首页> 外文期刊>Journal of plant nutrition and soil science >Release of nutrients and dissolved organic carbon during decomposition of Chamaecyparis obtusa var. formosana leaves in a mountain forest in Taiwan
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Release of nutrients and dissolved organic carbon during decomposition of Chamaecyparis obtusa var. formosana leaves in a mountain forest in Taiwan

机译:Chamaecyparis obtusa var分解过程中释放养分和溶解的有机碳。枫叶在台湾的山林里

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Forest ecosystems in Taiwan are periodically influenced by typhoons that cause large amounts of litter input to the soil. The potential rapid decomposition of such litter under the warm and moist climatic conditions in Taiwan may lead to nutrient losses via seepage. The goal of this study was to investigate the dynamics of C, N, K, Ca, Mg, and dissolved organic carbon (DOC) during decomposition of Chamaecyparis obtusa var. formosana leaves in a field study at the Yuanyang Lake site in N Taiwan. We simulated the effect of a typhoon by adding about three times the annual aboveground litterfall (totally 13,900 kg ha(-1)) as fresh leaves. Litterbags were taken at 7 dates over 16 months, followed by detection of mass loss and element composition in the remaining litter. Aqueous extracts of the remaining litter were analyzed for DOC and major elements. The properties of DOC were characterized by fluorescence spectra and by its stability against microbial decomposition. The litter mass loss was 35% after 16 months. The losses of Ca after 16 months from the litter bags were about equivalent to mass loss (39%), while those of K and Mg reached 86% and 60% of the initial amount, respectively. From the 13,900 kg ha(-1) of litter applied in total, 59 kg K ha(-1) and 12 kg Mg ha(-1) were released in the 16 months decomposition period, most of it in the first 4 months. The total release of Ca amounted to 69 kg ha(-1) but was more evenly distributed throughout the 16 months of observation. The absolute amount of N in the decomposing litter increased by 37% while the C : N decreased from 69 to 34. Extrapolated to the manipulation treatment, this resulted in a N gain of 36kg N ha(-1) within 16 months. The leaching of K and DOC in laboratory extractions followed an asymptotic function with highest leaching from the initial litter and subsequent decrease with time of decomposition. On the contrary, the leaching of Ca and Mg reached a maximum after 2-4 months of incubation. About 2% of the C was extractable with water from the initially incubated leaves. The bioavailability of the extracted DOC decreased with litter age. Our results indicate that the decomposition of large amounts of litter induces a high risk of K and Mg losses with seepage, but the risk for N losses is low. The sources of N accumulation in decomposing litter at this site require further studies. In the initial phase of litter decomposition, the release of DOC seems to be an important contribution to mass loss.
机译:台湾的森林生态系统会定期受到台风的影响,这些台风会导致大量垫料输入土壤。在台湾温暖潮湿的气候条件下,此类垃圾可能迅速分解,可能导致营养物通过渗漏而损失。这项研究的目的是调查Chamaecyparis obtusa var分解过程中C,N,K,Ca,Mg和溶解性有机碳(DOC)的动力学。台湾北部的元阳湖遗址进行了野外调查。我们模拟了台风的影响,方法是将每年地面上的凋落物增加约三倍(总计13,900 kg ha(-1))作为新鲜叶子。在16个月内的7个日期处取出小垃圾袋,然后检测剩余垃圾中的质量损失和元素组成。分析剩余垃圾的水提物的DOC和主要成分。 DOC的特性通过荧光光谱及其对微生物分解的稳定性来表征。 16个月后,垫料质量损失为35%。垃圾袋中16个月后钙的损失大约相当于质量损失(39%),而钾和镁的钙损失分别达到初始量的86%和60%。从总共施用的13,900 kg ha(-1)的垫料中,在16个月的分解期内释放了59 kg K ha(-1)和12 kg Mg ha(-1),其中大部分在头4个月释放。 Ca的总释放量为69 kg ha(-1),但在观察的16个月中分布更均匀。分解垫料中的N绝对量增加了37%,而C:N从69降低到34。根据操作处理推断,这在16个月内增加了36kg N ha(-1)。实验室提取物中的K和DOC的浸出具有渐近功能,从最初的凋落物中浸出最高,随后随着分解时间的减少而降低。相反,孵育2-4个月后,钙和镁的浸出量达到最大值。大约2%的C可以用水从最初孵育的叶片中提取。提取的DOC的生物利用度随同窝年龄而降低。我们的结果表明,大量凋落物的分解会导致高K和Mg渗漏的风险,但N损失的风险很低。在该地点分解垃圾中的氮积累来源需要进一步研究。在垫料分解的初始阶段,DOC的释放似乎是质量损失的重要原因。

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