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1.
《西部林业科学》2017,(1)
以三峡库区柏木纯林和柏木青冈混交林为研究对象,研究不同林分类型柏木林土壤有机碳与土壤呼吸特征。结果表明,柏木青冈混交林土壤各土层(0~20cm,20~40cm,40~60cm)的总有机碳、微生物生物量碳、易氧化有机碳及水溶性有机碳含量均极显著高于柏木纯林;混交林土壤各土层转化酶活性总体上均显著高于柏木纯林,但2种林分之间的土壤C/N无显著性差异;柏木青冈混交林各土层土壤呼吸强度分别比柏木纯林高出22.3%、18.3%、5.3%;各林分土壤有机碳、转化酶活性、C/N均与土壤呼吸强度存在显著的相关性。可见,与柏木纯林相比,柏木青冈混交林具有更大的有机碳储量,表现出更强的土壤固碳能力。 相似文献
2.
《西部林业科学》2019,(5)
以戴云山自然保护区毛竹向杉木林扩张形成的3种林分:杉木林、毛竹-杉木混交林和毛竹林为对象,测定其土壤易氧化态碳、土壤水溶性有机碳和土壤微生物量碳的含量,研究毛竹扩张对林分土壤活性有机碳和碳库管理指数的影响。研究结果表明:(1)3种林分8月和1月土壤易氧化态碳、土壤水溶性有机碳和土壤微生物量碳含量均随土层加深逐渐降低,表现出明显表层富集现象。各土层8月土壤易氧化态碳含量均比1月低,土壤微生物量碳含量则相反。3个土层土壤易氧化态碳含量排序为杉木林毛杉混交林毛竹林;(2)3种林分土壤微生物量碳、土壤易氧化态碳和土壤水溶性有机碳储量基本随土层深度增加呈递减趋势,0-60cm土层土壤水溶性有机碳和易氧化态碳储量均为杉木林毛杉混交林毛竹林,土壤微生物量碳储量则相反,3种林分间差异均未达到显著水平;(3)0-60cm土层3种林分土壤碳库活度和碳库活度指数基本为杉木林毛杉混交林毛竹林,土壤碳库指数为杉木林毛杉混交林毛竹林,土壤碳库管理指数为毛竹林毛杉混交林杉木林。研究表明,毛竹向杉木林扩张有利于土壤质量改善,但杉木林演替成毛竹纯林后对土壤质量长期影响,则需要进一步深入研究。 相似文献
3.
《林业勘察设计》2016,(3)
在福建省宁化国有林场开展了9年生杉木、木荷纯林及其不同混交比例林分生物量和碳储量的研究。结果表明,相对于杉木纯林,混交林干和根生物量的比例增加,枝和叶生物量的比例降低。5杉5荷林分总生物量分别比杉木和木荷纯林高25.8%和69.3%,7杉3荷和3杉7荷林分总生物量与杉木纯林接近,但分别比木荷纯林高41.2%和35.7%。7杉3荷、5杉5荷和3杉7荷混交林林分总碳储量分别比杉木纯林增加10.1%、22.2%和3.4%,比木荷纯林增加33.5%、48.3%和25.3%;碳储量的增加主要来源于乔木层和土壤层,灌木层、草本层和凋落物层碳储量与纯林差异不大。因此,相对于杉木或木荷纯林,5杉5荷混交可以显著提高林分生物量和碳储量。 相似文献
4.
为了分析不同林分类型的防护林对土壤理化性质的影响,以辽宁省泥质海岸5种不同类型防护林为研究对象,分析并得出了不同林分类型的防护林对土壤速效氮、速效磷、pH值、总孔隙度、体积含水量、土壤密度的影响,结果表明:防护林不同类型林分对土壤的理论性质有显著影响,其中速效氮含量的依次为刺槐纯林>辽宁杨纯林>小胡杨+紫穗槐混交林>刺槐+杨树混交林>小胡杨纯林,刺槐纯林和辽宁杨纯林与空白对照组存在显著差异;对土壤pH值影响的程度由大至小排列为辽宁杨纯林>小胡杨+紫穗槐混交林>小胡杨纯林>刺槐+杨树混交林>刺槐纯林,各林分与对照组均存在极其显著差异;对土壤速效磷含量影响的程度由大至小排列为辽宁杨纯林>小胡杨+紫穗槐混交林>小胡杨纯林>刺槐+杨树混交林>刺槐纯林,与对照组均存在极其显著影响,以辽宁杨纯林、小胡杨+紫穗槐混交林、小胡杨纯林的影响最为显著;对土壤孔隙度影响的程度由大至小排列为刺槐纯林>辽宁杨纯林>小胡杨纯林>刺槐+杨树混交林>小胡杨+紫穗槐混交林;刺槐+杨树混交林、辽宁杨纯林对土壤含水量的影响最为显著;刺槐纯林、辽宁杨纯林、小胡杨纯林对土壤密度影响效果最为显著。 相似文献
5.
为研究辽西地区人工林对石灰性褐土土壤质量的定向改良作用,以油松×沙棘混交林、山杏纯林、油松纯林3种人工林地为研究对象,对在石灰性褐土上的人工林土壤肥力进行了分析。结果表明,油松沙棘混交林能够显著提高有机碳含量,比荒地高42.8%;油松沙棘混交林、油松纯林土壤碱解氮分别比荒地增加34.6%和33.6%,人工林对土壤全氮含量影响不显著;油松沙棘混交林的土壤速效磷和水溶性磷分别比荒地提高14.9%和128.57%;人工林增加了土壤速效钾含量;林木的改良土壤作用主要表现在土壤表层。 相似文献
6.
《西部林业科学》2017,(4)
以宁夏中部干旱带罗山山地系统的4个典型植被类型(青海云杉纯林、针阔混交林、浅山灌丛和干旱草地)为研究对象,测定0~10cm、10~20cm、20~40cm土层土壤活性有机碳组分(土壤的微生物量碳、颗粒有机碳和易氧化有机碳),探讨其分布规律和影响因素。结果表明,不同植被类型间土壤活性有机碳含量有显著差异(p0.05),各植被类型的土壤微生物量碳和颗粒有机碳含量的排序为乔木林(青海云杉纯林、针阔混交林)浅山灌丛干旱草地;随着土层深度增加,土壤微生物量碳和颗粒有机碳含量逐渐减少(p0.05),而易氧化有机碳含量在10~20cm土层最高。相关性分析表明,土壤微生物量碳、颗粒有机碳均与土壤总有机碳、全氮有极显著的正相关,而与pH值、含水率、C/N的相关性不显著,土壤易氧化有机碳与土壤理化性质的相关性均不显著。这表明作为土壤有机质和氮素来源的植被,其组成差异会对土壤有机碳组分具有重要影响。 相似文献
7.
何立新 《中南林业科技大学学报(自然科学版)》1998,(1)
以湘中丘陵区石栎马尾松混交林和马尾松纯林为研究对象,对两类林分进行了生物量和封理化性质的测定分析,结果表明:混交林林分生物量远高于马尾松纯林,是纯林的2.99倍;混交林乔木层生物量也高于纯林;混交林林分平均净生产力高于纯林,是纯林的3.62倍;混交林和纯林的根系总质量分别占林分生物量的9.76%和11.08%.在各级根中,两类林分均以粗根所占比例最大,细根所占比例最小,根系质量均随深度的增加而递减;混交林枝叶比略小于纯林,而枝叶指数、冠根比及光合部分与非光合部分比值则相反;混交林土壤营养元素含量显著高于马尾松纯林,但混交林土壤容重比纯林低,总孔隙度与毛管孔隙度、非毛管孔隙度比纯林林地高,本研究结果,为湘中丘陵区石栎马尾松混交林及马尾松纯林的培育提供了重要参考依据。 相似文献
8.
本文对山杜英纯林、杉木山社英混交林,杉木纯林的林分燃烧性进行了定量测定与分析,有明：山杜英纯林与杉木山杜英混交林的林内湿度、地被物及表层土壤的含水率均高于杉木纯林;林内易燃危险物数量减少,且是间竭式分布,易燃危险物的生物量与有效潜在能量占林分总物生量与总潜在能量的比率均明显低于杉木纯林。营造杉木山杜英混交林能够降低林分的燃烧性,有利于阻隔或延缓林火蔓延,在营林防火上有推广应用价值。 相似文献
9.
为探究阜新地区不同林分类型的土壤肥力情况,试验以该地区6种林分(2种针叶林、2种阔叶林和2种混交林)为研究对象,分别通过测定土壤养分和土壤酶活性的相关指标对土壤肥力水平进行了分析,结果表明:不同林分类型各土壤养分及酶活性存在较明显的差异,土壤肥力综合表现以阔叶林最优,针阔混交林次之,针叶林最弱,并且灌木林和次生林优于人工林。6种林分土壤的具体肥力水平依次为山杏灌木林>蒙古栎次生林>油松+蒙古栎混交林>油松人工纯林>油松+樟子松混交林>樟子松人工纯林。 相似文献
10.
亚热带地区杉木人工林和阔叶林土壤活性有机质研究(英文) 总被引：1，自引：2，他引：1
土壤活性有机质对土壤养分如氮、磷、硫的生物化学循环具有作用,其含量和质量影响土壤的初级生产力。本试验在中国科学院会同森林生态实验站通过对第一代、第二代杉木纯林和地带性阔叶林土壤活性有机质组分的对比研究,发现杉木纯林土壤活性有机质的含量低于地带性阔叶林。第一代杉木纯林易氧化有机碳、微生物生物量碳、水溶性有机碳和水溶性碳水化合物的含量分别比第二代杉木纯林高35.9%、13.7%、87.8%和50.9%,比地带性阔叶林的低15.8%、47.3%、38.1%和30.2%。在调查的三种林地内,土壤微生物生物量碳和水溶性有机碳含量下降幅度较大,其次为水溶性碳水化合物,而易氧化有机碳的变化最小。同时,杉木纯林土壤养分等理化性质也比地带性阔叶林低。这表明在杉木纯林取代地带性阔叶林以及杉木纯林连栽后林地的土壤肥力降低。图3 表2参26。 相似文献
11.
土壤碳库平衡是土壤肥力保持的重要内容[1].不同森林类型,由于其凋落物数量、类组及分解行为不同,因而形成的土壤碳库大小与特征将存在较大差别.常绿阔叶林、马尾松(Pinus massoniana Lamp.)林、杉木(Cunninghamia lanceolata (Lamb.)Hook.)林和毛竹(Phyllostachys edulis(Carr.)H.de Lehaie)林是我国亚热带最主要的4种森林类型. 相似文献
12.
不同施肥雷竹林土壤水溶性有机碳动态变化 总被引：5，自引：0，他引：5
为了解目前生产上不同施肥习惯对土壤活性有机碳产生的影响，从2002年8月至2003年4月动态采集了各施肥处理土壤样品，用岛津TOC-VcPH有机碳分析仪测定了土壤水溶性有机碳含量。结果表明：不同施肥处理土壤水溶性有机碳含量均表现出8、10月最高，12月开始降低，次年2月降至低谷，而4月又上升的变化规律。试验全过程中，3个有机无机肥混合施用处理土壤水溶性有机碳含量始终高于3个单施化肥处理，并且差异达显著水平，并随着有机肥用量的增加，土壤水溶性有机碳含量也显著增加。所有施肥处理土壤水溶性有机碳含量均是覆盖区高于未覆盖区，覆盖区平均是未覆盖区的1．56倍。土壤水溶性有机碳含量与土壤总有机碳含量存在极显著相关性，与土壤水解氮相关性也达显著水平。 相似文献
13.
毛竹林集约经营过程中土壤活性有机碳库的演变 总被引：10，自引：0，他引：10
为了探讨不同集约经营历史毛竹林的土壤有机碳库演变规律,在浙江省安吉县分别采集了集约经营5、10、20和40年的毛竹林土壤样品,与粗放经营毛竹林进行比较.结果表明:毛竹林集约经营的前5年里,土壤总有机碳、微生物量碳、水溶性碳和矿化态碳含量均明显下降(P＜0.05);土壤总有机碳持续下降至20年后趋于稳定,土壤水溶碳、矿化态碳含量集约经营5年后一直到第40年无明显变化;随着集约经营措施的实施,土壤活性有机碳占总有机碳的比例变化不大(除矿化态碳在0～5年以及微生物量碳在10～20年明显下降外).集约经营20年后,土壤总有机碳下降了34.70%,微生物量碳下降了49.35%.相关分析表明,各活性碳之间显著或极显著相关.比较不同经营类型的毛竹林发现,集约经营并未改变土壤各类碳含量的剖面特征.集约经营会导致土壤碳的大量损失,并使土壤生物学性质明显下降. 相似文献
14.
Studying contents and seasonal dynamics of active organic carbon in the soil is an important method for revealing the turnover and regulation mechanism of soil carbon pool. Through 3 years of field sampling and lab analysis, we studied the seasonal variations, content differences, and interrelationships of total organic carbon (TOC), light fraction organic carbon (LFOC), and particulate organic carbon (POC) of the soil in the forest areas burned with different fire intensities in the Daxing’anling Mountains. The mean TOC content in the low-intensity burned area was greater than that in the unburned area, moderate-intensity, and high-intensity burned areas in June and November (P < 0.05). LFOC and POC in the low-intensity burned area were greater than that in either moderate-intensity or high-intensity burned areas, with significant differences in LFOC in September and November (P < 0.05). A significant difference in LFOC between the unburned and burned areas was only found in July (P < 0.05). However, the differences in POC between the unburned and burned areas were not significant in all the whole seasons (P > 0.05). Soil LFOC and POC varied significantly with the seasons (P < 0.05) in the Daxing’anling Mountains. Significant linear relationships were observed between soil TOC, LFOC, and POC, which were positively correlated with soil nitrogen and negatively correlated with soil temperature in the Daxing’anling Mountains. 相似文献
15.
Patrícia A. B. Barreto Emanuela F. Gama-Rodrigues A. C. Gama-Rodrigues Alexandre G. Fontes José C. Polidoro Maria Kellen S. Moço Regina C. R. Machado V. C. Baligar 《Agroforestry Systems》2011,81(3):213-220
Agroforestry systems can play a major role in the sequestration of carbon (C) because of their higher input of organic material
to the soil. The importance of organic carbon to the physical, chemical, and biological aspects of soil quality is well recognized.
However, total organic carbon measurements might not be sensitive indicators of changes in soil quality. Adoption of procedures
that can extract the more labile fraction preferentially might be a more useful approach for the characterization of soil
organic carbon resulting from different soils. This study aimed to evaluate organic carbon (C) fractions distribution in different
soil layers up to 50 cm depth in two soil orders under cacao (Theobroma
cacao) agroforestry systems (AFS) in Bahia, Brazil. Soil samples were collected from four depth classes (0–5, 5–10, 10–30 and 30–50 cm)
under two cacao agroforestry systems (30-year-old stands of cacao with Erythrina glauca, as shade trees) in Latosol and Cambisol, in Bahia, Brazil. The determination of oxidizable carbon by a modified Walkley–Black
method was done to obtain four C fractions with different labile forms of C (fraction 1: labile fraction; fraction 2: moderate
labile fraction; fraction 3: low labile fraction and fraction 4: recalcitrant fraction). Overall, at two cacao AFS, the C
fractions generally declined with increase in soil depth. The C fractions 1 and 2 were 50% higher on upper layers (0–5 and
5–10 cm). More than 50% of organic C was found in more labile fraction (fraction 1) in all depths for both soils. High value
of C fraction 1 (more labile C)-to-total organic C ratio was obtained (around 54–59%, on Latosol and Cambisol, respectively),
indicating large input of organic matter in these soils. 相似文献
16.
通过马尾松低效林改造试验,研究了不同改造措施(全砍重造(QKCZ)、封山育林(FSYL)和补植混交(BZHJ))对土壤有机碳和活性有机碳的影响.结果表明:马尾松低效林改造后土壤有机碳(SOC)、微生物量碳(MBC)、水溶性有机碳(DOC)和易氧化碳(EOC)含量分别比未改造的马尾松低效林(对照,CK)增加了1.06～3.30 g·kg-1、16.81～142.29 mg·kg-1 (P ＜0.05)、12.83～43.71 mg· kg-1(P＜0.05)和0.16 g～0.54 g·kg-1(P＜0.05);不同改造措施马尾松林土壤活性有机碳占土壤有机碳的比例大小顺序,微生物量碳/有机碳(MBC/SOC)为FSYL＞ CK＞ QKCZ＞ BZHJ,易氧化碳/有机碳(EOC/SOC)为CK＞ BZHJ＞ FSYL＞ QKCZ,水溶性有机碳/有机碳(DOC/SOC)为BZHJ＞ CK＞ FSYL＞ QKCZ.说明3种马尾松低效林改造措施中QKCZ的土壤有机碳稳定性最好,更有利于土壤有机碳固存. 相似文献
17.
《林业研究》2016,(6)
Studying contents and seasonal dynamics of active organic carbon in the soil is an important method for revealing the turnover and regulation mechanism of soil carbon pool. Through 3 years of field sampling and lab analysis, we studied the seasonal variations, content differences, and interrelationships of total organic carbon(TOC), light fraction organic carbon(LFOC), and particulate organic carbon(POC) of the soil in the forest areas burned with different fire intensities in the Daxing'anling Mountains. The mean TOC content in the low-intensity burned area was greater than that in the unburned area,moderate-intensity, and high-intensity burned areas in June and November(P0.05). LFOC and POC in the lowintensity burned area were greater than that in either moderate-intensity or high-intensity burned areas, with significant differences in LFOC in September and November(P 0.05). A significant difference in LFOC between the unburned and burned areas was only found in July(P 0.05). However, the differences in POC between the unburned and burned areas were not significant in all the whole seasons(P 0.05). Soil LFOC and POC varied significantly with the seasons(P 0.05) in the Daxing'anling Mountains. Significant linear relationships were observed between soil TOC, LFOC, and POC, which were positively correlated with soil nitrogen and negatively correlated with soil temperature in the Daxing'anling Mountains. 相似文献
18.
[目的]通过实地采样对黑碳进行量化研究。[方法]利用相对密度分组方法探讨了长白山典型森林土壤黑碳含量及在不同有机碳组分中的分布特征。[结果]表明:黑碳(BC)含量在表层(A11)、亚表层(A12)分别为6.39~16.55 g·kg-1、1.44~6.16 g·kg-1,随土壤深度的增加而显著下降(p﹤0.01)。在A11、A12层中,轻组有机碳(LFOC)平均含量分别为66.66 g·kg-1、6.65 g·kg-1,轻组黑碳(LFBC)平均含量分别为5.63 g·kg-1、1.21 g·kg-1,同时,LFBC/LFOC在A12层(10.02%~34.89%)显著高于A11层(6.99%~14.45%)(p﹤0.01);A11、A12层重组有机碳(HFOC)平均含量分别为49.16 g·kg-1、36.55 g·kg-1,重组黑碳(HFBC)平均含量分别为2.69 g·kg-1、1.44 g·kg-1,HFBC/HFOC在A11层(3.36%~8.08%)和A12层(3.21%~7.58%)之间没有显著差异(p>0.05)。另外,土壤中LFBC/LFOC显著高于HFBC/HFOC(p﹤0.01),LFBC/BC显著高于HFBC/BC(p﹤0.01)。[结论]长白山典型森林土壤中黑碳的含量、比例均较高;土壤表层(A11)有机碳、黑碳含量及各组分有机碳、黑碳含量均高于亚表层(A12),均随着土层加深而显著降低;轻组、重组有机碳中均含有一定比例的黑碳,黑碳主要分布在轻组分中;轻组、重组有机碳与组分中黑碳均显著相关,轻组中相关系数大于重组。 相似文献
19.
J. K. Jensen L. H. Rasmussen K. Raulund-Rasmussen O. K. Borggaard 《European Journal of Forest Research》2008,127(4):263-274
Despite high demand on the timber, sycamore (Acer pseudoplatanus L.) covers only about 2% of the forested area in Denmark, mainly because several examples of failed stands have made foresters
reluctant to grow sycamore. In order to optimize the use of sycamore, scientifically based knowledge is needed on the specific
demands of sycamore to soil properties. Therefore, 34 stands of sycamore covering a broad range of soil types, tree heights
and ages were investigated. Tree height and age were determined on 20 trees in each stand and combined into a site index.
In each stand, soil water status, slope and ground cover were determined and soil samples were taken and analyzed for pH,
organic carbon, total nitrogen, calcium carbonate, bulk density and texture in the laboratory. The data were analyzed by simple
regression supplemented by PCA and MLR. Accordingly, sycamore can grow well on a broad range of soils regarding texture and
water content. However, soils with stagnant water within 40 cm of the soil surface are unsuited for sycamore. On well-drained
soils, increasing clay content caused better sycamore growth, which was also improved on insufficiently drained soils with
calcium carbonate. Increased nitrogen content stimulated sycamore growth while, less productive stands occurred on carbon
rich soils indicating that carbon and nitrogen contents can serve as sycamore growth indicators. Bulk density, C/N ratio and
pH showed no significant influence on growth. The investigation showed that sycamore could grow well on a broader range of
soils than hitherto believed. 相似文献