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1.
选择半干旱(宁夏盐池)、干旱(内蒙古乌拉特后旗)荒漠草原区为研究样地,以牛枝子枯落物为研究对象,采用网孔分解袋法研究土壤动物分解功能对枯落物C、N、P、K分布的影响,结合枯落物分解过程中土壤有机碳(SOC)、全氮(TN)、全磷(TP)、全钾(TK)含量分布特征,阐明土壤动物分解作用对土壤营养元素含量分布的影响规律。结果表明：(1)共捕获土壤动物226只,隶属14科(属)。土壤动物个体数表现为盐池地区均高于乌拉特地区,而类群数差异较小,仅在乌拉特地区灌丛高于裸地。土壤动物Simpson指数、Shannon指数和Margalef指数在不同生境下均无显著差异,Pielou指数在裸地生境下表现为乌拉特地区显著高于盐池地区。(2)不同网孔分解袋中枯落物养分元素均处于不同程度的释放状态。其中枯落物C、N元素累积系数在盐池地区表现为2 mm网孔显著低于0.01 mm网孔,在乌拉特地区表现为2 mm网孔显著高于0.01 mm网孔;枯落物P、K元素累积系数分别在乌拉特地区和盐池地区表现为2 mm网孔显著高于0.01 mm网孔,且土壤动物对盐池枯落物C、N、P、K元素释放均表现为正效应;对乌拉特枯落物C、... 相似文献
2.
秸秆还田对东北黑土碳氮磷钾化学计量特征及玉米产量的影响 总被引：1，自引：0，他引：1
【目的】秸秆还田是提升农田土壤肥力,改善土壤养分含量及有效性的重要措施。我们分析了东北黑土区不同秸秆还田方式下土壤碳氮磷钾含量和玉米产量的年际变化,并从土壤化学计量特征角度研究了土壤养分的有效性。【方法】依托2012年在东北黑土区建立的秸秆还田长期定位试验,选取秸秆移除(CK)、秸秆混合还入0—20 cm耕层(RI)和秸秆覆盖还田(RC) 3个处理,测定了处理实施1年(2013)、3年(2015)、5年(2017)和8年(2020)后,不同土层土壤有机碳(SOC)、全氮(TN)、全磷(TP)、全钾(TK)含量及玉米产量,计算了土壤化学计量特征(C∶N、C∶P、N∶P),并分析了各指标之间的相关性。【结果】随试验年限的增加,在0—20 cm土层,CK处理SOC含量有所下降,TN含量基本保持不变,而RI和RC处理的SOC和TN含量均有所增加,RC处理下均为最高;RI处理的SOC和TN含量在0—20 cm土层分布相对均匀,RC处理SOC和TN含量在0—5 cm土层中明显增加,尤其在试验5～8年间的增幅明显升高。CK、RI和RC 3个处理的TP和TK含量均随试验年限的增加缓慢升高,处理间无显著... 相似文献
3.
Jagmandeep Dhillon Mariana Ramos Del Corso Bruno Figueiredo Eva Nambi William Raun 《Communications in Soil Science and Plant Analysis》2018,49(7):803-813
Continuous use of organic and inorganic fertilizers influences soil physical and chemical properties. Stored samples from the last 24 years of the Magruder Plots were analyzed to document changes in soil organic carbon (SOC), total nitrogen (TN) and soil pH. Since 1947, the same six treatments have been evaluated. Treatments included the use of cattle manure, inorganic nitrogen (N), phosphorus (P), potassium (K), and lime (L). Each year, a composite surface soil sample (0–15 cm) was taken in each plot, air-dried at ambient temperature, ground to pass a 2 mm sieve, and stored at room temperature, 25°C. Averaged over 24 years’ the manure plots resulted in the highest SOC and TN. Manure application maintained SOC at 0.92 and adequate soil pH (>6.0). The use of commercial fertilizers lowered soil pH over time but had higher yields compared to the manure plot. 相似文献
4.
黄土高原不同年限刺槐土壤化学计量特征分析 总被引：12，自引：1，他引：11
通过对陕北黄土高原4种不同年限(10,15,25,40年)刺槐林地0—200cm土壤的采集与分析,研究不同刺槐种植时间对土壤营养元素及化学计量比的影响。在每个林龄的林地内设3个小区,每个小区采用随机采样法选取3个采样点分层采集土壤样品,进行土壤碳、氮、磷、钾测定,计算化学计量比。结果表明:(1)有机碳和全氮、全钾含量随刺槐年限增加呈基本增大的趋势,全磷随刺槐年限的增长变化不大;有机碳、全氮和全磷呈极显著的正相关关系;(2)在0—200cm土层,有机碳、全氮空间分布基本一致,随土层深度增加均呈先减少后趋于稳定的变化趋势;全磷在整个空间中的分布较为均匀,其空间变异性低于有机碳和全氮;全钾含量高于碳氮磷含量,且随土壤深度变化不大;(3)土壤C∶N比,C∶P比,N∶P比和C∶N∶P比均随刺槐年限的增长呈先降低后升高的趋势,都在15年处有最低值;(4)土壤C∶N比随土层深度在一定范围波动,C∶P和N∶P比均随土层深度的增加呈先减少后趋于稳定的变化趋势。 相似文献
5.
贵州高原山地马尾松人工林土壤碳、氮、磷生态化学计量特性 总被引：2，自引：2，他引：0
采用空间代替时间的方法,选取贵州中部高原山地8,18,26,36年生4个林龄的马尾松人工林为研究对象,通过测定林下土壤有机碳(SOC)、全氮(TN)和全磷(TP)含量,分析不同发育阶段林分土壤养分变化规律及化学计量比特征。结果表明:马尾松人工林土壤SOC、TN、TP平均值分别为12.24,1.94,0.35g/kg,C∶N、C∶P和N∶P平均值分别为6.58,38.70和13.65,C∶N∶P的平均值为39∶6∶1,其养分含量总体不高。随土层深度增加,4个林龄土壤SOC、TN含量降低,但C∶N增加,TP、C∶P和N∶P无明显变化规律。随林龄增加,土壤SOC、TN、N∶P先降低后升高,而TP则持续降低;C∶N除在36年生林分中显著降低外,其余各林分均无显著差异;C∶P无明显变化规律。相关分析表明,SOC、TN是调控马尾松人工林土壤生态化学计量比的主要因素。研究结果可为进一步明确贵州高原山地马尾松人工林土壤养分循环特征提供重要参考。 相似文献
6.
A field experiment was conducted during two consecutive years of 2010–2011 and 2011–2012 to study the effect of biofertilizers in conjunction with organic and inorganic sources of nutrient management on productivity, quality and soil health on field pea at ICAR RC for NEH Region, Nagaland Centre Jharnapani, Nagaland, India. The experiment was laid out in split plot design with five nutrient sources in main plots and four treatment of biofertilizers with zinc in sub plots. Results indicated that the application of 100% recommended dose of fertilizer (RDF) through inorganic + 50% recommended dose of nitrogen (RDN) through vermicompost significantly improved root nitrogen (N) content, cation exchange capacity (CEC) of roots, NA activates, seed yield (1153 and 1262 kg ha?1), straw yield (2182 and 2332 kg ha?1) in the year of 2010–2011 and 2011–2012, respectively. Nutrients (N, P, K, S and Zn) uptake by seed and straw, protein content, protein harvest, soil organic carbon (SOC), available N, P, K, S, Zn and economics significantly higher with 100% RDF through inorganic + 50% RDN through vermicompost during both the years. Seed inoculation with biofertilizers along with 5 kg Zn ha?1 markedly enhanced the root N content, CEC of roots, nitrogenase activities (NA), seed yield (1080 and 1193 kg ha?1), straw yield (1978 and 2128 kg ha?1), nutrients [N, phosphorus (P), potassium (K), sulfur (S) and zinc (Zn)] uptake, soil organic carbon (SOC) (%), and available N, P, K, S, and Zn of pea in both the years, respectively. These sources also give more income and benefit cost ratio per rupees invested. 相似文献
7.
长期施用有机肥对稻麦轮作体系土壤有机碳氮组分的影响 总被引：5，自引：1，他引：4
8.
Effectiveness of surface-applied unincorporated broiler litter as a fertilizer relative to conventional inorganic fertilizers under no-till or conventional-till cotton (Gossypium hirsutum L.) production systems in the upland soils of the southern and southeastern USA is not well documented. The objectives of this research were to (1) test if broiler litter improves plant macronutrient (N, P, K, and Mg) nutrition of cotton above that of cotton fertilized with conventional inorganic fertilizers and (2) determine if lack of incorporating litter into the soil reduces macronutrient concentration in cotton plant parts in an upland soil considered marginal for cotton. Six treatments consisting of an unfertilized control, a fertilized standard (STD), two litter-only, and two litter plus inorganic N as urea–ammonium nitrate solution (UAN) were tested in two adjacent fields, one under no-till (NT) and the other under conventional-till (CT) systems. Litter alone, UAN, or a combination of litter plus UAN were applied to supply 101 kg ha−1 plant available N assuming nearly all of the UAN-N and 50% of the total litter N becomes plant available during the cotton growing season. Concentration of N, P, K, and Mg were measured in leaves, stems, and reproductive parts on three or four dates between early flowering and maturity. Cotton fertilized with the litter-only treatments always had less N concentration but greater P and K concentration in leaves, stems, and reproductive parts than cotton that received the STD treatment. Leaf and stem Mg concentration seems to depend on the N concentration in these plant parts. Lack of incorporating litter into the soil reduced N concentration in nearly all plant parts at all growth stages, suggesting some amount of the litter-derived N is lost due to lack of incorporation. Lack of incorporation also reduced leaf and stem Mg concentration, which seemed to be due to its reducing effect on N concentration. Unlike N and Mg, lack of incorporation did not consistently affect concentrations of P and K in all plant parts. Regardless of the incorporation treatment, fertilization with the litter-only treatments increased tissue P and K concentration and supported lint yield exceeding that of the STD without increasing tissue N concentration. 相似文献
9.
Summary An understanding of no-till ecosystems is essential for increased acceptance of conservation tillage practices. The primary objective of the present research was to assess the nutrient contributions of leachates from decomposing corn residue to soil in continuous-corn no-till ecosystems. A secondary objective was to estimate the phytotoxic effects of these leachates on corn seedling growth. The effects of moisture, temperature, and resident and non-resident microflora on leachates recovered from decomposing surface-applied corn residue were also studied. Leachates were analyzed for organic C, total N, PO
4
3–
-P, acid and alkaline phosphatase activity, urease activity, and phytotoxic effects. Within the first 90 days of a 215-day field study 73%, 83%, and 60% of C, N, and P, respectively, were leached. In terms of nutrient concentration, this suggests two distinct phases of release of nutrients onto the soil: A high initial flux of nutrients that is followed by a low-concentration release. No phytotoxic effect of field leachates was observed. Acid and alkaline phosphatase activity was highest on days 39 and 47 whereas urease activity peaked on day 149. In laboratory studies, alterations in temperature or moisture had little effect on the leachate nutrient concentration, or phytotoxic or enzyme activity. Increasing amounts of organic C and N were extracted over time. No phytotoxic effects were expressed in the laboratory. Overall, it appears that the maximum leaching of nutrients occurs early in the decomposition process and that in no-till systems no phytotoxicity can be associated with decomposition of surface residues.Paper No. 11871 of the Purdue University Agricultural Experiment Station Series 相似文献
10.
He Huan Xia Guotong Yang Wenjin Zhu Yunpeng Wang Guodong Shen Weibo 《Journal of Soils and Sediments》2019,19(12):3954-3968
Purpose
Wetlands in Mu Us Desert have severely been threatened by grasslandification over the past decades. Therefore, we studied the impacts of grasslandification on soil carbon (C):nitrogen (N):phosphorus (P) stoichiometry, soil organic carbon (SOC) stock, and release in wetland-grassland transitional zone in Mu Us Desert.
Materials and methodsFrom wetland to grassland, the transition zone was divided into five different successional stages according to plant communities and soil water conditions. At every stage, soil physical and chemical properties were determined and C:N:P ratios were calculated. SOC stock and soil respirations were also determined to assess soil carbon storage and release.
Results and discussionAfter grasslandification, SOC contents of top soils (0–10 cm) decreased from 100.2 to 31.79 g kg?1 in June and from 103.7 to 32.5 g kg?1 in October; total nitrogen (TN) contents of top soils (0–10 cm) decreased from 3.65 to 1.85 g kg?1 in June and from 6.43 to 3.36 g kg?1 in October; and total phosphorus (TP) contents of top soils (0–10 cm) decreased from 179.4 to 117.4 mg kg?1 in June and from 368.6 to 227.8 mg kg?1 in October. From stages Typha angustifolia wetland (TAW) to Phalaris arundinacea L. (PAL), in the top soil (0–10 cm), C:N ratios decreased from 32.2 to 16.9 in June and from 19.0 to 11.8 in October; C:P ratios decreased from 1519.2 to 580.5 in June and from 19.0 to 11.8 in October; and N:P ratios decreased from 46.9 to 34.8 in June and changed from 34.9 to 34.0 in October. SOC stock decreased and soil respiration increased with grasslandification. The decrease of SOC, TN, and TP contents was attributed to the reduction of aboveground biomass and mineralization of SOM, and the decrease of soil C:N, C:P, and N:P ratios was mainly attributed to the faster decreasing speeds of SOC than TN and TP. The reduction of aboveground biomass and increased SOC release led by enhanced soil respiration were the main reasons of SOC stock decrease.
ConclusionsGrasslandification led to lowers levels of SOC, TN, TP, and soil C:N, C:P, and N:P ratios. Grasslandification also led to higher SOC loss, and increased soil respiration was the main reason. Since it is difficult to restore grassland to original wetland, efficient practices should be conducted to reduce water drainage from wetland to prevent grasslandification.
相似文献11.
S. Kundu Ranjan Bhattacharyya Ved Prakash H. S. Gupta H. Pathak J. K. Ladha 《Biology and Fertility of Soils》2007,43(3):271-280
A long-term (30 years) soybean–wheat experiment was conducted at Hawalbagh, Almora, India to study the effects of organic
and inorganic sources of nutrients on grain yield trends of rainfed soybean (Glycine
max)–wheat (Triticum
aestivum) system and nutrient status (soil C, N, P and K) in a sandy loam soil (Typic Haplaquept). The unfertilized plot supported
0.56 Mg ha−1 of soybean yield and 0.71 Mg ha−1 of wheat yield (average yield of 30 years). Soybean responded to inorganic NPK application and the yield increased significantly
to 0.87 Mg ha−1 with NPK. Maximum yields of soybean (2.84 Mg ha−1) and residual wheat (1.88 Mg ha−1) were obtained in the plots under NPK + farmyard manure (FYM) treatment, which were significantly higher than yields observed
under other treatments. Soybean yields in the plots under the unfertilized and the inorganic fertilizer treatments decreased
with time, whereas yields increased significantly in the plots under N + FYM and NPK + FYM treatments. At the end of 30 years,
total soil organic C (SOC) and total N concentrations increased in all the treatments. Soils under NPK + FYM-treated plots
contained higher SOC and total N by 89 and 58% in the 0–45 cm soil layer, respectively, over that of the initial status. Hence,
the decline in yields might be due to decline in available P and K status of soil. Combined use of NPK and FYM increased SOC,
oxidizable SOC, total N, total P, Olsen P, and ammonium acetate exchangeable K by 37.8, 42.0, 20.8, 30.2, 25.0, and 52.7%,
respectively, at 0–45 cm soil layer compared to application of NPK through inorganic fertilizers. However, the soil profiles
under all the treatments had a net loss of nonexchangeable K, ranging from 172 kg ha−1 under treatment NK to a maximum of 960 kg ha−1 under NPK + FYM after 30 years of cropping. Depletion of available P and K might have contributed to the soybean yield decline
in treatments where manure was not applied. The study also showed that although the combined NPK and FYM application sustained
long-term productivity of the soybean–wheat system, increased K input is required to maintain soil nonexchangeable K level. 相似文献
12.
Md Mozammel Haque Jatish C. Biswas M. R. Islam A. Islam M. S. Kabir 《Journal of plant nutrition》2013,36(20):2901-2914
Nutrient sources and management influence soil properties and crop productivity indicating that sustained crop production needs nutrient rate specific tuning after certain periods of time. We hypothesize that long-term use of organic and inorganic nutrient sources maintains soil fertility and improve crop production. Yield and nutrient use efficiencies have not been evaluated in Bangladesh from long-term fertilizer trials focusing on adaptation strategies for sustained food production. So, the objectives of the present investigation were to examine the effects of organic and inorganic amendments on yields and soil properties under a rice-fallow-rice system. The experiment was initiated in 1985 with 12 treatments under dry season irrigated rice culture at the Bangladesh Rice Research Institute, Gazipur. The effects of organic and inorganic nutrient sources were evaluated under missing element techniques. The contributions of nitrogen (N), phosphorus (P), and potassium (K) fertilizers to yields were more in the dry season but the role of P was negligible in the wet season. The omissions of N, P and K nutrients are not suitable management option for rice cultivation during dry and wet seasons, although P can be omitted in the wet season provided its full dose is applied in the dry season. The combined use of organic and inorganic nutrient sources are the best option for improving rice productivity and sustaining soil fertility in a rice-fallow-rice system in Bangladesh. 相似文献
13.
不同气候和土壤条件下秸秆腐解过程中养分的释放特征及其影响因素 总被引：25，自引：1，他引：24
农田土壤中秸秆腐解伴随氮磷钾养分的释放是重要的生物地球化学过程,也是秸秆还田替代化肥养分的基础。了解不同农区秸秆分解过程中的养分释放动态,揭示秸秆、气候和土壤条件的交互作用机制,是制定秸秆还田合理措施的理论基础。基于寒温带-暖温带-中亚热带的黑土、潮土、红壤互置试验平台,研究了小麦、玉米秸秆在3年腐解过程中养分释放过程和影响因素。结果表明,秸秆中养分释放速率的大小顺序为KPN;秸秆中氮素和磷素在寒温带以及在红壤和潮土中表现为先富集再释放特征,在暖温带、中亚热带以及黑土中表现为直接释放特征;秸秆中钾素均表现为直接快速释放特征,在腐解0.5 a平均释放率达89.5%。气候和土壤条件主导了氮磷的释放,其相对平均贡献率分别为19.5%和15.2%。在腐解后期(2~3 a)气候、土壤和秸秆因素对养分释放的贡献率30%,说明土壤生物因素可能起了主导作用。 相似文献
14.
Influence of land use change on soil nutrients in an intensive agricultural region of North China 总被引：7，自引：0，他引：7
Xiangbin Kong Fengrong Zhang Qi Wei Yan Xu Jiangguang Hui 《Soil & Tillage Research》2006,88(1-2):85-94
The pressures of development and major shifts in land use have increased the need to assess the impact of land use change on soil nutrients. This study was conducted in an area with intensive agricultural land use in north China to assess effects of land use change on soil organic carbon (SOC), total nitrogen (TN), available phosphorus (AP) and available potassium (AK). Soil samples were collected from rainfed land, irrigated land, virgin grassland and vegetable land in 1980 and 1999. SOC, TN and AP were higher in 1999 than in 1980, and the increases followed the following order: vegetable land > irrigated land > rainfed land, except for AK. Soil nutrient contents were increased when land uses underwent the following changes (except for AK): virgin grassland → rainfed land → irrigated farmland → vegetable land. The SOC, TN and AP fluxes (rate of change in C, N, P and K as kg(ha y)−1) in the transition systems from rainfed land to vegetable land were 518.46, 69 and 3.9 kg(ha y)−1, respectively, which were considerably higher than the transition systems from rainfed land to irrigated land. The SOC, TN and AP fluxes in the transition systems from virgin grassland to irrigated land were 297.83, 56.3, 2.1 kg(ha y)−1, respectively, which were higher than the transition systems from virgin grassland to rainfed land. The study shows that land use intensification can increase soil nutrient contents if accompanied by increased fertilizer application. 相似文献
15.
16.
不同演化阶段白刺灌丛沙堆土壤生态化学计量特征 总被引：1，自引：1，他引：0
为了阐明灌丛沙堆发育对土壤碳(C)、氮(N)、磷(P)生态化学计量特征的影响,以吉兰泰荒漠区不同演化阶段白刺(Nitraria tangutorun)灌丛沙堆为研究对象,研究0—100 cm土层土壤C∶N∶P化学计量特征在不同演化阶段的变化规律和垂直分布规律。结果表明:(1)白刺灌丛沙堆土壤有机碳(SOC)、全氮(TN)和全磷(TP)随演化阶段(雏形阶段→发育阶段→稳定阶段→衰亡阶段)的变化呈先增后减的变化趋势。演化阶段对白刺灌丛沙堆SOC影响显著(P<0.05),对TN、TP无显著影响(P>0.05),其SOC、TN、TP均值含量在0—100 cm土层分别为0.42~0.58,0.04~0.07,0.22~0.25 g/kg,远小于全国土壤平均水平(11.12,1.06,0.65 g/kg)。(2)白刺灌丛沙堆SOC、TN、TP含量及其生态化学计量比随土层深度增加无明显规律性。(3)土壤SOC、TN、TP含量及其生态化学计量比均属于中等变异,且变异系数随白刺灌丛沙堆演化不断减小。(4)土壤容重、毛管孔隙度、非毛管孔隙度对白刺灌丛沙堆土壤TN、C∶N、N∶P影响显著,而土壤含水量、pH对白刺灌丛沙堆SOC、TN、TP含量及其生态化学计量比无显著影响。各演化阶段白刺灌丛沙堆SOC、TN是调控白刺灌丛沙堆土壤生态化学计量比的主要因素。因此,该研究结果明晰了白刺灌丛沙堆土壤C∶N∶P生态化学计量特征对不同演化阶段的响应,为该区域白刺群落的保护、利用和植被恢复与重建提供科学依据。 相似文献
17.
Sridhar Patra Stefan Julich Karl-Heinz Feger Mangi Lal Jat P. C. Sharma Kai Schwärzel 《Archives of Agronomy and Soil Science》2013,59(14):2013-2028
ABSTRACTDegradation of soil quality caused by conventional tillage practices is a major concern for the sustainability of rice-wheat cropping systems in South Asian region. Therefore, suitable conservation agriculture (CA) practices are required. This study investigates the stratification and storage of soil organic carbon (SOC) and total nitrogen (TN) as affected by eight years of different CA practices in the North-West Indo-Gangetic Plains of India. There were four treatments: (1) conventionally tilled rice-wheat cropping system, (2) reduced-till CA-based rice-wheat-mungbean system, (3) no-till CA-based rice-wheat-mungbean system, and (4) no-till CA-based maize-wheat-mungbean system. The mean stratification ratio (SR) (i.e. a ratio of the concentrations of SOC and TN in the soil surface to those in a deeper layer) of SOC and TN for 0–5:5–10, 10–15, 15–20, 20–25 and 25–30 cm were found higher (> 2) under CA practices compared to intensive tillage-based conventional agricultural practice (< 2). No-till CA-based rice-wheat-mungbean system stored the highest amount of SOC (25.32 Mg ha?1) whereas reduced till CA-based rice-wheat-mungbean system stored highest amount of TN (3.21 Mg ha?1) at 0–30 cm soil depth. This study shows that CA stratifies SOC and TN and helps to enhance SOC sequestration and soil quality. 相似文献
18.
不同耕作方式对豫西旱区坡耕地水肥利用与流失的影响 总被引：24，自引：4，他引：24
为筛选适宜豫西早坡地应用的耕作技术，对深松覆盖、免耕覆盖、一次深翻和传统耕作等4种耕作方式的土壤水分、养分及其利用与流失情况进行了研究，结果表明：深松覆盖、免耕覆盖能提高土壤蓄水量，土壤有机质和氮、磷、钾含量明显高于传统耕作，特别是对上层土壤全氮及碱解氮和深层土壤的有效磷及速效钾的影响更为明显，并能有效地减少地表产流次数和径流量，减少土壤养分的流失，提高水分利用效率和养分的生产效率，显著提高小麦产量。与传统耕作相比，深松覆盖和免耕覆盖水分利用效率提高16．37％和10．62％，氮素生产效率提高17．40％和10．27％，磷素生产效率提高19．80％和12．54％，钾素生产效率提高19．44％和12．19％，小麦产量提高23．22％和15．38％，经济效益提高29．36％和21．13％。 相似文献
19.
Zheng Xiangzhou Lin Cheng Guo Baoling Yu Juhua Ding Hong Peng Shaoyun Zhang Jinbo Ireland Eric Chen Deli Müller Christoph Zhang Yushu 《Journal of Soils and Sediments》2020,20(4):1897-1905
Purpose
Nitrogen (N) is an important nutrient for re-vegetation during ecosystem restoration, but the effects of cover restoration on soil N transformations are not fully understood. This study was conducted to investigate N transformations in soils with different cover restoration ages in Eastern China.
Materials and methodsSoil samples were collected from four degraded and subsequently restored lands with restoration ages of 7, 17, 23, and 35 years along with an adjacent control of degraded land. A 15N tracing technique was used to quantify gross N transformation rates.
Results and discussionCompared with degraded land, soil organic carbon (SOC) and total N (TN) increased by 1.60–3.97 and 2.49–5.36 times in restoration land. Cover restoration increased ammonium and nitrate immobilization, and dissimilatory nitrate reduction to ammonium (DNRA) by 0.56–0.96, 0.34–2.10, and 0.79–3.45 times, respectively, indicating that restoration was beneficial for N retention. There were positive correlations between SOC content and ammonium and nitrate immobilization and DNRA, indicating that the increase in soil N retention capacity may be ascribed to increasing SOC concentrations. The stimulating effect of SOC on ammonium immobilization was greater than its effect on organic N mineralization, so while SOC and TN increased, inorganic N supply did not increase. Autotrophic and heterotrophic nitrification increased with increasing SOC and TN concentrations. Notably, heterotrophic nitrification was an important source of NO3??N production, accounting for 47–67% of NO3??N production among all restoration ages.
ConclusionsThe capacity of N retention was improved by cover restoration, leading to an increase in soil organic carbon and total N over time, but inorganic N supply capacity did not change with cover restoration age.
相似文献20.
Pratap SRIVASTAVA Rishikesh SINGH Sachchidan TRIPATHI Pardeep SINGH Shikha SINGH Hema SINGH Akhilesh Singh RAGHUBANSHI Pradeep Kumar MISHRA 《土壤圈》2017,27(5):792-806
It is globally accepted that soil carbon (C) dynamics are at the core of interlinked environmental problems,deteriorating soil quality and changing climate.Its management remains a complex enigma for the scientific community due to its intricate relationship with soil nitrogen (N) availability and moisture-temperature interactions.This article reviews the management aspects of soil C dynamics in light of recent advances,particularly in relation to the availability of inorganic N pools and associated microbial processes under changing climate.Globally,drastic alterations in soil C dynamics under changing land use and management practices have been primarily attributed to the variation in soil N availability,resulting in a higher decomposition rate and a considerable decline in soil organic C (SOC) levels due to increased soil CO2 emissions,degraded soil quality,and increased atmospheric CO2 concentrations,leading to climate warming.Predicted climate warming is proposed to enhance SOC decomposition,which may further increase soil N availability,leading to higher soil CO2 efflux.However,a literature survey revealed that soil may also act as a potential C sink,if we could manage soil inorganic N pools and link microbial processes properly.Studies also indicated that the relative,rather than the absolute,availability of inorganic N pools might be of key importance under changing climate,as these N pools are variably affected by moisture-temperature interactions,and they have variable impacts on SOC turnover.Therefore,multi-factorial studies are required to understand how the relative availability of inorganic N pools and associated microbial processes may determine SOC dynamics for improved soil C management. 相似文献