和不同退耕还林年限(5、10、15年)的杨树人工林为对象,开展了退耕还林对生态系统有机碳储量和分配格局特征的研究。结果表明:随着退耕年限的增加,生物量碳储量不断积累,且其增加的碳库主要分配在树干。与农田(CK1)相比,退耕还林5年的杨树人工林(Poplarl)0~10、10~20、20~40和40~60cm土壤有机碳含量分别下降了7.65%、36.66%、51.94%和21.4%;退耕还林10年的杨树人工林(Poplar2),不同层次土壤有机碳含量分别提高了69.63%、62.46%、17.07%和66.94%。与农田(CK2)相比退耕还林15年的杨树人工林(Poplar3),0~10、20~40和40~60cm土壤有机碳含量分别提高了31.96%、81.50%和58.05%,而10~20cm土层下降了13.38%。与对照农田相比,5年生杨树人工林0~60cm土壤有机碳储量下降了31%,而10年和15年生杨树人工林土壤有机碳储量分别增加了47%和41%。退耕5年的杨树人工林总的碳储量比对照农田下降了10%,退耕10年和15年的杨树人工林与相应对照农田相比较,生态系统总的碳储量分别提高大约2倍和5倍。说明,农田退耕还林后生态系统碳储量明显增加,增加的碳储量主要积累在地上生物量碳库中。退耕还林初期,土壤有机碳储量表现出下降趋势,随后逐渐恢复甚至高于农田土壤碳储量。  相似文献   

2.
晋西北黄土高原丘陵区不同土地利用方式下土壤碳氮储量   总被引:14,自引:1,他引:13  
对晋西北黄土高原丘陵区杨树-小叶锦鸡儿人工林、小叶锦鸡儿人工灌丛、杨树人工林、撂荒地和农田5种土地利用方式下土壤碳氮储量进行研究.结果表明: 不同土地利用方式下土壤碳氮含量、碳氮密度和碳氮储量存在显著差异.5种土地利用方式0~20 cm表层土壤碳氮含量和碳氮密度均显著大于20~40 cm和40~60 cm土层.5种土地利用方式同一土层碳氮含量和碳氮密度大小为: 杨树-小叶锦鸡儿人工林>小叶锦鸡儿人工灌丛>杨树人工林>撂荒地>农田;0~60 cm土层土壤有机碳储量大小为:杨树-小-叶锦鸡儿人工林(30.09 t·hm-2)>小叶锦鸡儿人工灌丛(24.78 t·hm-2)>杨树人工林(24.14 t·hm-2)>撂荒地(22.06 t·hm-2)>农田(17.59 t·hm-2);土壤氮储量与有机碳储量变化规律相似,杨树-小叶锦鸡儿人工林0~60 cm土层土壤氮储量(4.94 t·hm-2)最高,其次是小叶锦鸡儿人工灌丛(3.53 t·hm-2)、杨树人工林(3.51 t·hm-2)和撂荒地(3.40 t·hm-2),农田土壤氮储量(2.71 t·hm-2)最低.杨树-小叶锦鸡儿人工林和小叶锦鸡儿人工灌丛是晋西北黄土高原丘陵区植被建设和生态恢复过程中较好的两种土地利用方式.  相似文献   

3.
土壤碳(C)、氮(N)、磷(P)化学计量是衡量土壤质量及生态系统元素限制的重要指标,探讨土地利用和土层深度对土壤化学计量特征的影响有利于揭示科尔沁沙地土壤元素循环规律。本研究以科尔沁沙地5种土地利用类型(灌溉农田、旱作农田、沙质草地、固定沙丘、流动沙丘)土壤为对象,分析不同土地利用类型和不同土层土壤有机碳(SOC)、全氮(TN)、全磷(TP)含量及其化学计量特征。结果表明: 1)科尔沁沙地0~10 cm SOC(3.23 g·kg-1)、TN(0.37 g·kg-1)、TP(0.15 g·kg-1)含量及化学计量比(C:N、C:P、N:P分别为9.07、25.56、2.97)远低于中国陆地土壤。2)土地利用变化显著改变了SOC、TN、TP含量及其化学计量特征,0~100 cm SOC、TN、TP含量均表现为灌溉农田>沙质草地>旱作农田>固定沙丘>流动沙丘;沙质草地、灌溉农田、旱作农田C:N显著高于固定沙丘和流动沙丘,沙质草地、固定沙丘、灌溉农田、旱作农田C:P显著高于流动沙丘,5种土地利用类型N:P无显著差异。3)随土层深度增加,沙质草地、固定沙丘、灌溉农田、旱作农田SOC和TN含量显著降低,流动沙丘SOC、TN含量和C:P在各土层间无显著差异;总体上,各土地利用类型TP含量和C:N受土层影响较小;沙质草地、固定沙丘、灌溉农田、旱作农田C:P和沙质草地N:P随土层深度增加而降低。4)SOC、TN、TP、C:N与中砂粒、细砂粒、土壤容重呈显著负相关,与黏粉粒和极细砂粒呈显著正相关。沙漠化导致科尔沁沙地SOC和养分流失,加剧土壤N缺乏,水肥投入有助于耕地维持相对较高的土壤养分水平。  相似文献   

4.
为正确认识桉树(Eucalyptus spp.)人工林凋落物和土壤C、N、P时空分配格局及两者间的关系,对5个林龄尾巨桉林分凋落物及土壤C、N、P含量及化学计量比进行测定分析。结果表明,凋落物的C含量均显著大于土壤,且不同林龄间凋落物C含量无显著差异,1年生人工林土壤表层(0~20 cm)的C含量显著小于3~7年生,其他土层C含量在不同林龄间差异不显著。凋落物的N含量均显著高于土壤,且1年生人工林显著大于其他林龄的,而土壤表层的N含量以7年生人工林最大,1年生的最小。凋落物的P含量除1年生人工林显著大于3年生外,其他林龄间均无显著差异,土壤的P含量在不同林龄间的差异均不显著。凋落物C∶N随林龄呈逐渐增大趋势,且显著大于土壤层。凋落物的C∶P和N∶P在不同林龄间的差异不显著,但均显著大于土壤层。凋落物的N含量与表层土壤的C、N含量呈极显著负相关,凋落物的C∶N与表层土壤的C∶P,N∶P呈显著正相关,表层土壤C、N积累受到凋落物N的制约。因此,在桉树人工林经营管理过程中如何降低凋落物分解的N限制性、提高养分传递效率及合理施肥显得十分重要。  相似文献   

5.
降水格局是影响陆地生态系统结构和过程的重要环境要素,尤其对于干旱/半干旱地区,降水变化是植物生长驱动的关键生态因子。目前,针对降水变化对陆地生态系统C、N、P等元素生物地球化学循环过程影响开展了大量研究。然而,关于沙地樟子松重要引种地科尔沁沙地自然降水梯度下沙地樟子松人工林土壤、植物生态化学计量特征的研究未见报道。因此,本研究以樟子松原产地红花尔基和引种地科尔沁沙地自然降水梯度下4个典型沙地樟子松人工林为对象,研究樟子松引种地降水变化对土壤(0—10,10—20 cm和20—40 cm)和植物(1年和2年生叶)生态化学计量特征的影响。研究结果发现:(1)与红花尔基原产地樟子松人工林相比,科尔沁沙地引种的樟子松人工林土壤C、N、P元素含量显著降低;(2)科尔沁沙地自西向东,随降水量增加,沙地樟子松人工林土壤C、N、P含量以及C∶P和N∶P表现为逐渐增加趋势,而土壤C∶N呈减少趋势;(3)随着降水量增加,樟子松叶C含量呈下降趋势,叶N含量和N∶P比值呈增加趋势,植物叶P含量无一致性规律;(4)樟子松叶片P含量与土壤C、N、P含量呈极显著正相关关系,而叶片C和N含量与土壤C、N、P含量无显著相关性。研究表明,沙地樟子松引种地科尔沁沙地土壤C、N、P养分比较缺乏,且随着降水增加土壤N养分限制降低,而土壤P养分限制增加。本研究从生态化学计量特征角度,为今后开展科尔沁沙地不同降水梯度条件下引种樟子松人工林提供理论依据。  相似文献   

6.
河西走廊中段绿洲退化土地退耕种植苜蓿的固碳效应   总被引:4,自引:0,他引:4  
苏永中  刘文杰  杨荣  范桂萍 《生态学报》2009,29(12):6385-6391
土地利用变化和耕作管理是人类影响陆地生态系统碳过程一个重要方面.对河西走廊中段张掖绿洲退化土地退耕种植苜蓿5a后土壤性状的分析表明, 49个退耕苜蓿地土壤与相邻未退耕农田土壤配对样本的比较,退耕苜蓿地0~15cm土层土壤粒级组成和容重并未发生显著变化,但土壤pH平均提高了0.11个单位,电导率降低34.8%,土壤有机碳(SOC)和全氮(全N)含量较对照农田土壤平均提高18.5%和9.3%,活性有机碳(labile C)增加53.3%.SOC含量受海拔高度和土壤粒粉粒含量的影响,退耕后SOC和全N的增加幅度沙壤土高于粉壤土,而labile C的增加幅度沙壤土低于粉壤土.退耕苜蓿地0~15cm土层SOC和全N储量较农田土壤分别增加2.84Mg hm~(-2)和0.21Mg hm~(-2),土壤C、N的固存率平均为0.57Mg hm~(-2)a~(-1)和0.04 Mg hm~(-2)a~(-1),表明退化土地由1年生作物向多年生牧草的转变有显著的固碳效应和潜力.活性有机碳的变化较总有机碳的变化更为显著,表明活性有机碳对土地利用变化的响应更为敏感.  相似文献   

7.
岷江干旱河谷区岷江柏人工林碳氮储量随林龄的动态   总被引:1,自引:0,他引:1  
研究了岷江干旱河谷区不同林龄岷江柏人工林生态系统碳氮储量及其分配特征.结果表明:岷江柏不同器官的碳含量相对稳定,氮含量则与器官类型密切相关,而土壤有机碳和氮含量均随着人工林林龄的增长而增加.岷江柏人工林植被层、土壤层以及生态系统的碳氮储量随着林龄的增长总体呈增加趋势.13、11、8、6和4年生岷江柏人工林生态系统总碳储量分别为190.90、165.91、144.57、119.44和113.49 t·hm-2,总氮储量分别为19.09、17.97、13.82、13.42和12.26 t·hm-2.岷江柏人工林生态系统碳氮大部分储存于0~60 cm土层,分别占生态系统总储量的92.8%和98.8%,且主要集中于0~20 cm土层,5个林龄平均碳氮储量分别为74.13和7.40 t·hm-2,分别占其平均土壤总碳氮储量(0~60 cm)的54.4%和48.9%.植被层有机碳和氮储量的分配不同,碳储量在乔木层(3.7%)的分配高于林下植被层(3.5%),而氮储量在乔木层(0.5%)的分配低于林下植被层(0.7%).不同林龄岷江柏人工林碳氮储量及其空间分布变化明显,且在此年龄段内,岷江柏人工林生态系统能够持续积累有机碳和氮.  相似文献   

8.
豫西黄土丘陵区不同林龄栎类和侧柏人工林碳、氮储量   总被引:2,自引:0,他引:2  
利用空间代替时间样地调查法,分析了豫西黄土丘陵区栎类和侧柏人工林生态系统碳、氮储量的分布格局,以及不同土层碳储量和氮储量随林龄的动态变化.结果表明:随着树龄的增加,两类人工林乔木层和枯落物层碳储量均增加,土壤碳储量和氮储量主要在表层(0~20 cm)汇聚,且各土层碳储量和氮储量随着林龄增加表现为减少-增加-减少的趋势.各林龄栎类人工林土壤表层碳、氮储量分别为20.31~50.07和1.68~2.12 t·hm-2;不同林龄侧柏人工林土壤表层碳、氮储量分别为23.99~48.76和1.59~2.34 t·hm-2;各林龄栎类和侧柏人工林生态系统的碳储量分别为52.04~275.82和62.18~279.81 t·hm-2;侧柏人工林碳汇能力略高于栎类人工林.土壤C/N随着造林年限的增加呈增加趋势.  相似文献   

9.
量化橡胶树和桉树人工林碳储量,为评价海南地区碳汇功能和可持续管理功能提供重要依据。在海南省儋州市选择不同林龄的橡胶树和桉树人工林,设置样地测算乔木层、林下植被和枯落物的生物量,土壤分层采集0—100cm土样,依据相对方程,计算橡胶树和桉树人工林生态系统的碳含量和碳储量。结果表明:不同林龄橡胶树和桉树人工林林下植被碳含量变化幅度为38.09%—45.31%,枯落物碳含量为38.50%—47.52%之间。0—100 cm土层碳含量变化幅度为0.31%—1.62%,各林分土壤含碳率均随土层深度增加而减少,除底层(50—100cm)土壤外,其它层次不同林分土壤有机碳的含量均表现为橡胶林桉树林。橡胶树、桉树人工林生态系统总碳储量分别为160.01和86.33 t C·hm~(-2),桉树人工林生态系统碳储量均表现为随林龄的增加而增加,橡胶树各林龄碳储量均高于桉树。橡胶树、桉树人工林乔木碳储量分别占其总碳储量的36.87%和23.92%。橡胶树和桉树人工林下植被碳储量表现为橡胶树(0.78 t C·hm~(-2))桉树(0.49 t C·hm~(-2)),枯落物碳储量分别占其总碳储量的1.00%和1.56%。橡胶树、桉树人工林土壤碳储量分别为96.22和63.88 t C·hm~(-2),橡胶树人工林土壤碳储量高于桉树,0—50 cm土层碳储量成为土壤的主体,橡胶树0—50 cm土层碳储量占其土壤总碳储量的64.39%,桉树为54.35%。乔木层和土壤层碳储量是整个森林生态系统碳贮量的主要部分。橡胶人工林生态系统的固碳速率和固碳潜力分别为4.20 t C·hm~(-2)·a~(-1)和64.78 t C·hm~(-2),桉树人工林生态系统的固碳速率和固碳潜力分别为11.06 t C·hm~(-2)·a~(-1)和23.98 t C·hm~(-2)。两个树种均具有较高的固碳能力,是海南营造高效固碳人工林的理想树种。  相似文献   

10.
靖磊  周延  吕偲  赵君茹  雷光春 《生态学报》2018,38(18):6530-6538
选取洞庭湖洲滩湿地挖沟抬垄造林的6林龄、9林龄和13林龄杨树人工纯林为研究对象,通过比较不同林龄杨树叶及沟垄土壤的C、N、P含量差异,研究湿地杨树人工林不同生长阶段养分元素的分配格局及生态化学计量学特征,揭示杨树种植对洞庭湖湿地生态系统的影响。结果显示,叶N、叶P以及C∶P和N∶P与林龄显著相关,但叶C和C∶N与林龄不相关。3个林龄杨树人工林叶N∶P均大于16,说明P是限制洞庭湖杨树生长发育的主要因子,9林龄叶P量显著低于6林龄和13林龄,而N∶P和C∶P则显著高于6林龄和13林龄,说明P的限制在9林龄尤为显著。3个林龄湿地杨树人工林树垄和树沟土壤有机C、全N和C∶N呈现出与林龄和土层深度的负相关关系,但全P与两者没有显著关系。C∶P在树垄样地中呈现出与林龄和土层深度的负相关关系,而在树沟样地中呈现出与土层深度的正相关关系,与林龄无显著关系。N∶P在9林龄和13林龄树垄样地和6林龄树沟样地中与土层深度呈负相关关系,说明挖沟抬垄造林方式不利于土壤有机C和全N的积累,也不利于维持洞庭湖湿地土壤的肥力。  相似文献   

11.
The cell has been represented as a charged liquid drop. Contrary to the DLVO-theory, the effect of the surface potential upon the value of the interfacial tension of the cell membrane has also been taken into consideration. The cell membrane has visco-elastic properties and its constituents may move against each other. Cell movement is caused by the appearance of a small number of the electrically charged constituents of the cell membrane on the leading edge of the cell. This produces a local decrease in the surface tension and the cell membrane expansion. At the moment of contact between two cells proton transfers occur between the strongly negatively charged microvilli of one cell and the body of the other, analogous to a condenser breakdown. This, through the effect on the surface tension, causes contact inhibition of movement. The distribution of the proton dissociable groups modifies the interaction between the cells (differentiation) and between the cell and the substratum (adhesion). Adsorption of the charged compounds at the surface of the cell membrane, decreasing the surface potential and increasing the surface tension, causes the phenomena of chemotaxis, phagocytosis and pinocytosis. Cell division, considered in the terms of the surface energy, requires an adequate supply of considerable quantities of energy inversely proportional to the surface potential value. In case of a reduction of the distance between the cells, their surface potential and the energetic barrier of the cell division processes increases, and causes contact inhibition of cell division. Due to their high charge, division of neoplastic cells is inhibited much later than division of normal cells, or is completely ininhibited due to geometric conditions. Fusion of the cell membrane in the intra-cellular and intercellular processes is a reverse process in relation to the cell division.  相似文献   

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The effect of age and gender on major, minor, and trace element contents in the intact rib bone of 80 relatively healthy 15–55-year-old women and men was investigated. Contents or upper limit of contents of 16 chemical elements in the rib bone were determined by inductively coupled plasma atomic emission spectrometry (ICP-AES). Mean values (M?±?SΕΜ) for the mass fraction of Ba, Ca, Cu, Fe, K, Li, Mg, Na, P, S, Sr, and Zn (milligram per kilogram of dry bone) were as follows: 2.54?±?0.16, 171,400?±?4,050, 1.35?±?0.22, 140?±?11, 1,874?±?71, 0.049?±?0.011, 2,139?±?38, 5,378?±?88, 75,140?±?1,660, 1,881?±?51, 291?±?20, and 92.8?±?1.5, respectively. The upper limits of contents of Al, B, Mn, and V were <7.20, <0.65, <0.36, and <0.03, respectively. Statistically significant tendency for the Ca, Mg, and P content to decrease with age was found in the human rib bone, regardless of gender. The mass fraction of Fe in the male rib bone increases with age. It was shown that higher Ca, Mg, Na, P, and Sr mass fractions as well as lower Fe content were typical of female ribs as compared to those in male ribs.  相似文献   

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Summary Concentration of N, P, K, Ca, Mg and S in summer groundnut crop was higher than in kharif while Zn, Fe, Mn and Cu contents were higher in summer crop. Kernel's N, P and Zn; Leaflet's Ca and Mn; Stem's K and Fe; Root's S and Cu and Petiole's Mg contents were highest. Shell's N, P, K, Mg, S, Zn and Cu; Kernel's Ca, Fe and Mn contents were the least. N, P, K, S, Zn and Cu concentrations decreased linearly as the crop grew. Ca, Mg, Fe and Mn concentrations did not display any distinct pattern. Ca concentration was positively correlated with pod yield in both the seasons.  相似文献   

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2-Dimethylaminomethylene-1-benzosuberone 1 was coupled with diazotized aniline derivatives to afford a series of the hitherto unreported 2-arylazo-1-benzosuberones 3ai. The tautomeric structure and the effect of substituents on the tautomeric form (s) of the products 3ai were discussed. Similar coupling of the enaminone 1 with diazonium salts of heterocyclic amines gave the respective fused azolotriazino-benzosuberones. Some of the newly synthesized compounds showed potent antimicrobial, anti-HCV, antioxidant, antitumor (as topoisomerase I inhibitors), and antimicrobial activities.  相似文献   

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DNA methylation analyses usually require a preceding bisulfite conversion of the DNA. The choice of an appropriate kit for a specific application should be based on the specific performance requirements with regard to the respective sample material. In this study, the performance of nine kits was evaluated: EpiTect Fast FFPE Bisulfite Kit, EpiTect Bisulfite Kit, EpiTect Fast DNA Bisulfite Kit (Qiagen), EZ DNA Methylation-Gold Kit, EZ DNA Methylation-Direct Kit, EZ DNA Methylation-Lightning Kit (Zymo Research), innuCONVERT Bisulfite All-In-One Kit, innuCONVERT Bisulfite Basic Kit, innuCONVERT Bisulfite Body Fluids Kit (Analytik Jena). The kit performance was compared with regard to DNA yield, DNA degradation, DNA purity, conversion efficiency, stability and handling using qPCR, UV, clone sequencing, HPLC, and agarose gel electrophoresis. All kits yielded highly pure DNA suitable for PCR analyses without PCR inhibition. Significantly higher yields were obtained when using the EZ DNA Methylation-Gold Kit and the innuCONVERT Bisulfite kits. Conversion efficiency ranged from 98.7% (EpiTect Bisulfite Kit) to 99.9% (EZ DNA Methylation-Direct Kit). The inappropriate conversion of methylated cytosines to thymines varied between 0.9% (innuCONVERT Bisulfite kits) and 2.7% (EZ DNA Methylation-Direct Kit). Time-to-result ranged from 131 min (innuCONVERT kits) to 402 min (EpiTect Bisulfite Kit). Hands-on-time was between 66 min (EZ DNA Methylation-Lightning Kit) and 104 min (EpiTect Fast FFPE and Fast DNA Bisulfite kits). Highest yields from formalin-fixed and paraffin-embedded (FFPE) tissue sections without prior extraction were obtained using the innuCONVERT Bisulfite All-In-One Kit while the EZ DNA Methylation-Direct Kit yielded DNA with only low PCR-amplifiability. The innuCONVERT Bisulfite All-In-One Kit exhibited the highest versatility regarding different input sample materials (extracted DNA, tissue, FFPE tissue, cell lines, urine sediment, and cellular fractions of bronchial aspirates, pleural effusions, ascites). The innuCONVERT Bisulfite Body Fluids Kit allowed for the analysis of 3 ml plasma, serum, ascites, pleural effusions and urine.  相似文献   

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