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1.
河北省北部森林植被碳储量和固碳速率研究 总被引：2，自引：1，他引：1
为了了解河北省北部森林植被固碳能力,本文以该区域阔叶林、针叶林、混交林、经济林和灌丛为研究对象,基于政府间气候变化专门委员会(IPCC)推荐采用的加拿大林业碳收支模型(CBM-CFS3),利用第7次全国森林资源连续清查数据和野外森林植被调查样地数据,拟合出研究区的蓄积-生物量转换参数和林木器官生物量比例参数,建立研究区内不同森林植被类型的蓄积生长方程、蓄积-干材生物量转换方程、生物量组分比例方程,采用这些方程评估了2010年河北省北部森林生态系统植被碳储量、碳密度和固碳速率。结果表明:拟合的不同森林植被蓄积生长方程的决定系数均大于0.7,蓄积-干材生物量转换方程的决定系数均大于0.8,生物量组分比例方程拟合效果较好,可用于评估该区域森林植被碳汇功能和潜力。2010年河北省北部森林植被碳储量为59.66 Tg(C),平均森林植被碳密度为25.05 Mg(C)×hm~(-2),森林植被固碳速率为0.07~1.87Mg(C)×hm~(-2)×a~(-1);其中阔叶林、针叶林、混交林、经济林碳储量和碳密度分别为30.97 Tg(C)、12.36 Tg(C)、15.73Tg(C)、0.60 Tg(C)和26.09 Mg(C)×hm~(-2)、26.14 Mg(C)×hm~(-2)、24.50 Mg(C)×hm~(-2)、7.53 Mg(C)×hm~(-2)。河北省北部森林植被碳密度与固碳速率均从西北到东南呈升高趋势。造林后森林面积增加6 400 km2,森林植被碳储量增加19.54 Tg(C)(不包括灌丛);林龄结构以中幼龄林为主,未来森林固碳潜力巨大。说明造林在增加森林植被碳储量和提高森林的固碳速率中起到了重要作用。 相似文献
2.
施肥对土壤有机碳含量及碳库管理指数的影响 总被引：16，自引：0，他引：16
在华北夏玉米生产体系中,采用田间试验,研究了不同施肥措施下（不施肥、单施有机肥、推荐施肥、习惯施肥和单施化肥）,土壤有机碳含量、活性有机碳含量和碳库管理指数的变化。结果表明:与不施肥相比,单施有机肥土壤有机碳和活性有机碳含量分别增加 11.68%,21.71%。推荐施肥和习惯施肥土壤有机碳含量分别增加 6.57%,7.58%,活性有机碳含量分别增加 8.53%,4.26%。单施化肥土壤有机碳与活性有机碳含量均没有显著增加;施有机肥和推荐施肥土壤碳库管理指数比不施肥分别高 31.79,13.01。单施化肥土壤碳库管理指数没有显著变化;土壤活性有机碳与总有机碳、碳库管理指数、玉米子粒产量均存在极显著相关关系。碳库管理指数与玉米子粒产量极显著相关,能够指示土壤生产力的变化。可见在当地土壤肥力条件下,施有机肥或有机无机适当配施能提高土壤有机碳含量和土壤碳库管理指数,有利于改善土壤质量,提高土壤肥力。 相似文献
3.
不同地表覆盖栽培对旱地土壤有机碳、无机碳和轻质有机碳的影响 总被引：10，自引：1，他引：9
通过田间长期定位试验,分层采集冬小麦-休闲种植体系0—40 cm土层的土样,研究了常规、地表覆膜和覆草栽培对土壤有机碳、无机碳和轻质有机碳的影响。结果表明,覆膜或覆草可以显著增加地上部小麦生物量和子粒产量。不同地表覆盖对0—40 cm土层的无机碳含量和分布无显著影响,但与常规栽培相比,地表覆膜使0—5 cm土层的有机碳含量显著降低,0—40 cm各土层轻质有机碳表现出明显降低趋势,平均降低 C 6.1~74.5 mg/kg;地表覆草却表现出明显增加土壤轻质有机碳的趋势,0—5,5—10,10—20 cm土层的轻质有机碳含量分别增加C 235.2、190.0和144.9 mg/kg,相当于常规的38.7%,32.9%和34.5%。同时,覆草栽培还表现出降低0—10 cm土层轻质有机质含碳量的趋势,并使0—20 cm土层轻质有机碳占有机碳的比例显著高于常规栽培和地表覆膜处理。可见,地表长期覆膜不利于旱地土壤有机碳累积,覆草不仅可以增加表层土壤的轻质有机碳累积,还可改善土壤碳氮组成。 相似文献
4.
不同农业废弃物还田对土壤碳排放及碳固定的影响 总被引：3，自引：1，他引：2
在玉米生长季,采用静态箱法,在氮磷钾等养分量(N 240kg/hm~2,P2O5100kg/hm~2,K2O 120kg/hm~2)的条件下,研究秸秆、牛粪、鸡粪与化肥配施还田,对土壤CO_2排放及碳固定的影响。研究结果表明:施肥促进土壤CO_2排放,其中100%秸秆粉碎还田配施化肥(S1)对土壤CO_2排放的促进作用最为明显,平均排放通量达389.0mg/(m~2·h);其次为单施化肥(S4)。S1、S2、S3和S4处理在6,7,8三个月份CO_2平均排放通量表现为S4S1S3S2,分别占整个生长季排放总量的80.1%,78.9%,78.8%和83.7%,表明单施化肥处理(S4)在玉米生长旺季CO_2排放通量最高达624.9mg/(m~2·h)。各施肥处理在玉米生长季出现2个CO_2排放高峰阶段,与2次氮肥(尿素)追施密切相关,2次追施氮肥后CO_2排放通量平均值均表现为S4S1S3S2,表明用农业废弃物中的氮部分代替化肥氮,可减少CO_2排放量。50%牛粪有机氮还田配施50%化肥氮(S2),能明显提高土壤有机碳含量。50%鸡粪有机氮还田配施50%化肥氮(S3)可明显提高玉米各器官及植株含碳量,其中S3处理植株含碳量最高为9.59t/hm~2,促进玉米碳固定;而100%秸秆粉碎还田配施化肥氮(S1),并不能提高玉米各器官及植株含碳量,甚至低于单施化肥(S4)。 相似文献
5.
《Communications in Soil Science and Plant Analysis》2012,43(17-18):2203-2212
Abstract The oxidable carbon content of 46 calcareous soils from the South‐East of Spain was determined by the Walkley and Black method and compared with the total organic carbon (C) content obtained by an automatic microanalysis method. The results were fitted to linear, curvilinear, and exponential equations which permit the conversion of the oxidable C values into those of total organic C when no direct means of analysis of the latter is available. A conversion factor of 1.26 is recommended. 相似文献
6.
土壤有机碳储量与外源碳输入量关系的建立与验证 总被引：2，自引：1，他引：2
7.
Wenming Ma Zhongwu Li Keyi Ding Bin Huang Xiaodong Nie Yinmei Lu Haibin Xiao Guangming Zeng 《Journal of Soils and Sediments》2016,16(6):1705-1717
Purpose
This study aims to explore the dynamics of the factors influencing soil organic carbon (SOC) sequestration and stability at erosion and deposition sites.Materials and methods
Thermal properties and dissolved aromatic carbon concentration along with Al, Fe concentration and soil specific surface area (SSA) were studied to 1 meter depth at two contrasting sites.Results and discussion
Fe, Al concentrations and SSA size increased with depth and were negatively correlated with SOC concentration at the erosion site (P?<?0.05), while at the deposition site, these values decreased with increasing depth and were positively correlated with SOC concentration (P?<?0.05). TG mass loss showed that SOC components in the two contrasting sites were similar, but the soils in deposition site contained a larger proportion of labile organic carbon and smaller quantities of stable organic carbon compared to the erosion site. SOC stability increased with soil depth at the erosion site. However, it was slightly variable in the depositional zone. Changes in SUVA254 spectroscopy values indicated that aromatic moieties of DOC at the erosion site were more concentrated in the superficial soil layer (0–20 cm), but at the deposition site they changed little with depth and the SUVA254 values less than those at the erosion site.Conclusions
Though large amounts of SOC accumulated in the deposition site, SOC may be vulnerable to severe losses if environmental conditions become more favorable for mineralization in the future due to accretion of more labile carbon. Deep soil layers at the erosion site (>30 cm deep) had a large carbon sink potential.8.
Soil erosion and carbon dynamics 总被引：2，自引：0，他引：2
Accelerated erosion involves preferential removal of soil organic carbon (SOC) because it is concentrated in vicinity of the soil surface and has lower density than the mineral fraction. The SOC transported by water runoff is redistributed over the landscape and deposited in depressional sites where it is buried along with the sediments. However, the fate of the SOC transported, redistributed and deposited by erosional processes is a subject of intense debate. Sedimentologists argue that SOC buried with sediments is physically protected, and that depleted in the eroded soil is replaced through biomass production. Thus, they argue that the erosion–sedimentation process leads to globally net SOC sequestration of 0.6–1.5 Gt C/year. In contrast, soil scientists argue that: (i) a large portion of the SOC transported by water runoff comprises labile fraction, (ii) breakdown of aggregation by raindrop impact and shearing force of runoff accentuates mineralization of the previously protected organic matter, and (iii) the SOC within the plow zone at the depositional sites may be subject to rapid mineralization, along with methanogenesis and denitrification under anaerobic environment. Whereas, tillage erosion may also cause burial of some SOC, increase in soil erosion and emission of CO2 from fossil fuel combustion are net sources of atmospheric CO2. Soil scientists argue that soil erosion may be a net source of atmospheric CO2 with emission of 1 Gt C/year. It is thus important to understand the fate of eroded SOC by measuring and monitoring SOC pool in eroded landscape as influenced by intensity and frequency of tillage operations and cropping systems. 相似文献
9.
不同氮水平下小麦植株的碳氮代谢及碳代谢与赤霉病的关系 总被引：4，自引：0，他引：4
为明确不同施氮量下小麦植株的碳氮代谢特性及碳代谢与小麦赤霉病的关系,本文采用田间小区试验,以小麦多穗型品种‘豫麦49-198’和大穗型品种‘周麦16’为供试材料,在0 kg(N)·hm-2 、120 kg(N)·hm-2 、180 kg(N)·hm-2 、240 kg(N)·hm-2 、360 kg(N)·hm-2 5个氮肥水平下,探讨了不同施氮水平对小麦植株可溶性糖含量、C/N以及小麦赤霉病发病率和病情指数的影响。结果表明:两个品种小麦植株内的可溶性糖含量和C/N由越冬到开花期呈"V"形变化,拔节期最低,分别为80~200 mg·g-1和3~10。开花期各处理间差异达到最大,且施氮处理植株的可溶性糖含量和C/N比不施氮处理分别低15.4%~47.7%和24.5%~63.1%。植株全氮含量随施氮量的增加而增加,各处理在小麦拔节期和开花期差异最大。两个品种小麦植株的可溶性糖和氮素的累积吸收量在小麦生育期内均呈增加趋势。相关分析表明,植株全氮含量与小麦的可溶性糖含量在小麦拔节期和开花期显著负相关;小麦拔节期和开花期的可溶性糖含量、C/N与小麦赤霉病的发病率和病情指数呈线性关系。说明小麦拔节期到开花期的碳氮代谢对赤霉病的发生影响较大。 相似文献
10.
蔬菜连作对铜尾矿土壤中有机碳、腐殖质碳以及可溶性有机碳的影响 总被引：2，自引：0，他引：2
Carbon of humus acids （HSAC） and dissolved organic carbon （DOC） are the most active forms of soil organic carbon （SOC） and play an important role in global carbon recycling. We investigated the concentrations of HSAC, water-soluble organic carbon （WSOC）, hot water-extractable organic carbon （HWOC） and SOC in soils under different vegetation types of four copper mine tailings sites with differing vegetation succession time periods in Tongling, China. The concentrations of HSAC, WSOC, HWOC and SOC increased with vegetation succession. WSOC concentration increased with the accumulation of SOC in the tailings, and a linearly positive correlation existed between the concentrations of HSAC and SOC in the tailings. However, the percentages of HSAC and DOC in the SOC decreased during vegetation succession. The rate of SOC accumulation was higher when the succession time was longer than 20 years, whereas the speeds of soil organic matter （SOM） decomposition and humification were slow, and the concentrations of HSAC and DOC increased slowly in the tailings. The percentage of carbon of humic acid （HAC） in HSAC increased with vegetation succession, and the values of humification index （HI）, HAC/carbon of fulvic acid, also increased with the accumulation of HSAC and SOC in soils of the tailings sites. However, the HI value in the each of the tailings was less than 0.50. The humification rate of SOM was lower than the accumulation rate of SOM, and the level of soil fertility was still very low in the tailings even after 40 years of natural restoration. 相似文献
11.
苏打盐碱水灌溉的土壤添加石膏肥和有机肥后水溶性碳和微生物碳研究 总被引：1，自引：0，他引：1
Microbial biomass carbon (MBC), a small fraction of soil organic matter, has a rapid turnover rate and is a reservoir of labile nutrients. The water-extractable carbon pools provide a fairly good estimate of labile C present in soil and can be easily quantified. Changes in soil MBC and water-extractable organic carbon pools were studied in a 14-year long-term experiment in plots of rice-wheat rotation irrigated with canal water (CW), sodic water (SW, 10-12.5 mmol c L-1 residual sodium carbonate), and SW amended with gypsum with or without application of organic amendments including farmyard manure (FYM), green manure (GM), and wheat straw (WS). Irrigation with SW increased soil exchangeable sodium percentage by more than 13 times compared to irrigation with CW. Sodic water irrigation significantly decreased hot water-extractable organic carbon (HWOC) from 330 to 286 mg kg-1 soil and cold water-extractable organic carbon (CWOC) from 53 to 22 mg kg-1 soil in the top 0-7.5 cm soil layer. In the lower soil layer (7.5-15 cm), reduction in HWOC was not significant. Application of gypsum alone resulted in a decrease in HWOC in the SW plots, whereas an increase was recorded in the SW plots with application of both gypsum and organic amendments in both the soil layers. Nevertheless, application of gypsum and organic amendments increased the mean CWOC as compared with application of gypsum alone. CWOC was significantly correlated with MBC but did not truly reflect the changes in MBC in the treatments with gypsum and organic amendments applied. For the treatments without organic amendments, HWOC was negatively correlated with MBC (r = 0.57*) in the 0-7.5 cm soil layer, whereas for the treatments with organic amendments, both were positively correlated. Irrigation with SW significantly reduced the rice yield by 3 t ha-1 and the yield of rice and wheat by 5 t ha-1 as compared to irrigation with canal water. Application of amendments significantly increased rice and wheat yields. Both the rice yield and the yield of rice and wheat were significantly correlated with MBC (r = 0.49**-0.56**, n = 60). HWOC did not exhibit any relation with the crop yields under the treatments without organic amendments; however, CWOC showed a positive but weak correlation with the crop yields. Therefore, we found that under sodic water irrigation, HWOC or CWOC in the soils was not related to MBC. 相似文献
12.
杨木炭胶合成型速燃炭的制备与燃烧性能 总被引：1，自引：1，他引：0
为了研究了胶黏剂的类型、胶炭比、引燃剂的种类和添加量、成型压力、成型时间等因素对速燃炭燃烧性能的影响,该文利用杨木屑经炭化后得到杨木炭,以杨木炭为主要原料,添加适量不同种类的胶黏剂和引燃剂制备速燃炭。结果表明：将胶黏剂A和杨木炭以质量比为0.6︰1的胶炭比混合,并添加占杨木炭质量分数为5%的硝酸钾,在25 MPa的成型压力下保持2 min,制备出的速燃炭有较好的速燃效果。不仅具有一定强度,燃烧时无毒、无烟、无味,并能在 5 s内快速点燃速燃炭。速燃炭的抗压系数达8.60 N/mm2,燃烧剩余物的质量分数为6.33%,燃烧时间可持续11.20 min/g,热值达到35 762.76 J/g。该研究可为粉末燃料的成型胶黏剂研制提供依据。 相似文献
13.
《Communications in Soil Science and Plant Analysis》2012,43(13-14):2571-2581
Abstract The objective of this experiment was to measure the impact of molybdenum (Mo) addition to the soil on changes in rate of photosynthesis (PN), specific root nodule nitrogenase activity (SNA), chlorophyll ‐ (Chl‐a) and (Chl‐b) and biomass of soybean (Glycine max L. Merrill), exposed to carbon dioxide (CO2) (350, 400, or 450 μL/L) for 5 d during its sensitive growth stage (R2). Plants grown in soil with Mo (0, 0.5, or 1.0 mg/kg soil dry weight) were exposed to carbon dioxide (CO2) in open‐top field chambers for 12 h/d for 5 d with a nitrogen (N)‐free fertilizer. Increasing CO2 levels reduced SNA and increased both Chl‐a and Chl‐b. Addition of 1 mg/kg Mo significantiy reduced SNA for plants grown with 350 μL/L CO2 with no change in PN. 相似文献
14.
不同橡胶生长期土壤中的微生物生物量碳和有机碳 总被引：16，自引：6，他引：16
Soil samples were collected from different rubber fields in twenty-five plots selected randomly in the Experimental Farm of the Chinese Academy of Tropical Agriculture Sciences located in Hainan, China, to analyse the ecological effect of rubber cultivation. The results showed that in the tropical rubber farm, soil microbial biomass C (MBC) and total organic C (TOC) were relatively low in the content but highly correlated with each other. After rubber tapping, soil MBC of mature rubber fields decreased significantly, by 55.5%, compared with immature rubber fields. Soil TOC also decreased but the difference was not significant. Ratios of MBC to TOC decreased significantly. The decreasing trend of MBC stopped at about ten years of rubber cultivation. After this period, soil MBC increased relatively while soil TOC still kept in decreasing. Soil MBC changes could be measured to predict the tendency of soil organic matter changes due to management practices in a tropical rubber farm several years before the changes in soil TOC become detectable. 相似文献
15.
Takuji Nakamura Mitsuru Osaki Takuro Shinano Toshiaki Tadano 《Soil Science and Plant Nutrition》2013,59(4):777-788
14CO2 was assimilated during 10 min in leaf of rice and soybean under 21 kPa O2 (21% O2 treatment) and 2 kPa O2 (2% O2 treatment) at the vegetative growth stage and flowering stage. The 14C distribution ratio to respired CO2 and crude chemical components (sugars, polysaccharides, amino acids, organic acids, and proteins) was determined. In this paper, since emphasis was placed on the 14C distribution mechanism to carbon compounds and nitrogen compounds, the terms carbon metabolism pool (C-pool) composed of sugars and polysaccharides, and nitrogen metabolism pool (N-pool) composed of organic acids, amino acids and proteins were used. The results obtained were as follows. 14C distribution ratio to N-pool at 0 min after 14C assimilation was higher in soybean than in rice regardless of the treatments and stages, and that at 30 min after 14C assimilation under light condition markedly decreased both in rice and soybean. Therefore, especially in soybean, a large amount of photosynthesized 14C was once distributed to the N-pool, then 14C compounds in the N-pool were reconstructed into the C-pool. During this reconstruction process, 14C compounds in the N-pool were actively respired. 14C distribution to N-pool at 0 min after 14C assimilation changed slightly or did not change by the N treatment. 14C distribution to N-pool in the - N treatment of soybean (13–29 mg N g-1 content in leaves) was higher than that in the + N treatment of rice (31–48 mg N g-1 content in leaves). Photosynthesized carbon distribution to N-pool in rice decreased with growth, while it remained constant in soybean. Accordingly, in soybean, photosynthesized carbon was predominantly distributed to the N-pool through photorespiration and/or Calvin cycle (supplying triose-P), which was less affected by nitrogen nutrient and aging. Thus, the mechanism of photosynthesized carbon distribution to carbon and nitrogen compounds was basically regulated by inherited characters of each plant more than by the nitrogen status of leaves. By the 2% O2 treatment, 14C distribution to N-pool decreased in both crops regardless of N treatment, indicating that photorespiration plays an important role in the supply of the preliminarily photosynthesized carbon compounds to N-pool. In the 2% O2 treatment, 14C distribution to N-pool was higher in soybean than in rice, indicating that triose-P transported from chloroplast was preferentially distributed to N-pool in the case of soybean. 相似文献
16.
施肥对喀斯特地区植草土壤活性有机碳组分和牧草固碳的影响 总被引：1，自引：0，他引：1
通过盆栽试验,研究施肥对喀斯特地区植草土壤不同活性有机碳组分和牧草固碳的影响。试验处理包括CK（不施肥）、 N1 （N 150 mg/kg）、 N2 （N 250 mg/kg）、 N1P1 （P2O5100 mg/kg）、 N2P2 （P2O5150 mg/kg）、 N1P1K1 （K2O 70 mg/kg）、 N1P1K2 （K2O 105 mg/kg）和N2P2K1和N2P2K2。结果表明,与对照（不施肥）相比,施肥处理增加植草土壤有机碳、 微生物量碳和易氧化碳,有机碳日矿化量和累积矿化量以及牧草固碳量。其中N1P1K1处理土壤有机碳和易氧化碳最高,N1P1处理土壤微生物量碳最高,N2P2K1处理土壤可溶性碳最高,N2P2K2处理牧草地上部及根系固碳量、 有机碳日矿化量和累积矿化量均最高。综上,低量氮磷钾肥配施有利于土壤活性有机碳的积累,高量氮磷钾平衡配施牧草固碳效果最佳。 相似文献
17.
Summary Soil was amended with a variety of carbon sources, including four soluble compounds (glucose, sucrose, glycerol and mannitol) and two plant residues (straw and alfalfa).. Potential denitrification rates, measured both as N2O accumulation and NO3
– disappearance, were compared, and the predicted values of available C, measured as CO2 production and water-extractable C, were assessed.The two measures of denitrification agreed well although N2O accumulation was, found to be most sensitive. Soil treated with the four soluble C compounds resulted in the same rate of denitrification although glycerol was not as rapidly oxidized. Alfalfa-amended soil produced a significantly higher rate of denitrification than the same amount of added straw. CO2 evolution was found to be a good predictor of denitrification over the first 2 days of sampling, but neither measure of available substrate C correlated well with denitrification rate beyond 4 days, when NO3
– was depleted in most treatments. The data with alfalfa-amended soil suggested that denitrifiers used water-extractable C. materials produced by other organisms under anaerobic conditions. 相似文献
18.
碳源调理剂对黄瓜秧堆肥进程和碳氮养分损失的影响 总被引：4，自引：3，他引：4
由于中国蔬菜产地的黄瓜秧无害化处理与循环利用缺乏针对性的使用技术,这类废弃资源多成为当地的环境污染源。该文以黄瓜秧为原料(空白对照,CK)进行高温好氧堆肥,并在此基础上设置2组处理,即把玉米秸秆(CS)和木本泥炭(WP)作为辅助碳源调理剂,按照C/N比为25添加到物料中。通过对比分析不同处理的CO2和氨气的排放速率和累积量、物料损失率、有机质含量、p H值、电导率(EC)、发芽指数等指标,研究外加碳源对黄瓜秧堆肥过程和碳氮氧分损失的影响,以期实现对黄瓜秧堆肥化进程进行工艺优化,并降低碳氮元素以气态形式的损失,进而减少温室气体排放。结果表明:玉米秸秆和木本泥炭作为外加碳源调理剂,可以减少物料损失量,加速堆肥腐熟进程,其中尤以玉米秸秆效果更佳。但是,玉米秸秆的添加会增加整个堆肥过程中有机质的降解和CO2的排放强度,提高累积排放量(100g/kg),而木本泥炭会减少有机质的降解总量和CO2的累积排放量(77g/kg);玉米秸秆和木本泥炭都有利于控制堆肥过程中氨气的排放,且作用时间和机理不同。综合考虑堆肥进程和气体损失,木本泥炭作为碳源调理剂的改良效果更优于秸秆,应进一步研究两者联合使用的效果。 相似文献
19.
长期施肥对黑土有机碳矿化和团聚体碳分布的影响 总被引：12，自引：1，他引：11
采用我国东北地区的连续施肥28 a的典型黑土,通过颗粒分组的方法,研究了长期不同施肥处理对土壤团聚体形成和有机碳在各级团聚体中的分布规律,以及各粒级团聚体对养分的贡献能力的影响。结果表明,施用有机肥促进了土壤中大颗粒团聚体(>0.25 mm)的形成,尤其以2~1 mm粒级增加的比例最大;而当化肥和有机肥配合施用后,主要促进土壤中<1 mm团聚体形成,尤其对0.5~0.25 mm粒级团聚体形成的促进作用最大。施肥(无论是有机肥还是化肥)能增加土壤有机碳含量,而且,化肥有机肥配合施用较单施化肥和单施有机肥的效果更好。随着团聚体粒级的降低,团聚体中有机碳的分配出现两个峰值,分别在2~1 mm和0.25~0.053 mm两个粒级中出现。单施化肥处理及化肥有机肥配施处理与无肥处理相比均增加了0.5~0.25 mm粒级团聚体对有机碳的贡献率;单施有机肥的处理与无肥处理相比增加了1~0.5 mm粒级团聚体对有机碳的贡献率。然而,对于东北的典型黑土,2~1 mm和0.25~0.053 mm两个粒级对土壤有机碳的保护作用最大,表明团聚体对有机碳的保护作用是碳分配和矿化分解作用的综合结果,通过调控施肥种类可以达到有效保护土壤质量和肥力的效果。 相似文献
20.
S. Lettens B. De Vos P. Quataert B. van Wesemael B. Muys & J. van Orshoven 《European Journal of Soil Science》2007,58(6):1244-1253
There is considerable interest in the computation of national and regional soil carbon stocks, largely as the result of the provisions of the Kyoto Protocol. Such stocks are often calculated and compared without proper reference to the uncertainties induced by different analytical methodologies. We illustrate the nature and magnitude of these uncertainties with the present soil organic carbon (SOC) study in Belgium. The SOC recovery of the Walkley‐Black method was investigated based on a database of 475 samples of silt loam and sandy soils, which cover different soil depths and vegetation types in northern Belgium. The organic carbon content of the soil samples was measured by the original Walkley‐Black method and by a total organic carbon analyser. The recovery was computed as the ratio of these two results per soil sample. Land use, texture and soil sampling depth had a significant influence on the recovery as well as their three‐way interaction term (land use × texture × sampling depth). The impact of a land use, texture and sampling depth dependent Walkley‐Black correction on the year 2000 SOC inventory of Belgium was determined by regression analysis. Based on new correction factors, the national SOC stocks increased by 22% for the whole country, ranging from 18% for cropland to 31% for mixed forest relative to the standard corrected SOC inventory. The new recovery values influenced therefore not only C stocks in the year 2000, but also the expected SOC change following land use change. Adequate correction of Walkley‐Black measurements is therefore crucial for the absolute and comparative SOC assessments that are required for Kyoto reporting and must be computed to take into account the regional status of soil and land use. ‘Universal’ corrections are probably an unrealistic expectation. 相似文献