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卷二十八 志第八: 音樂一

Volume 28 Treatises 8: Music 1

Chapter 32 of 舊唐書 · Old Book of Tang
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1
Treatise 12: Calendars, Part One
2
輿
In remote antiquity the sage rulers took up the genesis of yin and yang and fathomed the forms of Heaven, Earth, and humanity; they devised chronology to exhaust number and drew the hexagrams to trace change. Chronology held the method of the Great Expansion, and the hexagrams held the texts for casting and counting—out of this calendrical science was born. The Yin drew on the books of the Nine Categories and the Five Regulators; the Rites of Zhou sets down the posts of the court astronomers, by which one traced the courses of sun, moon, and stars and read fortune and misfortune across the nine regions. Down the generations calendrical experts passed their craft from hand to hand—the settled rules of computation and the long-standing regulations they applied together. After the Qin burned the classics, what survived was broken; when the Han arose, each new author followed a different school. They might cite the same texts on pitch-pipes and bells and rehearse the same lore of milfoil and tortoise, yet their era-origins diverged and their cycle constants clashed; some dragged in the Spring and Autumn Annals as proof, others forced the Appended Texts and Images into doubt—every party arched a brow and clapped a palm, insisting that Gan De and Shi Shen were unworthy to be called officers of the sun; Those who cast stalks and sifted the subtle said that Gongshu Ban and Lu Ban did not understand the Way of Heaven. When they turned to the observatory to read omens and tested fortune along the ecliptic, what they said shrank when fullness came; few predictions hit and many failed—on a miss they blamed faulty arithmetic, on a hit they boasted that they knew the seasons. Zhang Shou and Guo Hehai were not living in our day—what proof can settle the matter?
3
輿
Under the Northern Qi, in the Tianbao era, a solar eclipse was due at new moon in the sixth month. Emperor Wenxuan asked the astronomy clerk in advance when the eclipse would occur. Zhang Mengbin said at shen, Zheng Yuanwei and Dong Jun said at chen, and Song Jingye said at si. That day the eclipse fell between the shen and you hours—not one prediction matched the moment. From the Tianbao Calendar that Jingye devised, one can see how coarse or fine it was. Long ago Deng Ping and Luoxia Hong devised the Han Taichu Calendar, and seventeen schools rose against it. Later Liu Hong, Cai Yong, He Chengtian, and Zu Chongzhi were all masters of mathematical astronomy; yet when their calendars came up for imperial review, partisan clamor still shut them out. The art has grown desolate, and those who truly understand it are few. Hence Zhang Zaiyuan wore his seal while the court seethed, and Liu Xiaosun brought a coffin and wept in protest—so that later students only grew more uncertain. In this subject's judgment, nothing surpasses the established methods.
4
綿
When Gaozu took the throne from the Sui, Fu Renjun was first to submit seven proposals, arguing that the wuyin year fell at the head of the upper origin and a new calendar should be set to match the transfer of mandate—thus the Wuyin Calendar was created. Zu Xiaosun and Li Chunfeng argued against him on principle; Renjun rebutted each point at length, and his system was adopted in the Zhenguan reign. Under Gaozong the Grand Astrologer reported that the old calendar's time corrections were drifting and ought to be revised; the emperor ordered Li Chunfeng to create the Linde Calendar. Earlier, at the end of the Sui, Liu Zhuo had devised the Huangji Calendar, but his method had not been adopted; Chunfeng distilled it into a system that contemporaries hailed as precise. Under the Empress Wu, Gautama Siddhartha devised the Guangzhai Calendar. Under Zhongzong, Nangong Shuo devised the Jinglong Calendar—methods the older tradition had already cast aside, yet they were revived. They spoke only of change and could not produce anything truly deep; in the end none of these was kept in use. In the Kaiyuan era the monk Yixing mastered every school's calendrical methods and reported that the Linde Calendar had been in use so long that gnomon readings and celestial coordinates were drifting. Chief Minister Zhang Yue relayed this; Xuanzong summoned Yixing and ordered a new calendar. He and the court astronomer Liang Lingzan first built the armillary chart of the ecliptic, verified the courses of the seven luminaries, took the Great Expansion numbers from the Book of Changes as their standard, and fashioned a new method that remained in use for nearly fifty years. Under Suzong, Han Ying devised the Zhide Calendar. Under Daizong, Guo Xianzhi devised the Wuji Calendar. Under Dezong, Xu Chengsi devised the Zhengyuan Calendar. Under Xianzong, Xu Ang devised the Guanxiang Calendar. Their methods still survive, yet the constants for era-cycles, obscurations, and intercalation sometimes diverge from earlier canons; yet in fixing the seasons of solstice, equinox, and the quarter-points, how do they differ from the old methods? When it comes to empirical proof, few achieve real precision. Handed down through the ages, they merely show that the canonical methods still endure.
5
The earlier history drew the calendrical treatises of Fu Renjun, Li Chunfeng, Nangong Shuo, and Yixing from four masters and compiled them into four fascicles of the Treatise on Calendars. Recent masters of calculation all hold that the methods of Chunfeng and Yixing stand for ages without measurable error; later reformers sought chiefly to distinguish themselves and could not surpass their precision. The Jinglong Calendar was never adopted in practice; the world judged it unsound, and it is passed over here. Only the methods of the Wuyin, Linde, and Dayan calendars are included in this treatise, set before the calendrical officers.
6
The Wuyin Calendar Classic
7
滿
The text above is lost as of this record. From the Start of Autumn, add 4,080 parts on the first day and subtract 76 parts on each later day; take the first day's addition and subtract the running total of later reductions. When this is done, reduce the remainder by the motion-part divisor to obtain the day count. Add these to the mean appearance day and parts; whenever the total fills the motion-part divisor, remove one divisor and carry one day—this yields the fixed appearance day and parts. All later cases follow this rule. This continues through the Autumn Equinox. From Cold Dew, subtract 127 parts per day; if the subtraction cannot be completed, add one motion-part divisor for one day and subtract in reverse to obtain the fixed appearance day and parts. All later cases follow this rule. This continues through the Start of Winter. From Minor Snow through Major Snow, reduce evenly by eight days. At first appearance it stands fourteen degrees from the sun.
8
Mars
9
Mean appearance: from the Winter Solstice, subtract 16,354 parts on the first day and 545 parts on each later day, through Minor Cold. From Major Cold, add 426 parts per day through the Start of Insects. From Rain Water through Grain Rain, add evenly twenty-nine days. From the Start of Summer, add 19,392 parts on the first day and subtract 213 parts on each later day, through Major Heat. From the Start of Autumn, follow the mean rate. From End of Heat, subtract 184 parts per day through the Start of Winter. From Minor Snow through Major Snow. Reduce evenly by twenty-five days. At first appearance it stands seventeen degrees from the sun.
10
Saturn
11
Mean appearance: from the Winter Solstice, subtract 4,814 parts on the first day and add 79 parts on each later day, until the qi period ends. From Minor Cold through Major Cold. Reduce evenly by nine days. At the Start of Spring, reduce evenly by eight days. At the Start of Insects, reduce evenly by seven days. At Rain Water, reduce evenly by six days. At the Spring Equinox, reduce evenly by five days. At Clear Brightness, reduce evenly by four days. From Grain Rain through Grain in Ear, reduce evenly by three days. From the Summer Solstice, within the first ten days reduce evenly by two days. After the tenth day, from Minor Heat, within the first five days reduce evenly by one day. After the fifth day, through the end of the qi period, follow the mean rate. From Major Heat, add 181 parts per day through the Start of Autumn. From End of Heat, add evenly nine days. From White Dew, add 6,002 parts on the first day and subtract 133 parts on each later day, through Cold Dew. From Frost Descent, subtract 79 parts per day through Major Snow. At first appearance it stands seventeen degrees from the sun.
12
Venus
13
滿
Morning mean appearance: from the Winter Solstice, follow the mean rate. From Minor Cold, add 66 parts per day through Major Cold. From the Start of Spring through the Start of Summer, add evenly three days. From Minor Fullness, add 1,964 parts on the first day and subtract 66 parts on each later day, through Grain in Ear. From the Summer Solstice, follow the mean rate. From Minor Heat, subtract 60 parts through Major Heat. From the Start of Autumn through the Start of Winter, reduce evenly three days. From Minor Snow, subtract 1,964 parts on the first day and 66 parts on each later day, through Major Cold.
14
滿
Evening mean appearance: from the Winter Solstice, subtract 100 parts per day through the Start of Spring. From the Start of Insects through the Spring Equinox, reduce evenly nine days. From Clear Brightness, subtract 5,986 parts on the first day and 100 parts on each later day, through Minor Fullness. From Grain in Ear, follow the mean rate. From the Summer Solstice, add 100 parts per day through the Start of Autumn. From End of Heat through the Autumn Equinox, add evenly nine days. From Cold Dew, add 5,986 parts on the first day and subtract 100 parts on each later day, through Minor Snow. From Major Snow, follow the mean rate. At first appearance it stands eleven degrees from the sun.
15
Mercury
16
滿
Morning mean appearance: from the Winter Solstice, reduce evenly four days. From Minor Cold through Major Cold, follow the mean rate. From the Start of Spring through Awakening of Insects, subtract three days. If within Awakening of Insects, more than eighteen degrees but less than forty degrees from the sun, and no Jupiter, Saturn, or Venus is visible in the morning, it is not seen. From Rain Water through the Start of Summer, it should appear but does not. If within Start of Summer, at the same solar distance as described above, and Jupiter, Mars, Saturn, or Venus is visible in the morning, it is also seen. From Minor Fullness through Cold Dew, follow the mean rate. From Frost's Descent through the Start of Winter, add one day. From Minor Snow through the twelfth day before Major Snow, follow the mean rate. If it falls on the thirteenth day before Major Snow, subtract one day. On the fourteenth day before Major Snow, subtract two days. On the fifteenth day before Major Snow, subtract three days. On the sixteenth day before Major Snow, subtract four days.
17
Evening mean appearance: from the Winter Solstice through Clear Brightness, follow the mean rate. From Grain Rain through Grain in Ear, subtract two days. From the Summer Solstice through Major Heat, follow the mean rate. From the Start of Autumn through Frost's Descent, it should appear but does not. If within Start of Autumn or Frost's Descent, at the same evening solar distance as the morning rule above, it is also seen. From the Start of Winter through Major Snow, follow the mean rate. At first appearance it stands seventeen degrees from the sun.
18
Method for Computing the Five Planets' Motion
19
宿 滿 滿
For each planet, set the lodge degree count and parts of the sun's position at midnight before its fixed appearance; to each add the fixed appearance's offset from new moon in days and one part. When minor parts fill the divisor of fourteen parts, carry one to the motion-parts. When motion-parts fill the divisor of 676 parts, carry one degree. Take the star's first-appearance distance from the sun; subtract for morning appearances and add for evening appearances. Count off through the degrees in order to obtain the star's first-appearance degree and parts. From this point onward, discard these minor parts.
20
Procedure for the Next Day
21
滿 滿 退
Add each day's motion in degrees and parts. For Mars and Venus, when minor parts are involved, use the day-rate as denominator. When minor parts fill their denominator, cast out the excess and carry one to the motion-parts. When motion-parts fill the divisor, cast out the excess and carry one degree. When motion varies between faster and slower phases, set aside one day's motion-parts. Apply the daily differential for acceleration or deceleration, then add the result. During stationary motion, continue from the prior value; during retrograde motion, subtract accordingly; during invisibility, do not record longitude. In direct motion exiting the Dipper asterism, subtract the fractional parts; in motion entering the Dipper, first add the fractional parts. When complete, divide all motion-parts by 26 to convert to degree-parts.
22
Jupiter
23
退 退 滿
At first appearance it moves directly, 176 parts 50 seconds per day, slowing by 1 part each day. In 114 days it travels 19 degrees 209 parts. Then it stations for 28 days. Then it retrogrades 97 parts per day. In 84 days it retreats 12 degrees 50 parts. It stations again for 26 days 596 parts, 74 minor parts. Add the parts from the first fixed-appearance day; whenever the total fills the motion-part divisor, cast out the excess and carry one day. Then it moves directly again: 60 parts on the first day, speeding by 1 part each day. In 114 days it travels 19 degrees 437 parts and becomes invisible.
24
Mars
25
At first appearance upon entering the Winter Solstice, the initial rate is 241 days for 163 degrees of travel. Thereafter decrease the day-rate and degree-rate by 1 every 2 days. Through 128 days the rate becomes 177 days for 99 degrees. This rate holds through day 161. Then decrease the day-rate and degree-rate by 1 every 3 days. Through 182 days the rate becomes 170 days for 92 degrees. This rate holds through day 188. Then increase the day-rate and degree-rate by 1 every 3 days. Through 227 days the rate becomes 183 days for 105 degrees. Then increase the day-rate and degree-rate by 1 every 2 days. Through 249 days the rate becomes 194 days for 116 degrees. Then increase the day-rate and degree-rate by 1 each day. Through 310 days the rate becomes 255 days for 177 degrees. This rate holds through day 337. Thereafter decrease by 1 every 2 days. Through 365 days it returns to the initial rate of 241 days for 163 degrees.
26
滿 滿 退退 滿 滿
At first appearance after Minor Cold, remove 1 from the day-rate every 3 days through Awakening of Insects. From Rain Water through the Start of Summer, uniformly remove 20 from the day-rate. From Minor Fullness, initially remove 20 from the day-rate. Next remove 19 every 3 days, then 18 each day. Next remove 1 day every 3 days through Minor Heat, then follow the mean rate—this is the fixed day-rate. If the motion begins between End of Heat and the Autumn Equinox, subtract 6 from the degree-rate throughout; adjust according to the number of days past the Winter Solstice and subtract according to the solar term entered—this is called initial rapid motion. The day-rate and degree-rate follow the same rules as the initial motion phase. If the motion falls between Major Cold and Major Heat, use variable motion, slowing by 1 part each day. In all other seasons, use uniform motion. If entering between White Dew and the Autumn Equinox, start at half a degree per day, covering 20 degrees in 40 days. Set aside 40 days of the day-rate and 20 degrees of the degree-rate as a separate half-degree segment; when that segment is complete, calculate the uniform-motion parts and continue from there. To find uniform-motion parts, multiply the fixed degree-rate by the part divisor and divide by the fixed day-rate; the quotient is one day's uniform motion, and the remainder gives the minor parts. For differential motion, take the day-rate and subtract 1. Halve the result, add the one-day uniform-motion parts—that yields the initial day's motion-parts. Continue until the allotted days and degrees are used up, then enter slow motion. Initial daily motion is 326 parts, slowing by 1.5 parts each day; in 60 days it covers 25 degrees and 5 parts. If the initial rapid phase had 6 degrees subtracted from the degree-rate, on the first day of this slow phase add 67 parts and 36 minor parts. When minor parts fill 60, cast out the excess and carry one to the motion-parts; in 60 days it covers 31 degrees with the same fractional value. Then it stands still for 12 days. If days were subtracted during initial rapid motion, split those days between the two stationary periods, with any odd days assigned to the later one. Then it retrogrades at 192 parts per day, covering 17 degrees 28 parts in 60 days. It stands still again for 12 days 626 parts, 30 minor parts. Apply the parts from the first fixed appearance as before; when full, cast out the excess as above. Then it resumes direct motion in the later slow phase. In the later slow phase, initial daily motion is 238 parts, accelerating by 1.5 parts each day; in 60 days it covers 25 degrees 35 parts. If this slow phase falls between the Start of Autumn and the Autumn Equinox, add one day, with motion of 67 parts and 36 minor parts. When full, cast out the excess as before; in 60 days it covers 31 degrees. The fractional values match. Then comes the later rapid phase. Entering the Winter Solstice, the initial rate is 136 degrees in 214 days. Thereafter decrease the day-rate and degree-rate by 1 each day. Through 37 days the rate becomes 99 degrees in 177 days. Then decrease the day-rate and degree-rate by 1 every 2 days. Through 57 days the rate becomes 89 degrees in 167 days. This rate holds through day 79. Then increase the day-rate and degree-rate by 1 every 3 days. Through 130 days the rate becomes 160 degrees in 184 days. Then increase the day-rate and degree-rate by 1 every 2 days. Through 144 days the rate becomes 113 degrees in 191 days. Then increase the day-rate and degree-rate by 1 each day. Through 190 days the rate becomes 159 degrees in 237 days. Then increase the day-rate and degree-rate by 1 each day. Through 210 days the rate becomes 189 degrees in 267 days. This rate holds through day 259. Then decrease the day-rate and degree-rate by 1 every 2 days. Through 365 days the rate returns to 136 degrees in 214 days. If the later slow phase added 6 degrees, subtract 6 from the degree-rate in this later rapid phase—that is the fixed degree-total. Adjust each by the day-count after the Winter Solstice to obtain the day- and degree-rates for the later rapid phase. If the phase falls between the Start of Summer and the Summer Solstice, use half a degree per day, covering 30 degrees in 60 days. If it falls between Minor Heat and Major Heat, it covers 20 degrees in 40 days. Set aside the corresponding day- and degree-rates as a separate half-degree segment; when that segment is complete, calculate the uniform-motion parts and continue from there. Each phase runs through its allotted days and degrees, then the planet disappears.
27
Saturn
28
退退 滿
At first appearance it moves directly at 60 parts per day, covering 7 degrees 248 parts in 83 days. Then it stands still for 38 days. Then it retrogrades at 41 parts per day, covering 6 degrees 44 parts in 100 days. It stands still again for 37 days 61 parts, 4 minor parts. Also add the parts from the first fixed appearance day. When full, cast out the excess as before. Then direct motion at 60 parts per day, 7 degrees 248 parts in 83 days, then it disappears.
29
Venus
30
退退 滿
At morning first appearance it retrogrades at 1.5 degrees per day, covering 15 degrees in 10 days. Then it stands still for 9 days. Then it resumes direct slow motion with variable rate. Beginning slow, it accelerates by 8 parts each day, covering 30 degrees in 40 days. If this slow phase falls between Great Snow and Lesser Full Grain, use this as the fixed rate to calculate the motion-parts. From Grain in Ear, subtract 1 degree every 10 days as the fixed total, through the Summer Solstice. From Minor Heat through Frost Descent, subtract an even 3 degrees. From the Start of Winter, subtract 3 degrees on the first day and 1 degree every 10 days thereafter, through Frost Descent and Minor Snow—these are the fixed degrees. To find one day's motion-parts, multiply the fixed degrees by the motion-parts factor and divide by 40 for the equal parts; the remainder gives the minor parts. Multiply 4 by 39, subtract from the equal parts—that yields the initial day's motion-parts. Uniform motion: 1 degree per day, 15 degrees in 15 days. If this uniform-motion phase begins after Minor Cold, increase both the day-count and degree-count by 1 every 10 days, through Awakening of Insects. From Rain Water onward, the rate is 21 degrees in 21 days throughout. After the Spring Equinox, decrease by 1 every 10 days through the Start of Summer, ending at 15 days. From End of Heat through Cold Dew, this uniform-motion phase does not apply. From Frost Descent, increase by 1 every 4 days through Great Snow; then the rate is 15 degrees in 15 days. Rapid motion: 204 degrees in 170 days. If the earlier direct slow phase subtracted degrees, add that amount to this phase's degree-total as the fixed value. To find one day's motion in degrees and parts, subtract the degree-total from 170 days, multiply the remaining travel by the part divisor, and divide by 170—the quotient gives the daily uniform-motion degrees and parts. It disappears in the morning in the east (at conjunction).
31
滿 退退西
At evening first appearance, direct rapid motion: 200 degrees in 170 days. Through the Start of Summer, follow this direct rapid rate. From the Winter Solstice through the Start of Summer, use this as the fixed rate. From Lesser Full Grain, add 1 degree every 6 days. From the beginning of Major Heat through Grain in Ear, and from the Summer Solstice through Minor Heat, adjust by an even 5 degrees. From Major Heat, add 5 degrees initially, then subtract 1 degree every 3 days until the qi period ends. From the Start of Autumn through Great Snow, revert to the base rate. From White Dew through the Spring Equinox, all phases use variable motion. Beginning fast, it slows by 1.5 parts each day. From Clear Brightness through End of Heat, use uniform motion matching the morning rapid phase. For variable motion, halve 169, multiply by 1.5 parts, add to the uniform-motion parts—that yields the initial day's motion in degrees and parts. Uniform motion: 1 degree per day, 15 degrees in 15 days. If this uniform-motion phase begins after the Winter Solstice, decrease both the day-count and degree-count by 1 every 10 days, through the Start of Spring. From Awakening of Insects through Grain in Ear, the rate is 9 degrees in 9 days throughout. After the Summer Solstice, increase by 1 every 5 days, through Minor Heat. From Major Heat through the end of the qi period, the rate is 15 degrees in 15 days throughout. After the Start of Autumn, adjust by 1 every 6 days, through Minor Snow. From Great Snow through the end of the qi period, the rate is 15 degrees in 15 days throughout. Direct slow motion with variable rate. Beginning fast, it slows by 8 parts each day, covering 30 degrees in 40 days. If degrees were added earlier, subtract that amount here; to find one day's motion-parts, apply the morning slow procedure in reverse—where that called for subtraction, add instead. It stands still again for 9 days. Then it retrogrades at half a degree per day, covering 5 degrees in 10 days, and disappears in the evening in the west.
32
Mercury: at morning first appearance it stands still for 6 days. Direct slow motion at 169 parts per day, covering 1 degree in 4 days. If first appearance falls between Major Cold and Awakening of Insects, omit this slow-motion phase. Uniform motion: 1 degree per day, 10 degrees in 10 days. If this uniform-motion phase begins after Major Cold, decrease both the day-count and degree-count by 1 every 2 days; at 20 days both are used up—there is no uniform-motion phase. Rapid motion at 1 degree 690 parts per day, covering 19 degrees 6 parts in 10 days. If there was no slow phase earlier, reduce this rapid motion by 203 parts per day, covering 17 degrees 4 parts in 10 days. It disappears in the morning in the east (at conjunction).
33
西
At evening first appearance, direct rapid motion at 1 degree 609 parts per day, covering 19 degrees 6 parts in 10 days. If this rapid phase falls between Minor Heat and End of Heat, reduce daily motion by 203 parts, covering 16 degrees 4 parts in 10 days. Uniform motion: 1 degree per day, 10 degrees in 10 days. If this uniform-motion phase begins after Major Heat, decrease both the day-count and degree-count by 1 every 2 days. At 20 days both day- and degree-rates are used up—there is no uniform-motion phase. Slow motion at 169 parts per day, covering 1 degree in 4 days. If the rapid phase was reduced by 203 parts, omit this slow-motion phase. It stands still again for 6 days 9 parts. It disappears in the evening in the west (at conjunction).
34
Method for Computing Conjunctions and Crossings
35
Conjunction divisor: 12,741,205 parts.
36
Node-parts factor: 6,370,629 parts.
37
New-moon difference: 1,085,492 parts.
38
Full-moon parts: 6,913,350 parts.
39
Conjunction limit: 5,827,858 parts.
40
Full-moon difference: 542,747 parts.
41
Outer limit: 6,760,782 parts.
42
Middle limit: 12,351,025 parts.
43
Inner limit: 12,198,458 parts.
44
Node-time factor: 29,018.
45
Method for Computing Node Parts
46
滿 滿 滿 滿 滿
Take the accumulated months since the upper origin and divide by the conjunction divisor. Multiply the remainder by the new-moon difference. When the product fills the conjunction divisor, discard full multiples again. In Renjun's original procedure, the Wude-era revision adds 7,755,164 parts to the node difference. The remainder is the mean node parts for the new moon of the year's Heavenly First Month. To find the mean node parts at full moon, add the full-moon parts; discard full multiples as before, and the result is the mean parts. For subsequent months, when new moon or full moon falls within the Winter Solstice solar term, take the mean value as fixed. From entry into Slight Cold, add 1,650 parts of solar-term difference per day until Start of Spring. From Awakening of Insects through Clear Brightness, add 76,100 parts in total. On each subsequent day, subtract 1,650 parts until Grain Fills. Take the amount added on the first day, subtract the cumulative reductions for later days, and add the remainder to the mean node parts. From Grain in Ear through the Summer Solstice, again take the mean as fixed. Add the result; when it fills the conjunction divisor, discard the multiple. The remainder is the fixed node parts. When the new moon falls in an eclipse-prone conjunction—between Slight Cold and Rain Water, or between Beginning of Summer and Grain Fills—and the excess amounts to less than two hours, add half the solar-term difference in each case. If two hours or more, add nothing. When the new moon's timed node parts fall below the full-moon difference and above the outer limit, and planets are invisible—Jupiter and Saturn more than ten days from appearance, Mars more than forty days from appearance, or Venus in morning or evening concealment more than twenty-two days from appearance— if any one of these planets is present, do not add the solar-term difference. For new and full moons after Slight Heat, subtract 1,200 parts of solar-term difference per day until End of Heat. From White Dew through Frost's Descent, subtract 95,820 parts in total. From Beginning of Winter, subtract 63,300 parts on the first day and 2,110 parts on each subsequent day until Slight Snow. Take the amount subtracted on the first day, subtract the cumulative reductions for later days, and use the remainder to reduce the mean node parts. From Great Snow onward, again take the mean as fixed. If the remainder is insufficient for subtraction, add one conjunction divisor before subtracting. The remainder is the fixed node parts. When the new moon's node parts lie above the inner conjunction limit and below the middle node limit, and planets are invisible as described above, do not subtract the solar-term difference.
47
滿 滿
Method for determining inner versus outer path and distance before or after conjunction: if the fixed node parts amount to less than the node-parts factor, the moon is on the outer path. Discard one full node-parts factor; the remainder places the moon on the inner path. If the remainder is less than the full-moon difference, it is the distance before conjunction. Divide by the hour factor; each unit is the number of hours before conjunction. If above the conjunction limit, subtract the node-parts factor instead. The remainder is the distance after conjunction; divide again by the hour factor to obtain the number of hours. At full moon there is a lunar eclipse. If the new moon is on the inner path, there is a solar eclipse at new moon. Even if the moon is on the inner path but far from conjunction, or on the outer path but near it, an eclipse may still occur.
48
Method for Computing the Hour of Lunar Eclipse
49
Take the fixed minor remainder of the eclipsed full moon. If the moon is on the first day of the sequence, subtract 280. On the fifteenth day, add it back. If on the fourteenth day, add 550. On the twenty-eighth day, subtract it. For each day entered thereafter, add 280 when the moon is in excess and subtract when it is in contraction; the result is the fixed remainder. Multiply by twelve and divide by the hour factor, 6,503; the quotient is the number of half double-hours. Count from midnight, and the double-hour reached outside the count is the position. Midnight counts as one; each subsequent double-hour counts as two. The remainder is the fractional part within the double-hour. If the fractional remainder falls before the middle of the double-hour, double it. If division by the factor yields nothing, the time is the start of the double-hour. Multiply by three; each unit obtained by division is called a strong. One strong, or two strongs, yields the designation minor-weak. If doubled, each unit obtained is minor. In quarter divisions, one is minor, two is half, and three is major. For whatever remains, multiply by three again; each unit obtained is a strong. Two strongs yield the designation half-weak. If the fractional remainder falls after the middle of the double-hour, double it as well. If division yields nothing, the time is exactly the middle of the double-hour. Multiply by three; two units obtained are one strong, yielding the designation half-strong. Two strongs yield the designation major-weak. If doubled, each unit obtained is major. For whatever remains, multiply by three again; one unit obtained is a strong, yielding the designation major-strong; If two strongs are obtained, the time is the end of the double-hour. It may also be named from the preceding double-hour. When the moon eclipses at opposition, if the eclipse falls more than one and a half hours after sunrise or before sunset, do not record it.
50
Method for Computing the Hour of Solar Eclipse
51
退 退 滿 退
Take the fixed minor remainder of the eclipsed new moon. If the moon is on the first day of the sequence, subtract 300. On the fifteenth day, add it back. If on the fourteenth day, add 550. On the twenty-eighth day, subtract it to obtain the fixed value. Thereafter the seasonal addition-and-subtraction limits no longer apply. In spring, on the inner path, when the moon is more than four hours from conjunction and has entered the sequence, add 280 if in excess and subtract if in contraction. In summer, on the inner path, add 280 if in excess and subtract if in contraction. In autumn, on the inner path, when the moon is within eleven hours of conjunction, add 280 if in excess and do not add if in contraction; if more than eleven hours from conjunction, add 550 if in excess and subtract 180 if in contraction. In winter, on the inner path, when within five hours of conjunction, add 280 if in excess and do not add if in contraction. These yield the fixed remainder. Multiply by twelve and divide by the hour factor to obtain the number of half double-hours; count from midnight, and the double-hour reached outside the count is the position. Determine the double-hour by the method above. The remainder is the fractional part within the double-hour; set it aside as an auxiliary value. If the time falls before the middle of a cardinal double-hour, subtract the auxiliary from the factor; the remainder is the difference rate. If after the middle, retreat one half double-hour, add the remainder back to the factor, and use the auxiliary as the difference rate. If before the middle of a seasonal double-hour, add the auxiliary to the factor to obtain the difference rate. If after the middle, take one half double-hour, add the remainder back to the factor, double the factor and add the auxiliary, and the result is the difference rate. If before the middle of an angular double-hour, triple the factor and subtract the auxiliary; the remainder is the difference rate. If after the middle, retreat one half double-hour, add the remainder to the factor and the factor to the auxiliary, then triple the factor and subtract the auxiliary to obtain the difference rate. Also take the hours from conjunction: if three or fewer, add three; if six or fewer, add two; if nine or fewer, add one; if more than nine, use the number itself; if twelve or more, use twelve; multiply the difference rate by this value. If the time falls after the middle of a seasonal double-hour and before the middle of an angular double-hour, and the moon is six or more hours from conjunction, use six to multiply the difference rate. If six hours or fewer, use the number itself without addition. Divide by fourteen; the quotient is the time difference. From zi through the middle of mao, and from wu through the middle of you, add the hour remainder; from mao through the middle of wu, and from you through the middle of zi, subtract the hour remainder. If addition fills the hour factor, discard the multiple and carry one to the double-hour, advancing to the preceding one. If subtraction is insufficient, retreat one half double-hour, add the hour factor, then subtract, moving back to the following one. The remainder is the fixed fractional part within the double-hour. Then, as with the lunar-eclipse method, name the fractional part: zi, wu, mao, and you are cardinal double-hours; chen, xu, chou, and wei are seasonal; yin, shen, si, and hai are angular. If the eclipse falls more than one and a half hours before or after sunrise, do not record it.
52
Method for When the Inner Path Does Not Eclipse
53
西
On the fifth-month new moon of summer, if the computed hour falls in the three southern double-hours and the moon is more than thirteen hours before conjunction; or on the sixth-month new moon, if it is more than thirteen hours after conjunction—no eclipse occurs. From Awakening of Insects through Clear Brightness, if the moon is more than thirteen hours before conjunction, is in contraction, and the computed hour falls in wei, si, or the western double-hours, there is also no eclipse. From End of Heat through Cold Dew, if the moon is thirteen hours after conjunction, is in excess, and the computed hour falls in si, ji, or the eastern double-hours, there is also no eclipse.
54
Method for Solar Eclipse on the Outer Path
55
Regardless of whether conjunction comes before or after, if the moon is within one hour of conjunction, there is always an eclipse. If before conjunction within two hours and the moon is in excess more than two hours from conjunction, there is also an eclipse. If after conjunction within two hours and the moon is in contraction more than two hours from conjunction, there is also an eclipse. In summer, if the moon is two hours from conjunction and the computed hour falls in the three southern double-hours, there is also an eclipse. If the eclipse falls within twelve hours of an equinox or solstice and within six hours of conjunction, there is also an eclipse. If within three days of the Spring Equinox and within two hours after conjunction, there is also an eclipse. Within three days of the Autumn Equinox, if the moon is within two hours before conjunction, there is also an eclipse. Whenever the moon is within three hours of conjunction and planets are invisible as described above, there is also an eclipse.
56
Method for Computing Lunar Eclipse Magnitude
57
Take the parts of departure from conjunction. In winter, subtract two hours' worth of non-eclipse parts whether conjunction comes before or after. In spring, subtract half an hour before conjunction and two hours after conjunction. In summer, use the fixed value unchanged. In autumn, subtract two hours before conjunction and half an hour after conjunction. If the subtraction cannot be completed, the eclipse is total; otherwise divide by 36,183, and the quotient is the non-eclipse parts. For the remainder, count above half the divisor as half-strong and below as half-weak; subtract from fifteen, and the remainder is the eclipse magnitude in great parts.
58
Method for Determining Where the Lunar Eclipse Begins
59
西 西
On the outer path, obscuration first appears in the northeast and reaches its maximum in the northwest. On the inner path, obscuration first appears in the southeast and reaches its maximum in the southwest. If the magnitude is thirteen parts or more, obscuration begins due east. All these directions are reckoned from due south.
60
Method for Computing Solar Eclipse Magnitude
61
Take the parts of departure from conjunction. From after the Winter Solstice through the Start of Spring, subtract 120,800 in total; the remainder is the non-eclipse parts. If the remainder is insufficient, subtract from the node parts instead; what remains is the non-eclipse parts. Also subtract the full-moon difference to obtain the fixed factor. When conjunction comes after and the moon is in contraction, take the full-moon difference itself as the fixed factor without subtracting it. From Awakening of Insects, subtract 228,000 parts on the first day and 1,810 parts on each later day; take the first day's subtraction, subtract the running total of later reductions, and use the remainder to reduce the node parts. Continue until Grain in Ear. From the Summer Solstice, subtract 2,400 parts per day until White Dew. From the Autumn Equinox through Great Snow, subtract 228,000 parts in total. Whenever subtraction is insufficient, reverse the operation against the node parts as before; when this is done, the result is the non-eclipse portion throughout. From the Winter Solstice through Slight Cold, the non-eclipse parts follow the fixed value unchanged. From Great Cold through Beginning of Summer, if the moon is more than five hours after conjunction, subtract one hour's worth of non-eclipse parts in every case. When the time difference requires subtraction, subtract from the before-conjunction figure and add to the after-conjunction figure. If subtraction cannot be completed, the eclipse is total. When the time difference requires addition, add to the before-conjunction figure and subtract from the after-conjunction figure. If subtraction cannot be completed, the eclipse is total. Take this as the fixed parts, multiply by fifteen, and divide by the fixed factor; the quotient is the non-eclipse parts. For the remainder, count above half the divisor as half-strong and below as half-weak; subtract from fifteen, and the remainder is the eclipse magnitude in great parts.
62
Method for Determining Where the Solar Eclipse Begins
63
西 西 西
On the outer path, obscuration first appears in the southwest and reaches its maximum in the southeast. On the inner path, obscuration first appears in the northwest and reaches its maximum in the northeast. If the obscuration is thirteen degrees or more, it begins due west. These directions, too, are reckoned from due south.
64
Method for Finding Sunrise and Sunset Times
65
Subtract the entered solar term's sunrise or sunset double-hour quarters and parts from those of the next solar term. Multiply the remainder by the number of days elapsed within the solar term and divide by fifteen. Add or subtract this result to the entered solar term's value to obtain the fixed times of sunrise and sunset. From the Winter Solstice to the Summer Solstice, subtract for sunrise and add for sunset. From the Summer Solstice to the Winter Solstice, add for sunrise and subtract for sunset. The remainder within the double-hour is the fixed quarter and fractional parts.
66
On the second day of the fifth month: calendar verifier, former Calendar Doctor Nangong Ziming.
67
Calendar verifier, former Calendar Doctor Xue Hongyi.
68
Calendar verifier, Computational Calendar Doctor Wang Xiaotong.
69
Superintendent of calendar verification, Chief Minister of the Court of Judicial Review and Duke of Qinghe County, Cui Shanwei.
70
Half the night clepsydra.
71
As prescribed in the classic, enter these values below the clepsydra quarters for sunrise and sunset under each of the twenty-four solar terms.
72
Method for Computing the Hour of Lunar Eclipse
73
滿
For each eclipsed full moon, multiply the fixed minor remainder by a hundred quarters and divide by the day factor; check whether the nearest solar term falls short of midnight, assign the day, and enter it on the calendar from the jiazi count.
74
滿
Method for Lunar Eclipse First Contact and Full Recovery: Pre-establishing the Quarter-Use for Each Clepsydra Arrow and Watch Tally
75
Double the half-night clepsydra for the solar term on the day of the lunar eclipse and divide by twenty-five; the result is the tally quarter-parts, entered below on the calendar.
76
Lunar Eclipse Magnitude Quarter-Rate: set the lunar eclipse parts.
77
Method for Fixed Quarters of Solar and Lunar Eclipse Hour-Addition
78
Take the fixed remainder of the solar or lunar eclipse hour-addition. If the time falls after the middle of the double-hour, add the hour-addition factor to the hour remainder, multiply by twenty-five, and take one quarter for every 39,018; count off the quarters, and the result is the entered double-hour quarter.
79
滿
Method for First Contact and Full Recovery
80
滿
Set the eclipse parts with the quarter-rate as auxiliary, multiply by the entered calendar increase-decrease rate, and divide by 4,057. If in excess, reverse the increase and decrease; if in contraction, apply the increase and decrease as given; take the auxiliary as the fixed eclipse quarter-count, multiply by six, divide by ten, and subtract from the eclipse hour-addition double-hour quarter to obtain first contact. Again multiply the remainder's fixed quarter-count by four, divide by ten, and add to the eclipse hour-addition double-hour quarter to obtain full recovery.
81
Method for First, Maximum, and Last Watch Tallies of the Eclipse Night
82
滿 滿
From that day's entered double-hour with its remaining quarters and parts, add double-hour quarters and parts in sequence until first contact; subtract two quarters and twelve parts; divide by the watch's quarter-use and parts, and if the result is less than one full watch, that is the first-eclipse watch tally. Add the quarters to maximum as obtained by the method and assign the time; that is maximum obscuration. Add the post-maximum quarters as obtained and assign the time; that is the last watch tally's quarters and parts. If full recovery occurs before sunrise or first contact after sunset, do not record the eclipse.
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